From collection Creating Acadia National Park: The George B. Dorr Research Archive of Ronald H. Epp

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Davis, Wm M. (1850-1934)
Davis, WM. M
(1850-1934)
8/21/2018
William Morris Davis I Harvard Magazine
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William Morris Davis
On Reader
Brief life of a pioneering geomorphologist: 1850-1934
1. The Low End Th
by PHILIP S. KOCH
2. Oasis in Limesto
SEPTEMBER-OCTOBER 2018
3. The Pragmatist
4. Who Built the Py
5. Take Care of Eac
You Might
Alexis Sa
general
profile
The Har
offers re
reflectio
2018 Hir
winners
Davis relaxing in 1910 at Devil's Thumb, on the Continental Divide near Corona, Colorado
Photograph courtesy of the Houghton Library
Naught looks the same for long..
Waters rush on, make valleys where once stood plains;
hills wash away to the sea.
Marshland dries to sand, while dry land
becomes stagnant, marshy pool.
From Nature, springs erupt or are sealed;
from earthquakes, streams burst forth or vanish.
8/21/2018
William Morris Davis I Harvard Magazine
IN Metamorphoses, the Roman poet Ovid, echoing Pythagoras, alludes to
geomorphology: the study of the forms taken by the earth's surface, and what causes
them. Almost 19 centuries later, William Morris Davis, S.B. 1869, devised a clear,
concise, descriptive, and idealized model of landscape evolution that revolutionized and in
many ways created this field of study.
Born into a prominent Philadelphia Quaker family, Davis studied geology and geography at
Harvard's Lawrence Scientific School and then joined a Harvard-sponsored geographic-
exploration party to the Colorado Territory, led by the inaugural Sturgis-Hooper professor of
geology, Josiah Dwight Whitney. Wild stories had circulated since soon after the Louisiana
Purchase about Rocky Mountain peaks 18,000 feet or higher. The Harvard expedition set out to
investigate, and found none, but they did find "14ers" (14,000-plus feet). Among these, the
expedition members surveyed, named, and made two first-recorded summitings in the
"Collegiate Peaks," designating the tallest in the group Mount Harvard (honoring their
sponsor), and the second tallest Mount Yale (honoring Whitney's alma mater).
Once back in Cambridge, Davis earned a master's in mining
engineering from the University's short-lived Hooper
School of Mining and Practical Geology in 1870. Three
years at an Argentinian observatory, and a bookkeeping
stint in Philadelphia, followed-until geologist Nathaniel
Southgate Shaler hired him to teach at Harvard in 1876.
He had a slow start in academe, with few accolades for
either his early teaching or his early research. (In 1882,
President Charles William Eliot even advised him to seek
employment elsewhere.) But Davis was tenacious, as well as
a keen observer of nature, a master of logical deduction, and
a brilliant synthesizer of disparate observations and ideas.
From his own field observations and studies made by the
original nineteenth-century surveyors of the western
Davis, looking professorial in 1910
United States, he devised the theory for which he is best
Photograph courtesy of the Harvard University
known: the "Erosional Cycle." Inspired by the work of
Archives
Erasmus and Charles Darwin and Jean-Baptiste Lamarck, it
had a strong evolutionary flavor.
Alongside tectonic uplift, Davis identified rivers and their tributaries as the primary agents for
altering the appearance of landscapes, and distinguished three anthropomorphically named
stages of landscape evolution, all initiated by uplift. In "Youth," narrow, incised river valleys
locally decrease the growing elevation differences between "uplands" and "base-level" caused by
uplift. In "Maturity," these elevation differences and the number of branching streams reach
their maxima, while valleys cut downward and broaden. In "Old Age," the ever-broadening
valleys hold meandering channels that create rolling lowlands ("peneplains"). In a complete
cycle, the stages transition gradually unless interrupted and reset by subsequent uplift
("Rejuvenation"). This theory, published between 1886 and 1911, moved geomorphology,
despite some opposition, from purely local descriptions to global explanations-and in the
history of his discipline, time is often demarcated as "before" or "after" Davis.
By the time he became a full professor in 1890, Davis had published more than 100 works on
everything from astronomy to zoology and was renowned for inspirational lecturing and the
complex but lucid blackboard illustrations he executed ambidextrously. Having lamented once
that his field was "as much a sealed book to the person of ordinary intelligence and education
as.
a great cathedral would be to a backwoodsman. It makes one grieve to think of
the
8/21/2018
William Morris Davis I Harvard Magazine
he worked to rectify the situation; his pedagogical ideas would affect the content and teaching
of physical geography in primary and secondary schools worldwide for nearly a century.
Sharing an outing in Colorado in the 1890s with Scottish geologist Henry M. Cadell (front left) and a former
student, R.E. Dodge, A.B. 1890, A.M. '94 (at rear), a future professor at Columbia
Photograph courtesy of the Cabot Science Library
In 1899, Davis himself became the Sturgis-Hooper professor, like his mentor, Whitney. He
received numerous awards from professional societies and honorary doctorates on three
continents; he even became a knight of the Legion of Honor. Retirement from Harvard in 1912
did not end his influence. Although deeply shaken by World War I and the deaths of his first,
and then his second, wife, he rallied by the mid 1920s: marrying a third time, lecturing widely,
and relocating first to the University of Arizona and subsequently to Caltech. He produced key
works on the origins of coral reefs and on erosion in deserts, along coasts, and in limestone
caverns, and created more print pages and drawings as an octogenarian than most do in an
entire career.
His cyclical model fell under attack-including by some in his former department at Harvard:
faulted for ignoring the erosional roles of climate, underlying geology, physical processes, and
the marine environment as well as changes in global sea-level. In his deductive determinism, he
often appears to conflate model with observation. Dogmatic? Perhaps he was. Yet Davis was
the first to give qualitative coherence to a field awash in decades of disconnected descriptions.
His model does not answer all geomorphological questions, but in its elegant simplicity, it still
holds pedagogical value.
Philip S. "Flip" Koch '78, a faculty member at the Colorado School of Mines professing in earth science
and finance, has ascended Mount Harvard multiple times.
LETTERS
Harvard
Facebook. The implication that it was only
Jr.) for an ascent of
HM
after the revelation of the inappropriate use
Mount Mitchell, the
of Facebook data by Cambridge Analytica
highest peak in east-
Visit harvardmag.com
ern North America
for additional letters.
Authors!
that it was necessary "to ask broader ques-
tions..." is not supported by the facts.
Yet their most
Were Faust and the members of the Cor-
lasting institutional contribution may have
poration and the Board of Overseers unaware
been as charter members of the Harvard
Miss the deadline for our
of the extremely numerous reports in widely
Travellers Club, established in 1902. Under
Holiday Reading List?
read publications over many years regard-
Davis's presidency, speakers discussed their
ing the cavalier attitude toward user privacy
explorations of sites from the South Pole to
of Facebook leadership (e.g./https://www.
Abyssinia. Dorr's home was the site of the
wired.com/story/facebook-a-history-of
club's second meeting-which continues to
WE CAN DO IT
mark-zuckerberg-apologizing/?mbid=Botto
convey their enthusiasm to this day.
mRelatedStories), in conjunction with evi-
RONALD H. Epp
dence that the company/leadership clearly
Farmington, Conn.
prioritized growth and profit over user wel-
In Peace
The Jaguars
fare despite protestations to the contrary?
Editor's note: Epp is the author of Creating
That
and Freedom
Drewl Our
Were the leaders of the University also un-
Acadia National Park: The Biography of George
eams
aware of the repeated/instances of Facebook
Bucknam Dorr.
COACH
having to "adjust" the numbers and meth-
STRANGLED
ods for publicly reported advertising metrics
AMERICAN TRUTHS
BULLDOG
(e.g., https://www.forbes.com/sites/great-
ACCORDING to Casey N. Cep's review of Jill
speculations/2016/11/17/more-bugs-found-
Lepore's These Truths: A History of the United
in-facebooks-ad-metrics-to-the-dismay-of-
States (September-October, page 64), the re-
advertisers/#48ffoabe2a85): One might have
vision from "these truths" being character-
thought that these widely reported and well-
ized as "sacred and fundamental" to 'self-
known realities would have weighed heav-
evident" meant that those rights were "the
ily against inviting Zuckerberg to deliver a
stuff of science" and not "the stuff of reli-
Advertise your book in the
commencement address at an institution that
gion... But the term "self-evident" precisely
Summer Reading List.
claims to prize, as its highest value, "veritas."
excludes scientific observation as the basis
NEIL GREENSPAN 75
of knowledge We cannot, through scien-
THE DEADLINE IS:
Shaker Heights, Ohio
tific inquiry alone. discover that all mean
MARCH 14, 2019
are "endowed by their Creator with certain
IDEOLOGICAL DIVERSITY
unalienable Rights. And the Creator puts
Reach 258,000 Harvard
REGARDING the letter from David W.
religion right back into the picture-if not
alumni, faculty, and staff.
Thompson in the September-October is-
organized religion. at the very least Faith.
sue (page 2) decrying the lack of ideologi-
Regardless I have the highest degree of
Your book ad will include:
cal diversity at Harvard, I wonder just how
admiration for Lepore and look forward to
a book jacket photo, your
easy it is to have ideological diversity on a
reading her book
name and Harvard class year,
university faculty when almost half of the
MICHAEL JORRIN '54
and a short description -
ideological spectrum in this nation does not
Ridgefield, Conn.
accept science, changes long-held beliefs
totaling 8 lines of text.
on a dime, and believes truth is not truth?
ERRATA
Your ad will appear both
JOHN T. HANSEN, LL.B. 63
A PRODCCTIONEROR mans-
in print and online.
San Francisco
posed the names of Charles
E. Gilberr IV and John F.
For information about pricing
VITAE
Kotouc both since of 2018
and ad specifications, go to:
WITHIN two years, profiles of George Buck-
Hunn Meteorial Schools
Charles E.
nam Dorr and William Morris Davis have
and Scholarships Awards
harvardmagazine.com/hauthors
Gilbert III
been published (September-October 2016,
in photo captions (Septem
contact Gretchen Bostrom
page 44; September-October 2018, page 44).
ber-Occupet page
at 617-496-6686, or e-mail
Neither profile mentioned the other alum-
In the paragraph
classifieds@harvard.edu.
nus by name, though their relationship was
of inte Shards Disso-
tight-especially in 1902 when Davis invited
name (September-Oc-
Dorr to join his scientific team to the Ameri-
tober page (a) the
TURNTO PAGE 62
can Southwest. Later that year Dorr returned
were missing from Michael
the favor by inviting Davis to join his com-
Schadleer's x
John F.
to browse the Holiday Reading List
panions (including Frederick Law Olmsted
We regist
Kotouc
6
NOVEMBER - DECEMBER 2018
Hanverd Magazine
16 June 2021
After completing the most recent of Chebacco (2021) devoted to the initial
logbooks documenting the efforts of "Captain" Charles Eliot to spend his
summer months with a select group of fellow Harvard undergrads. The
location was Mount Desert Island and the inquiries were scientific and
provided evidence that convinced this "Champlain Society"-initiated in
1880--that land conservation was necessity given the impact of tourism.
At this time the Charles and Mary Dorr family was living in Storm Beach
Cottage while their larger residence was being cionstructed on the Oldfarm
property in Bar Harbor. George B. Dorr had graduated from Harvard in 1874
and spent the next four years abroad, traveling with his parents throughout
Europe where he continued his studies at times independently of them.
Nothing in the Dorr Archive nor in the Champlain Society early notebooks
suggests interaction between Dorr and Eliot's student colleagues. To be sure,
travel between Bar Harbor and Northeast Harbor was difficult unless one
took to the sea. Yet it seems plausible that George might have been curious
about these Harvard investigators, especially since Harvard geology
instructor William Morris Davis spent a portion of the first two summers as a
Champlain Society investigator. The historical record to date provides no
evidentiary link during the early 1880's between Morris and Dorr. Two
decades later in 1902 Dorr joined a Morris-led team investigating the
geological character of the American Southwest.
I find this to be a provocative area for future research.
R.H. Epp
NATIONAL ACADEMY OF SCIENCES
OF THE UNITED STATES OF AMERICA
BIOGRAPHICAL MEMOIRS
VOLUME XXIII-ELEVENTH MEMOIR
BIOGRAPHICAL MEMOIR
OF
WILLIAM MORRIS DAVIS
1850-1934
BY
REGINALD A. DALY
PRESENTED TO THE ACADEMY AT THE AUTUMN MEETING, 1944
WILLIAM MORRIS DAVIS
1850-1934
BY REGINALD A. DALY
William Morris Davis won distinction as geologist, meteor-
ologist, and geomorphologist, but primarily as teacher. He made
personal, outdoor researches in every continent except Ant-
arctica, as well as in island groups of the Atlantic and the Pacific;
yet his international fame rests chiefly on his development of a
system of thought concerning the reliefs, the scenery, of our
planet. His system is the "American" system, but it is appli-
cable to the landscapes of the whole world. His early training
in geology led him to the principle by which he, more than any-
one else, has revolutionized the teaching of, and research on,
the endlessly varied forms of the lands and coastlines. To
geographers and geologists alike he was an apostle bringing
to them the gospel of method in research and method in the
presentation of the results of research. For him the root of
the matter is evolution, orderly development. Many geologists
had used this principle, so essential to understanding the protean
crust of the earth, but few geographers had used it in describing
land forms. Davis emphasized a mode of thinking and for its
expression he devised a system which has greatly appealed to
teachers and investigators in many foreign countries as well
as in the United States of America. While creating his de-
scriptive method in terms of evolutionary changes, he found
our English tongue sadly deficient. He had to create a new,
necessarily technical language. Every man of science knows
the difficulty of such an invention. Some of his verbal tools
Davis was able to adopt from the literature of earth science,
an immense literature which he thoroughly mastered; other vital
terms were his own. The combination has been put to construc-
tive use by geologists and geographers, foreign and domestic,
to an extent encouraging to our pioneer. He lived to see notable
improvement of geographical instruction in grammar school,
high school, college, and university improvement in the report-
ing of geographical and geological facts by staffs of the State
263
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
and Federal surveys; and improvement in the discussion of
"terranes" by the more philosophically-minded historians and
economists.
Knowing that even a long life could not vitalize all the dry
bones of the old geography, Davis specialized on physical geog-
raphy, leaving to others the problem of systematizing the in-
finitely varied responses of organisms to their environment.
This other half of geography needs today a clarifying leader
like Davis.
Davis was born in Philadelphia on February 12, 1850. At
that time his father, Edward M. Davis, a business man, and his
mother, Maria (Mott) Davis, were members of the Society of
Friends and fully shared the best characteristics and activities
of Quakers in full standing. Yet a hatred of injustice, which
was to be an outstanding emotion of their son, led them into
rebellion against one of the ironclad rules of the Society. Not
content with helping to operate the "underground railway" for
escaping slaves, Edward Mott enlisted in the Northern Army.
For this action he was expelled from the Society of Friends
and soon after his wife resigned from it. To both of them
the question of States' rights was quite subordinate to the prob-
lem of human freedom. To break with the Society's tradition
took courage of the kind shown in the remarkable life of
Lucretia Mott, the mother of Maria Mott.
Theodore Tilton called Lucretia Mott, born in Nantucket,
Massachusetts, "the greatest woman ever produced in this coun-
try." "She was the real founder and the soul of the woman's
rights movement in America and England. She was the out-
standing feminine worker in the struggle to rid our country
of slavery. She advocated labor unions in a day when they were
proscribed and generally considered illegal. She proscribed
war, and worked diligently for liberal religion." Her crusad-
ing force "had its source in the love of freedom of her seafaring
ancestry, and she feared opposition or the exploration of un-
charted regions of the mind no more than they feared to venture
into unknown seas" (quotations from Anita Moffett in the
New York Times Book Review, August I, 1937). That her
264
WILLIAM MORRIS DAVIS-DALY
some of the more dramatic and better understood processes that
mold the surface of our planet. But the young instructor knew
full well that effective, authoritative teaching of geology, the
principal subject of his first instructorship, demanded close
personal touch with Nature. To get such experience he selected
for field study in detail the Triassic formation of New England
and New Jersey. On those regions he published fifteen pre-
liminary papers (1882-1896), and a monographic summary of
most of his results in "The Triassic Formation of Connecticut"
(1898). This gave the first full account of the Triassic vol-
canic history of the region, announced criteria for proving the
extrusive character of some of the "trap sheets" and the in-
trusive character of others. He also showed how the analysis
of topographic forms could be used in explaining the under-
ground, invisible structures of Connecticut and similarly faulted
areas of the earth's crust.
While working on the complex history of the Triassic areas,
Davis interpolated field investigations: in Columbia County,
New York, and the Catskills, where he described the northward
continuation of the Appalachian structure; on the glacially-
formed drumlins of New England and other regions; on the
structure and origin of glacial sandplains and eskers; and on
the geological history of Mount Desert Island. In later years
he studied : the origin of the thick and widespread Tertiary
formations of the Rocky Mountain region, showing that these
are not lake beds, as had been generally assumed, but are flu-
viatile and alluvial-fan deposits; the origin and erosional history
of the Basin Ranges of the West; the development of the
Colorado Canyon; the mechanical conditions leading to the
formation of limestone caverns; and the nature of geological
proof, asking geologists "how do you know you are right?"-
a question that illustrated the fact that he was as much concerned
with the method of scientific thinking as he was in the majestic
happenings of earth history. Yet Davis must have been con-
scious that he made a principal contribution to the philosophy
of geology itself. His major contribution to earth science was
the conception of the "erosion cycle." He applied it to the
269
WILLIAM MORRIS DAVIS-DALY
Field Work in Physical Geography. J. Geog. I : 17-24, 62-9.
The New England States. Boston, Supplement to Frye's Complete
Geography. [Also 1895 edition.]
The Progress of Geography in the School. Chicago, pp. 49- (In National
Society for Scientific Study of Education. Ist Yearbook, Pt. II 7-49.)
River Terraces in New England. Harvard Coll. Mus. C. Z. Bull. 38
(g S 5) : 281-346.
Systematic Geography. Am. Ph. Soc. Pr. 4I: 235-59.
The Terraces of the Westfield River, Mass. Am. J. Sci. (4) 14: 77-94.
1903
The Basin Ranges of Utah and Nevada. (Abst.) J. G. II : 1201.
Block Mountains of the Basin-Range Province. (Abst.) Science n.s. 17:
301 ; G. Soc. Am. Bull. 14: 55I ; Eng. Mo. J. 75: 153.
The Blue Ridge in Southern Virginia and North Carolina. (Abst.) J. G.
II 121.
The Blue Ridge of North Carolina. (Abst.) Science n.s. 17: 220.
The Development of River Meanders. G. Mag. (4) IO: 145-8.
Effect of Shore Line on Waves. (Abst.) Science n.s. I5: 88; G. Soc.
Am. Bull. 13: 528.
An Excursion to the Plateau Provinces of Utah and Arizona. Harvard
Coll. Mus. C. Z. Bull. 42 (g S. 6) : I-50.
The Fresh-Water Tertiaries at Green River, Wyo. (Abst.) Science n.s.
17: 220-221 ; G. Soc. Am. Bull. 14 544; J. G. II 120.
The Mountain Ranges of the Great Basin. Harvard Coll. Mus. C. Z. Bull.
42 (g S. 6) : 129-77.
Practical Exercises in Physiography. J. Geog. 2: 516-20.
The Question of Seminars. Harvard Grad. Mag. pp. 8.
A Scheme of Geography. Geog. J. 22 413-23. London.
The Stream Contest Along the Blue Ridge. Geog. Soc. Phila. Bull. 3:
213-44.
Walls of the Colorado Canyon. (Abst.) Science n.s. 15: 87; G. Soc. Ain.
Bull. 13: 528.
1904
A Flat-Topped Range in the Tian-Shan. Appalachia IO: 277-84.
Glacial Erosion in the Sawatch Range, Colo. Appalachia IO: 392-404
Geography in the United States. Am. G. 33: 156-85; Am. Assn. Adv. Sc.
Pr. 53.
The Relations of the Earth Sciences in View of Their Progress in the
Nineteenth Century. J. G. 12: 669-87.
A Summer in Turkestan. G. Soc. Am. Bull. 36: 217-28.
1905
The Bearing of Physiography Upon Suess' Theories. Am. J. Sci. (4) 19:
265-73; (Abst.) Int. Cong. Geog. VIII, Rp. 164.
293
MAY 18, 1934
SCIENCE
445
other could be detached by procedures which leave
valeric aldehyde and on the other the phenylureide of
the normal peptide linkage intact.
glycylalaninamide. The original leucine has thus been
L. Zervas and I have worked out such a method,
split off in the form of the easily identifiable aldehyde
which I should like to illustrate by the simplest ex-
containing one less carbon atom.
ample which we have studied, namely, the tripeptide,
The remaining substituted peptide-amide can now
glycyl-1-alanyl-l-leucine. The first step is to block the
be further treated with an equivalent amount of hy-
free amino group by substitution. As a substituent
drazine, again converted into a peptide-hydrazide and
we chose in the first place phenyl-isocyanate and pre-
through the azide with benzyl alcohol into the benzyl-
CH2 CO-NH. CH (CH3) CO-NH CH C,H
NH2
COOH
CH2 CO-NH. CH (CH3) .CO-NH CH C.H.
C.H..NH.CO.NH
COOH
CH2 CO-NH. CH (CH3 CO-NH.CH.CH,
C.H.NH.CO.NH
CO.N3
CH2 CO-NH. CH (CH3) CO-NH.CH. C,H
C.H..NH.CO.NH
H2
NH CO O CH2 . C.H
CH2 CO NH CH (CH3) CO-NH2
CH C,H
||
C,H3 .NH.CO.NH
O
NH2 I CO2 CH. C.H5
-CO NH. NH2
etc.
pared a phenylureide of the tripeptide. By thus
urethane, etc.; the alanine is finally split off as acetal-
neutralizing its basic function the tripeptide is con-
dehyde and can thus be easily identified. In this
verted into a true acid: from this the methyl ester
manner we are able to break down a peptide chain
can be prepared under very mild conditions with the
step by step from the carboxyl end obtaining the
aid of diazomethane The ester is treated with the
successive amino-acids in the form of easily recog-
equivalent amount of hydrazine to yield the hydrazide
nizable derivatives.4
which in turn is converted according to the method of
The above work was undertaken in view of the
Curtius into the azide. Such azides on treatment
with alcohols readily yield urethanes. The essential
urgent need of improved analytie and synthetic meth-
point of our method consists in the fact that we choose
ods for the study of proteins and proteolytic enzymes.
benzyl alcohol and thus obtain a benzyl-urethane.
Now that some progress has been made in this direc-
Now we hydrogenate catalytically this urethane and
tion a general plan of attack on the problems of pro-
are able to obtain on the one hand toluene and iso-
tein constitution lies at hand.
OBITUARY by Douglas Johnson.
WILLIAM MORRIS DAVIS
before the Boston meeting of the American Associa-
ON the fifth of February last (there closed a life
tion for the Advancement of Science. When he lay
which profoundly affected the development of two
down to rest his writing table was filled with work
earth sciences, geology and geography. For more
actively in progress.
than half a century William Morris Davis was a
(Professor Davis enriched the science of geology by
distinguished leader in these related fields. At the
a long succession of able papers based on original
end of this period he possessed, in his eighty-fourth
studies covering a remarkable range of subjects. In
year, the same enthusiasm of purpose, the same
1882 there began a series of fifteen articles and mono-
flexibility of mind, the same penetrating powers of
graphs on the Triassic formations of the Connecticut
reasoning which made his career remarkable in the
Valley, out of which came our first full knowledge
annals of American science. Only a few weeks before
his death he crossed the continent during an excep-
4 This process can no doubt be successfully applied to
tionally severe winter to deliver the Maiben lecture
other classes of compound. Its application to sugars and
saccharides is contemplated.
This content downloaded from 137.49.124.119 on Mon, 15 Oct 2018 14:42:44 UTC
446
SCIENCE
VOL. 79, No. 2055
of the intrusive and extrusive trap sheets of this
processes, acting on geological structures, through
region, our first recognition and location of many
recent geological time.
oblique faults traversing the formations and our first
Davis's "Geological Dates of Origin of Certain
satisfactory understanding of the extent to which
Topographic Forms on the Atlantic Slope of the
topographic form could be utilized in unraveling
United States" was for a quarter century the funda-
faulted structures. To this early period belong papers
mental paper on which correlation of geomorphic
on details of Appalachian structure in the Hudson
features in this region rested, and is to-day fre-
Valley, which extended northward the known area of
quently quoted. His papers on southern New En-
typical Appalachian folding and gave us a clearer
gland, in which the scheme of the fluvial erosion cycle
conception than we had before possessed of the classic
is carried to its ultimate stage in the peneplanation
unconformity at Becraft Mountain, A series of
of a vast area of resistant crystalline rocks, present
papers on the distribution and origin of drumlins,
a wholly novel interpretation of the later geological
on glacial erosion, on lakes and valleys, gorges and
history of the region in question, an interpretation
waterfalls and on the origin of cross-valleys laid the
which in its main outlines is still accepted. Davis
foundation of his later geomorphic studies.
makes clear the fact that he did not originate the idea
In 1884 Davis published a short paper on the
of land reduction to baselevel; but he gave name to
classification of plains, plateaus and their derivatives
a conception which had not previously gained wide
which contains the first published statement of the
currency, and SO effectively pictured the process of
scheme of the erosion cycle, and which may therefore
land-form evolution by orderly, sequential stages that
be held to mark the beginning of the modern concep-
the idea of fluvial peneplanation spread rapidly
tion of land-form evolution. At this same early
throughout the world. In Great Britain the novel
period, in a report on the relation of the coal of
American conception encountered the firmly estab-
Montana to older formations, Davis recognized the
lished theory of marine abrasion set forth by Ramsay
extensive degradation to which the Great Plains pro-
nearly half a century before; but largely through
vince had been subjected, and began developing work
the influence of Davis's pen the American view
on the physical history of rivers which was to cul-
gradually gained a place for itself. In France prog-
minate in 1889 and 1890 in two brilliant essays: one
ress was more rapid, while in Germany acceptance of
on "The Rivers and Valleys of Pennsylvania," the
the new idea was aided when Davis by field studies
other on "The Rivers of Northern New Jersey."
demonstrated peneplanation of the Hunsrück border-
These essays, highly original in both content and
ing the gorge of the Rhine. Into central Asia Davis
method, are remarkable for their close analysis of
carried the new conception of land evolution by
the influence of geologic structures upon stream de-
demonstrating the peneplaned character of uplifted
velopment at successively lower horizons in strongly
and tilted blocks of the earth's crust in Tian Shan.
folded regions. Although they appeared but a decade
Later we find him in South Africa, where he was the
after Davis's first published work, they exhibited such
first to discover and describe the peneplane of the
a mastery of deductive reasoning and such profound
high veldt and the baselevelling of the Cape Colony
knowledge of the effects of geologic processes upon
ranges. Thus not by his pen alone, but by appro-
complex geologic structures that they remain to-day
priate field studies in four continents, Davis carried
much-quoted classics of American geology.
a great American idea to every quarter of the globe.
With the year 1890 began a steady flow of impor-
To him, more than to any other, is due the fact that
tant papers from Davis's skilful pen which at the
in almost every country where geological studies are
time of his death, nearly half a century later, con-
prosecuted to-day, the investigator dates a long series
tinued unabated. It is not possible, within reasonable
of major geological events in terms of ancient erosion
space, to do more than indicate contributions of ex-
planes.
ceptional importance. The remarkable versatility of
Nor were Davis's foreign studies confined to the
Davis's mind, and the breadth of his interests, is
problem of peneplanation. In France, Switzerland
evidenced by papers, monographs and books of a
and Norway he threw needed light on the moot ques-
geographical, meteorological and pedagogical char-
tion of glacial erosion. British geologists find in his
acter; but we shall for the most part confine our
work on Mount Snowdon the most systematic discus-
attention to the field in which his chief labors lay,
sion of alpine glacial erosion in their country; and in
geomorphology. His preparation and training were
his studies of English rivers a new and fertile treat-
mainly in the field of geology; he drew his inspiration
ment of stream adjustments in successive erosion
primarily from the great geologists of the early sur-
cycles. In France we look to Davis for the earliest
veys-Powell, Dutton, Gilbert; and his life work has
account of the extensive drainage modifications on
chiefly been concerned with the study of geological
structures of the Paris basin. A study of Permian
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MAY 18, 1934
SCIENCE
447
glaciation in South Africa presents evidence that the
and a volume indispensable to future workers in this
ice could not have had its source in a mountainous
field.
region, while an account of folded mountains in the
We have touched but a limited portion of Davis's
same continent traces the evolution of ranges of the
record of scientific productivity. It is
a
record
truly
Appalachian type. Similarly, in other countries we
remarkable for breadth of field covered, for penetrat-
find his significant contributions to geomorphology in
ing analysis of the problems treated, for quantity of
studies of fault phenomena, continental platforms,
new facts first established, for freshness and vigor of
shoreline evolution and other problems.
methods employed, and for number of novel and
(No reference to Davis's shoreline studies can be
fruitful
ideas
contributed.
His
notable
achievements
complete which does not record the fact that his con-
in geomorphic research evidence a creative mind of
tributions in this field opened a new era in shoreline
high order whose talents were long and industriously
investigations.) He closed the door on the old, em-
devoted to the service of science. Such achievements
pirical methods of shoreline description, and pointed
could not fail to have a profound influence upon the
the way to a genetic study of the effects of marine
development of both geology and geography. It is
processes on variable geologic structures. He showed
impossible to measure the full extent of that influence;
that there was a cycle of marine erosion just as truly
but it is easy to point to evidences of its far-reaching
as there were cycles of stream erosion and of glacial
character and to indicate some of the ways in which
erosion. Every modern account of shoreline evolution
it has operated.
is a tribute to the genius of William Morris Davis.
By his writings Davis practically created a new
In earlier paragraphs emphasis has been placed
branch of geology, physiographic geology or geo-
especially on Davis's original ideas, and only inciden-
morphology. Men have, of course, long given atten-
tally on work which followed the lead of others. But
tion to the visible manifestations of geologic proc-
even where he was not a pioneer Davis made note-
esses, and great contributions in this field are asso-
worthy contributions to geomorphology.
In
the
ciated with the names of Hutton and Playfair, Lyell,
Grand Canyon region he was first to discover that
Geikie and Ramsay, DeLapparent, LaNoë and De-
the major faulting antedated the "Great Denudation"
Margerie, Von Richthofen and Penck, Powell, Dutton
of Dutton, that the Esplanade had a structural and
and Gilbert. But it was Davis who codified the work
not a cyclic origin, and that the Colorado was not
of these masters into a definite science, unified and
necessarily an antecedent stream but might more
vivified by a wholly new conception the orderly evo-
reasonably be interpreted as superposed from a
lution of landforms through systematic stages of
course determined by geologic structures.) In a
development. (It was he more than any other who
notable series of papers on fault block mountains, he
gave precision to this new branch of geology by a
confirmed and extended ideas earlier promulgated by
large body of critical work, and it was he who had
Gilbert, and cast the study of these forms into an
the largest share in creating an "American School"
entirely new mold by developing to an unprecedented
of geomorphology and giving to it international
degree the value of physiographic evidence of fault-
prestige.)
ing. His paper on "The Sculpture of Mountains by
By individual studies of high excellence in many
Glaciers" has been widely quoted because of its artis-
foreign lands and by field discussions with foreign
tically eloquent and scientifically convincing com-
investigators on their own territory, Davis initiated a
parison of forms found in non-glaciated mountains
large volume of work in other countries. Thus by
and in formerly glaciated mountains of similar alti-
personal example and oral teaching he supplemented
tude. To him we owe our first full understanding of
the labors of his pen in carrying the doctrine of
the relation of rock defense to the positions and pat-
land-form evolution throughout the world. In Europe
terns of river terraces, imperfectly appreciated by
a great range of geomorphic studies traces its inspira-
earlier writers. (He added new evidence in support
tion directly to him. In Asia his studies of the Tian
of the fluviatile origin of the fresh-water Tertiaries
Shan peneplanation were fruitful in later studies
of the Rocky Mountain region, broadened our under-
widely extending his original ideas. The South Afri-
standing of erosion in the Front Range of the
can geologists base the later geologic chronology of
Rockies, enriched by field studies our knowledge of
their region on Davis's study of the high veldt, and
desert rock planes in the Southwest, and gave us our
describe the evolution of their terrain in terms of his
first detailed comparison of such planes with those
theories of land-form evolution. It is doubtful
of humid regions.) Following the lead of Darwin and
whether any other American geologist or geographer
Dana in the coral reef problem he visited thirty-five
is so frequently quoted over so great a proportion of
reef-encircled islands of the Pacific, and on the basis
the world's surface.
of years of study published a long series of articles
In the development of any science the rôle of the
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448
SCIENCE
VOL. 79, No. 2055
critic is an important one. There can be no doubt work on the physiography of the lands. His vision
that in this capacity Davis has rendered great ser-
of the field of geography was thus broad as well as
vice to the related sciences of geography and geology.
penetrating.
His many published reviews of geomorphic work at
It was not surprising that Davis's well-equipped
home and abroad not only kept workers in this field
and disciplined mind should bring about a great
in touch with the progress of events, but by their
awakening in American geography. In a long series
penetrating and constructive criticisms pointed the
of papers on the teaching of geography he laid the
way to higher achievement. Davis was a crusader in
foundations for a new conception of the subject in
the holy war against archaic theories and careless
which scientifically organized content and scientific
thinking; and if with the crusader's enthusiasm for a
methods of instruction should replace a conglomera-
cause he sometimes handled his lance with pitiless
tion of facts empirically presented. (In lectures to
skill, the victims have usually lived to forget the pain
teachers of geography, in training future teachers in
of criticism in the pride of work yet more skilfully
his university classes and seminars, in founding the
accomplished. Geomorphology has not yet outgrown
Association of American Geographers, and in organ-
the faults inherent in the youth of any science; but
izing local and international geographical excursions
few will doubt that its achievements are greater in
he spread the doctrine of a new geography which
quantity and higher in quality because of the analyti-
should be as truly scientific in content and method
cal mind and critical powers of William Morris Davis.
as were its sister sciences.) Although late in life he
(Truly great teachers have ever exerted a profound
wrote that he would not class himself as a geographer,
influence upon the growth of a science; and as a
he is known throughout the world as one of the great
teacher Davis was truly great. Through disciples in
leaders in this field, one who inspired new life in the
this and other lands who sat under his instruction in
geography of his own country and profoundly affected
the university, or listened to his teachings in the
the course of geographic progress in others.
field, or knew him only through the printed page,
The extraordinary accomplishments of William
Davis has exerted incalculable influence. In the pub-
Morris Davis for the sciences of geology and geogra-
lications of federal and state surveys, in the class
phy won cordial recognition from his colleagues in
work of universities at home and abroad, in the
both fields. The Geological Society of America be-
changed scope and emphasis of text books of geology,
stowed on him its two highest honors: the presidency
the effects of his teachings are strikingly apparent.
of the society and the Penrose Gold Medal. The
In SO minor a matter as the method of illustrating
Association of American Geographers placed him
relations of geologic structure to topographic form
twice in the presidency, the American Geographical
by block diagrams, one can trace his growing influence
Society awarded him its Cullum Geographical Medal,
in the geologic literature of many countries. And
the National Council of Geography Teachers its Dis-
this is but symptomatic of the deeper influence which
tinguished Service Award. Twice the British Asso-
has transformed the substance of geomorphic litera-
ciation for the Advancement of Science made him
ture in every land. Not only in English, but also in
an honored guest, once in South Africa and once in
German and in French he has carried his teachings
Australia. Twice he was called as exchange professor
to foreign lands both in lectures and in writings.
to foreign lands, spending one year in Berlin and
To-day one of the best advanced treatises on geo-
one year in Paris, in each case lecturing in the lan-
morphology is his "Erklärende Beschreibung der
guage of the nation to which he was accredited. He
Landformen," published in Leipzig and Berlin.
was the recipient of many medals for signal service
It is not easy to determine whether the geologist
in geologic and geographic fields, held honorary doc-
or the geographer is most greatly in his debt, but
torates from four foreign universities in three dif-
there can be no doubt that Davis profoundly affected
ferent continents and was elected to honorary mem-
the development of geography as he did that of geol-
bership in the scientific societies of a dozen countries.
ogy. For high accomplishment in the geographic
Few men whose honors came solely as the result of
field he was admirably prepared first by training in
individual scientific labors, and in no degree as execu-
astronomy, and practical work in the National Ob-
tives or other official representatives of great insti-
servatory at Cordoba, Argentina, where he discovered
tutions or societies, have been accorded such world-
several new variable stars; then by many years of
wide distinction.
research and teaching in the field of meteorology,
(Among those who knew him intimately the memory
bearing fruit in a text book in this subject remarkable
of Davis the man will be treasured. His Quaker
for clarity and logical presentation of matter, and a
ancestry was perhaps responsible for a certain rigid-
series of original papers which won for him election
ity of discipline and a relentlessness in his antagonism
as corresponding member of the German Meteorologi-
to careless thinking which made him a severe master
cal Society; and finally by his still more abundant
and an uncomfortable opponent.) But those who could
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MAY 18, 1934
SCIENCE
449
endure the discipline and place high value on criticism
of the man who was his most vigorous critic. Be-
as helpful as it was keen, found in Davis a loyal
neath a brilliant and incisive intellect beat a warm
friend. He told a man his faults, but told others his
heart capable of strong affection, whether for a great
virtues. Many a student and younger scientific col-
master like Gilbert or for his own disciples of a
league has learned to his surprise of opportunities
younger generation.
opened to him by the quiet but effective intervention
DOUGLAS JOHNSON
SCIENTIFIC EVENTS
PEAT INVESTIGATIONS AT THE INTERNA-
cured from the chairman of the National Section, Dr.
TIONAL CONGRESS OF SOIL SCIENCE
A. G. McCall, U. S. Bureau of Chemistry and Soils,
THE projected arrangements for the third Interna-
Washington, D. C. Manuscripts and reports for the
tional Congress of Soil Science, to be held at Oxford,
congress are to be sent to Dr. R. V. Allison, at the
England, from July 30 to August 6, 1935, include a
same address.
program of the Subcommission for Peat Soils.
As at the previous congress, the interests of Amer-
THE RAINBOW BRIDGE-MONUMENT
ican members will find expression in the organization
VALLEY EXPEDITION
under the chairmanship of Dr. A. G. McCall, the rep-
AN expedition to continue exploration of the Rain-
resentative of the United States National Section, and
bow Bridge-Monument Valley area on the Utah-Ari-
Dr. R. V. Allison, chairman of the regional committee.
zona border, one of the few Mittle-known large areas
The outstanding part of the program is to be a
remaining in the United States, will leave New York
major theme dealing with the comparative study of
on June 28 under the direction of Ansel Franklin
"low moor" peat land from the standpoint of morpho-
Hall, chief forester of the National Park Service.
logical profile features and the influence of drainage
According to an announcement in The New York
on the physical, chemical and biological properties of
Times, the tract to be visited, about three thousand
peat soils. Regional examples will be drawn upon to
square miles in extent, is known from exploration last
establish an agreement on methods and technique. The
year to contain interesting archeological, biological
contributions will be summarized in a paper of 30
and other data. Its scenic features have led to dis-
minutes' duration, to be read at a plenary session of
cussion of the area as a national park.
the congress, and to be followed by general discussion.
Last year's expedition, under the leadership of Mr.
In addition there will be sessions open to papers
Hall, mapped the principal features of the area, but
and discussions on various subjects in peat investiga-
did not succeed, in the time at its disposal, in reach~
tions, such as surveys performed by government bu-
ing the less accessible parts, many of which are be-
reaus of different countries, cartographic work and
lieved never to have been seen by a white man. A
aerial photography, ecological and geographic rela-
few Piute Indians, who are being made the basis of
tionships, changes in climate since postglacial times,
an ethnological study, live in the area.
localization of peat industries, problems connected
Professor Charles Del Norte Winning, of New
with the various uses of peat land resources, highway
York University, has been appointed associate field
construction and amelioration.
director. He will be accompanied by about thirty
Another question to be discussed is the classification
specialists. Fifteen of these have already been ap-
of peat soils and the terminology required to express
pointed. Additional members will include biologists
new concepts. Lacking any authoritative standard, it
or specialists in particular fields of biology, such as
is hoped that a tentative statement may be presented
herpetology or ornithology, and architects and artists
to the commission for approval.
to survey and sketch Indian cliff and mound dwellings,
It is deemed desirable to stress American attendance
of which several have been discovered.
and participation in the program. The session is open
Besides Mr. Hall and Professor Winning, the staff
to any person engaged in some field of peat investiga-
as selected to date includes Gerald E. Marsh, of the
tion or interested in its practical application. The
University of California; John Wetherill, custodian
British government has taken official cognizance of
of the Navaho National Monument; John E. Arm-
the International Congress of Soil Science and has in-
strong, of the University of California; Dr. Herbert
vited the United States government to be represented
E. Gregory, of Yale University, director of the Bishop
by a limited number of delegates. Attention is di-
Museum, Honolulu; Professor N. E. A. Hinds, of the
rected also to the fact that during the congress facili-
University of California; Thorne E. Mayes, engineer
ties will be afforded to visit historic places, and that
of the General Electric Company, and Lyndon L.
immediately after the congress there will be a three-
Hargrave, archeologist.
weeks tour of England, Wales and Scotland.
As was the case last year, the expedition is financed
Blanks for membership in the congress may be se-
by its members, each being assessed $398. The field
This content downloaded from 137.49.124.119 on Mon, 15 Oct 2018 14:42:44 UTC
THEME: Americans at Work
Form No. 10-300 (Rev. 10-74)
SUBTHEME:
"
ence and Invention"
UNITED STATES DEPART ENT OF THE INTERIOR
FOR NPS USE ONLY
NATIONAL PARK SERVICE
RECEIVED
NATIONAL REGISTER OF HISTORIC PLACES
INVENTORY -- NOMINATION FORM
DATE ENTERED
SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS
TYPE ALL ENTRIES -- COMPLETE APPLICABLE SECTIONS
1
NAME
HISTORIC
William Morris Davis House
AND/OR COMMON
17 Francis Street
2
LOCATION
STREET & NUMBER
17 Francis Street
NOT FOR PUBLICATION
CITY, TOWN
CONGRESSIONAL DISTRICT
Cambridge
VICINITY OF
8th
STATE
CODE
COUNTY
CODE
Massachusetts
75
Middlesex
017
3
CLASSIFICATION
CATEGORY
OWNERSHIP
STATUS
PRESENT USE
DISTRICT
PUBLIC
OCCUPIED
AGRICULTURE
MUSEUM
BUILDING(S)
PRIVATE
UNOCCUPIED
COMMERCIAL
PARK
STRUCTURE
BOTH
WORK IN PROGRESS
EDUCATIONAL
PRIVATE RESIDENCE
SITE
PUBLIC ACQUISITION
ACCESSIBLE
ENTERTAINMENT
RELIGIOUS
OBJECT
IN PROCESS
YES: RESTRICTED
GOVERNMENT
SCIENTIFIC
BEING CONSIDERED
YES: UNRESTRICTED
INDUSTRIAL
TRANSPORTATION
NO
MILITARY
OTHER
4
OWNER OF PROPERTY
NAME
Francis M. Shea
STREET & NUMBER
17 Francis Street
CITY, TOWN
STATE
Cambridge
VICINITY OF
Massachusetts
5
LOCATION OF LEGAL DESCRIPTION
COURTHOUSE
Middlesex Registry of Deeds--Southern District
REGISTRY OF DEEDS, ETC
STREET & NUMBER
3rd and Ottis Streets
CITY, TOWN
STATE
Cambridge
Massachusetts
6
REPRESENTATION IN EXISTING SURVEYS
TITLE
None
DATE
FEDERAL
STATE
COUNTY
LOCAL
DEPOSITORY FOR
SURVEY RECORDS
CITY, TOWN
STATE
15
7
DESCRIPTION
CONDITION
CHECK ONE
CHECK ONE
X
XEXCELLENT
DETERIORATED
UNALTERED
ORIGINAL SITE
GOOD
RUINS
ALTERED
MOVED
DATE
_FAIR
(unrestored)
UNEXPOSED
DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE
The William Morris Davis House in Cambridge, Massachusetts, is a frame, 2 story
gabled roof house with a gambreled roof wing. The exterior is sheathed in
shingles. The main entrance is located on the side of the house and there is
also a rear entrance. The front elevation is characterized by an irregular or
assymetrical window arrangement and a columned porch at the entrance. An end
bay window faces the street.
The date of construction and the builder are unknown. The use of shingles as
covering indicates that the-house belongs to what the authors of the Cambridge
Historical Commission's Old Cambridge (1973) call the "shingle style" of the
Queen Anne movement in Cambridge. This would indicate that the house was
probably built in the 1890's. Old Cambridge does not note 17 Francis Street
as a distinguished illustration of the "shingle style." In itself the
building appears to be of no particular architectural significance.
17 Francis Street was the home Willima Morris Davis lived in from approximately
1898, the time he was appointed to the Sturgis-Hooper Professorship at
Harvard, until 1916. It was during this period that Davis performed some of
his most productive work in geography.
17 Francis Street retains an integrity of association with the Davis period.
The building has undergone no significant exterior alterations since its
construction. The basic interior floor plan is also intact with the exception
that the present owner has installed an apartment on the third floor. The
structure continues to function as a private residence.
8
SIGNIFICANCE
PERIOD
AREAS OF SIGNIFICANCE -- CHECK AND JUSTIFY BELOW
_PREHISTORIC
ARCHEULOGY-PREHISTORIC
COMMUNITY PLANNING
LANDSCAPE ARCHITECTURE
RELIGION
_1400-1499
ARCHEOLOGY-HISTORIC
.CONSERVATION
_LAW
SCIENCE
__1500-1599
AGRICULTURE
ECONOMICS
LITERATURE
SCULPTURE
_1600-1699
ARCHITECTURE
EDUCATION
_MILITARY
SOCIAL/HUMANITARIAN
1700-1799
ART
LENGINEERING
MUSIC
THEATER
1800-1899
COMMERCE
LEXPLORATION/SETTLEMENT
_PHILOSOPHY
_TRANSPORTATION
1900-
LCOMMUNICATIONS
INDUSTRY
POLITICS/GOVERNMENT
_OTHER(SPECIFY)
INVENTION
SPECIFIC DATES
1898-1916
BUILDER/ARCHITECT
unknown
STATEMENT OF SIGNIFICANCE
William Morris Davis was born February 12, 1850, in Philadelphia. His father was
a successful Philadelphia businessman and young Davis grew up in comfortable and
secure surroundings. His early education was typical of the period. His mother
taught him at home until he was eleven at which time he entered a private school.
In 1866 at age 16 Davis enrolled at Harvard's Lawrence Scientific School. In
1869 he earned a bachelor of science degree magna cum laude and a year later he
received an engineering degree. Although Davis early displayed a high aptitude
for scientific and engineering subjects, he returned to Philadelphia in 1873
and entered his father's business. The life of a businessman soon proved
unsatisfactory to the young man and in 1876 Davis returned to Harvard to pursue
the study of geology under Nathaniel S. Shaler. In 1877-78 he took a trip
around the world studying geological formations and meeting his colleagues in
other countries. Upon his return Davis was appointed an instructor of geology
at Harvard. The appointment marked the beginning of a teaching career at
Harvard that lasted until 1912. Davis' academic career was highly successful
and reached its high point in 1898 when he was appointed to the Sturgis-Hooper
Professorship of Geology. In 1912 Davis resigned from the Harvard faculty.
His elevation to emeritus status did not mean the end of his research, writing,
and active participation in geological and geographical circles. According to
Herman R. Friss, Davis' biographer in the Dictionary of American Biography,
it was during the 36 years between his appointment as Sturgis-Hooper professor
in 1898 and his death in 1934 that Davis,
"
profoundly affected the science
of geology and geography.
After his retirement from Harvard, Davis traveled widely at home and abroad.
In 1908-09 and again in 1911-12 he taught in Germany and France. Upon returning
home in 1912 he lead a cross country excursion of leading American geologists
and geographers. During World War I Davis served as chairman of the geography
committee of the National Research Council. Beginning in approximately 1924
his interest centered on California where he studied oceanography and coral
formations and lectured at various universities. Davis was active until the
end of his life. He died on February 5, 1934, at Pasadena during the National
Academy of Science annual meeting.
Herman R. Friss, "William Morris Davis," Dictionary of American Biography,
21, (New York, 1944), p. 230.
16
(Continued)
9
MAJOR BIBLIOGRAP CAL REFERENCES
Reginald A. Daly, "William Morris Davis, 1850-1934," National Academy of
Science Biographical Memoirs, 23, (Washington, 1945).
Herman R. Friss, "William Morris Davis," Dictionary of American Biography, 21,
(New York, 1944).
New York Times, February 7, 1934.
10 GEOGRAPHICAL DATA
ACREAGE OF NOMINATED PROPERTY less than one acre
UTM REFERENCES
A
19 3:26 155
4494030
B
ZONE EASTING
NORTHING
ZONE
EASTING
NORTHING
C
D
VERBAL BOUNDARY DESCRIPTION
LIST ALL STATES AND COUNTIES FOR PROPERTIES OVERLAPPING STATE OR COUNTY BOUNDARIES
STATE
CODE
COUNTY
CODE
STATE
CODE
COUNTY
CODE
11 FORM PREPARED BY
NAME/TITLE
James Sheire, Historian
ORGANIZATION
DATE
Historic Sites Survey, National Park Service
July 1975
STREET & NUMBER
TELEPHONE
1100 L Street NW.
202-523-5464
CITY OR TOWN
STATE
Washington
D.C.
12 STATE HISTORIC PRESERVATION OFFICER CERTIFICATION
THE EVALUATED SIGNIFICANCE OF THIS PROPERTY WITHIN THE STATE IS:
NATIONAL
X
STATE
LOCAL
As the designated State Historic Preservation Officer for the National Historic Preservation Act of 1966 (Public Law 89-665). I
hereby nominate this property for inclusion in the National Register and certify that it has been evaluated according to the
criteria and procedures set forth by the National Park Service.
FEDERAL REPRESENTATIVE SIGNATURE
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DATE
FOR NPS USE ONLY
I HEREBY CERTIFY THAT THIS PROPERTY IS INCLUDED IN THE NATIONAL REGISTER
DATE
DIRECTOR, OFFICE OF ARCHEOLOGY AND HISTORIC PRESERVATION
ATTEST
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KEEPER OF THE NATIONAL REGISTER
19
Form No 10-300a
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UNITED STATES DEPARTMENT OF THE INTERIOR
FOR NPS USE ONLY
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DATE ENTERED
INVENTORY -- NOMINATION FORM
William M. Davis House, Mass.
CONTINUATION SHEET
ITEM NUMBER
8
PAGE 2
William Morris Davis' significance in the history of science in America rests in
his contributions to meterology, geology, and gemorphology. In over 500 books
and periodical publications he created a body of work in the earth sciences that
mark him as an outstanding American scientist.
In 1894 Davis published Elementary Meteorology. Although the work, which was
essentially a textbook, did not contain any new basic science knowledge, it
did bring organization and refinement to a large body of previously uncoordinated
knowledge. Elementary Meteorology became the standard textbook on the subject
for many years.
Davis' international fame as a creator of new knowledge rests chiefly on his
contributions to geology and geomorphology. In 1912, after he had resigned from
Harvard and while teaching in Germany, Davis published Die erklaerende
Beschreibung der Landformen (A Reasoned Description of Landforms) The
work
represented a summation of Davis' forty year study of the shape of the earth
and the evolution of the earth's forms. Employing the knowledge of meteorology,
geography, and geology Davis offered an explanation of the genesis, development,
EADin
v
and classification of landforms. His system, which could be applied to the
Eopography of the entire earth, became known as the Davisian or American school
of geomorphological thought. In this work and subsequent studies Davis created
6
new doctrines and concepts (for example the concept of "erosion cycle") to
explain the shaping and forming of the earth. In so doing he opened new areas
of study for geologists and geographers. According to Reginald A. Daly, the
distinguised geologist, Davis transformed the study of geography in America into
a true earth science.
Davis' contributions to the earth sciences earned him the esteem and recognition
of his peers. Among his awards were the Cullum Medal of the American
Geographical Society (1903), the Academy of Natural Sciences' Hayden Medal,
and the Patron's Medal of the Royal Geographical Society. Leading scientific
societies both here and abroad, among them the National Academy of Sciences,
the American Association for the Advancement of Science, and the Deutsche
Meteorologische Gesellschaft, elected him to membership.
Page 1 of 4
William Morris Davis
No Erosion of Impact
Personal Life History- William Morris Davis was born in Philadelphia, Pa., on February 12, 1850. He died in
Pasadena, CA., on February 5, 1934. He was the son of Edward M. Davis and Martha Mott Davis, who were
both members of the Society of Friends. His father a Philadelphia businessman, was expelled from the society
for enlisting in the Union army during the civil war. His mother was the daughter of Lucretia Mott an early and
strenuous worker for women's rights and a firm antagonist of slavery. His mother resigned her post on the
society shortly after the expulsion of her husband from the group.
In 1879 Davis married Ellen B. Warner of Springfield Massachusetts. After her death he married Mary M.
Wyman of Cambridge, Massachusetts in 1914. After her death he married Lucy L. Tennant of Milton,
Massachusetts in 1928. She miraculously survived him.
Academic History- Davis' contributions cover the separate field of geography, geology, and meteorology. He
had an emphasis throughout his career on education in both the high school level as well as the college level.
Davis' most influential concept was the "cycle of erosion". He worked on refining and detailing this concept for
most of his professional career. Many of his early publications layed the foundation for this concept but it is the
essay "the rivers of pennsylvania,1889" where he first states and defines the concept.
It is clear that Davis was influenced by Darwin's organic evolution theory. In a 1883 writing he states "it seems
most probable, that the many pre-existent streams in each river basin concentrated their water in a single
channel of overflow, and that this one channel survives- a fine example of natural selection."
He is noted in bibliographies reviewed that he was an avid sponsor of bringing professionals together. This is
supported most notable by his involvement as one of the founders of the Association of American Geographers.
Something of which I have been puzzled over however is the lack of mention of his involvement with the
National Geographic Society(NGS). He is given credit as having an article or essay in the NGS magazine in
each of its first nine years. Also these articles seem to have been some of his preeminent, most influential
works. He is also listed as one of the original members of the NGS.
Honorary Degrees from: The Cape of Good Hope University 1905; Greifswald University 1906; Christiana
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University(Oslo) 1911; Melbourne University 1914. Was decorated Chevalier Legion of Honor(France) 1912.
Memberships/Leadership in Organizations: Founding member of Geological Society of America(pres. 1906 &
1911); Founding member of Association of American Geographers(pres. 1904,1905,1909); member of
American Academy of Arts and Science; member of American Philosophical Society; Member National
Academy of Sciences; member Imperial Society of Natural History(Moscow); member of the New Zealand
Institute; Science and America(asso Editor); member American Association for the Advancement of Science
(v-pres. 1903) Geographical Societies of: Berlin, Vienna, Madrid, Rome, Buda-pest, Leipzig, Greifswald,
Frankfurt, Geneva, Petrograd, Amsterdam, Neuchatel, Copenhagen, Stockholm, New York and Chicago. The
total list of is memberships honorary and otherwise is well over thirty memberships strong. He is also listed as
having 501 titles in his bibliography with dates spanning between 1880 and 1938.
Professional Time Line
1869- Bachelor of Science degree from Harvard University(Lawrence Scientific School)
1870- Master of Engineering from Harvard University
1870- Spends three years at Cordoba, Argentina as meteorologist in national observatory
1874-Assistant to Raphael Pumpelly on the Northern Pacific Survey
1877- - Assistant to Nathaniel Shaler professor of geology at Harvard University
1879-Instructor of geology at Harvard University
1882&1911 - Lecturer Lowell Institute
1883- Assistant geologist Northern Transcontinental Survey
1885-Appointed assistant professor of physical geography at Harvard University
1890-Full professorship in physical geography at Harvard University
1890-1915- Assistant geologist U.S. Geological Survey
1898-Appointed Sturgis Hooper professor of geology at Harvard University
1903-Physiographer to Pumpelly's Carnegie Institute survey of Turkestan
1908- Visiting professor at Berlin University
1911- Visiting professor at University of Paris
1911- Lead 9 week geographical pilgrimage from Wales to Italy
1912- Became Emeritus professor at Harvard University
1912- Organized an 8 week transcontinental expedition of the American Geographical Society
1925-26 Visiting lecturer Western Colleges
1927-30- Visiting lecturer at University of California at Berkeley
1927-31 Visiting lecturer at the University of Arizona
1927-32- Visiting lecturer at Stanford University
1930- Visiting lecturer at the University of Oregon
1931-32 Visiting lecturer at the California Institute of Technology
1931- Visiting lecturer at Columbia University
Professional Contribution- Often called "the father of American geography". He was a professor of physical
geography at Harvard, teaching many of the great American geographers to follow him. These students
included Albert Perry Brigham, Richard Dodge, Ellsworth Huntington, Mark Jefferson, and Isaiah Bowman.
He founded the Association of American Geographers in 1904. He became the first president of the AAG, and
shaped the early years of the society. Davis wanted the AAG to be of high intellectual standing, and a
contribution to geography, such as fieldwork or a publication, was required for membership.
Davis called for an increase in geography curriculum at universities. He saw a break between school geography
and professional geography. He wrote a series of papers giving advice on how to teach geography from grade
school all the way up to college. To emphasize education he lead the Conference on Geography in 1894.
In 1889 he wrote "The Rivers and Valleys of Pennsylvania", which was the first paper of it's kind in America.
Within this article he presented the "cycle of erosion".
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His ideas organized the principles of modern meteorology and contributed to significant studies in geology.
Serving as president of the Geological Society of America Davis became an important figure in field research.
Annotated Bibliographies
Davis, William Morris. 1888. "Geographic methods in geologic investigations", "National Geographic
Magazine" 1: 11-26.
The article starts with a definition of geography as "the account of present forms of the earth". Then he states
that this definition is limited. The definition should include description and statistical account of the present
surface of the earth, but also include a systematic classification of the features, viewed as the result of
processes, acting for various periods, at different ages, on diverse structures. He sites two events that create an
advance in geographic study. First the Pennsylvania surveys in 1840. Second the surveys of the west 1870. The
advance is from the old school where structure determines form, to the new school where slow "form
producing" processes create a sequence of forms. He uses an analogy with an oak tree. An individual is not able
to witness a specific tree continually grow. But the individual can make reference to seeing the tree at different
stages. Then apply the form development of the oak to other similar trees. This analogy examples how our
understanding of the earth's surface features should be. His analogy of the oak does not hold true for structures
which go through a repetition of the same process. He mentions an example of a stream which course was
changed by glacial deposits and began eroding a portion of land which had reached its base level.
He applies the ideas to how they can be received in schools and mentions the importance of having a base set of
standard forms, to study from, for geographers and students. These would be used when applying knowledge of
familiar areas to new areas. He also encourages the use of models in teaching. By saying "Good illustrations,
photos, and maps are becoming more common; but the most important means of teaching will be found in
models."
He finishes by saying physical geography is too largely descriptive and statistical. It holds promise for wide
usefulness when its forms are systematically studied and its principles are broadly applied. The essential
element here is the systematic relation of form to structure, base level, and time. He suggests a new term might
be Systematic Geography.
Davis, William Morris. 1889. "The Rivers and Valleys of Pennsylvania", "National Geographic Magazine" 1:
183-253.
In this essay of 70 pages Mr. Davis first sets the scene for the whole essay with an introduction explaining
certain assumptions made in the essay and the organization of the essay. To set the scene he cites a description
of the region by Lewis Evans in 1755. He also describes and comments on previous work done on this area by
Peschel, Tietze, Lowl, Philippson, Lesley.
The second chapter of the essay gives a geological history the region and describes the formations. Many
figures and sketches occupy this portion of the essay to graphically give reference and clarify how the structures
were developed.
In the third chapter he introduces the concepts which he is famous for. The complete cycle of river life: Youth,
adolescence, Maturity, and Old Age. He examines the history of an ideal river life in order to study the
Pennsylvania region. The cycle is started by what he calls an Original river the definition is a stream starting on
a new land. After becoming established the stream then starts the cycle. After describing each stage of the cycle
he indicates that a cycle can be changed by changes in the structure of the landscape.
With the last chapter of the essay he traces the development of streams through the geologic history of
pennsylvania. By making comparisons between streams in contrasting development with similar geologic
structure. He defends the different stages of stream development found in various parts of Pennsylvania.
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Although thought of today as a work which signifies a period of time in geographic development his systematic
approach to organizing streams is still used as a fundamental basis for stream development.
Davis, William Morris. 1900. "The Physical Geography of the Lands", "Popular Science Monthly". 2:157-170.
This article describes the physical features of the world known up to that time. It discusses the advances
regarding the study of the earth, and mentions some geographers who helped make these advances. This article
describes how the various physical features of the world interact with each other, and shows Davis' passion for
physical geography.
created 11-02-96; assistance by John Pruyne at Valparaiso Univerity
If you would like to post materials on the History and Philosophy of Geography in this test area, please contact
Jon T. Kilpinen.
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This page is maintained by the Department of Geography and Meteorology at Valparaiso University. Please send comments and
corrections to Jon T. Kilpinen at jkilpinen@exodus.valpo.edu.
Last revised 25 March 1997 by JTK.
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12/16/2004
LETTER FROM DR. ROBERT STERLING YARD TO DR. H. C. BRYANT
June 24, 1931.
"I have read with keenest interest your report to the Laura Spelman Rockefeller
Memorial on educational activities in National Parks. While it contains few details of
which I was unaware (having been secretary from the beginning of the National Park Educa-
tional Committee, of the National Parks Association, and of the Museums Association's
Outdoor Education Committee under both its titles) I find the achievement as a whole, as
here presented, little short of astonishing. So lusty a growth from so small a start.
in so short a time is not only eloquent of the public need that inspired it, but highly
dramatic also, and I am keen for the popular rewriting which you promise as a public
document.
"But do not think of confining a statement so valuable to outdoor education and the
fame of the National Park Service merely to the Nature Guide System. The story off the
whole should be available in the public and university libraries of the country.
"The only criticism I have concerns the beginning of education in the National
Parks Service which preceded by several years the Nature Guide System. Of course that
was before your personal observation, but I can make the facts available and will be
very glad to do so. Here they are in, I think, sufficient detail.
"Unofficially, the use of the national parks by universities as class rooms began
many years ago. The University of California probably began it, but I havent the record.
In 1899, Doctor Rollin D. Salisbury began taking University of Chicago geological classes
into what afterward became Glacier National Park, Doctor Thomas C. Chamberlin and Doctor
J. Paul Goode following his example. Doctor William M. Davis took Harvard classes to
the Grand Canyon at an early date. Doctor Douglas W. Johnson took Columbia Universi ty
classes into several national parks. Doctor Frederick G. Pack took Utah State University
classes into Yellowstone and the Zion country long before our time. Doctor Ernest Lehner
took University of Minnesota classes into Glacier for several consecutive years, and I
have less definite notes in my 1916 files about several other state universities includin
Texas.
"Mr. Mather caught the educational idea, and definitely determined upon educational
development, as early as the summer of 1916; this was on his second "Mather Mountain
Party" in the Sierra, of which I was a member. We developed it together during our
trail riding of many days. On our way back east we spent eight wonderful September days
in Glacier where we met Dr. Ernest Lehnerts who had just dismissed his University of
Minnesota geology class. During a stormy day in Lewis's hotel on Lake McDonald the three
of us talked over many ideas, some of which afterward were realized.
"We returned full of purpose, and sprung the educational idea officially at the
fourth National Park Conference which was held in the Smithsonian during the first days
of the following January, 1917. The second day of five was called Educational Day, and I
presided at both sessions. Dr. Lehnerts, Dr. Charles D. Walcott, Dr. William H. Holmes
and Dr. Arthur E. Bester, president of Chautauqua, were among eight or nine who spoke
on education, but no one advanced any defined program. Dr. Claxton, U. S. Commissioner
of Education, offered to cooperate with the National Park Service in securing 'educational
extension in the national parks', but his ideas were vague like those of all the rest of
us. At that meeting, by the way, I predicted the National Parks Association which actual]
appeared two and a half years later.
"No definite plans were made either at this meeting or in the months that followe
though many were talked over. Mr. Mather assigned me to canvass opinion, but I found
who took the idea seriously. In May, 1917, the question came up of a title to give my
educational work more weight. I suggested (Educational Adviser to the National Park
Service', but some one, I think Mr. Albright, thought that 'Chief of the Educational
Division' would accord better with Interior Department usage. That was painted on my
door (room 4133) in which, for two years, I carried on a vigorous composite of park
publicity and educational promotion, writing, meantime, my 'Book of the National Parks
The latter was built on an educational frame work which some of us had worked out as
a basis for work in the Service.
"Educational promotion wasn't much of a success at first. No one in Washington
took any interest in it except Mr. Mather, spasmodically; Congressmen smiled over it;
and, with a very few exceptions the concessioners opposed it. Somebody politically
influential on the Pacific Coast slammed the whole idea of education in national parks
by letter to his Senator, who called up Secretary Lane about it, and Lane phoned down
to Mather that he'd better go slow on that unpopular kind of stuff. Thus the cause pe
under a heavy cloud just as things were beginning to look hopeful. But I still kept my
title, and hammered away as inconspicuously as possible.
"Meantime Dr. Charles D. Walcott and a few Smithsonians, together with Mr. Matthe
Mr. Campbell, and others of the Geological Survey, had been getting enthusiastic over
our ideas, and we had a number of good friends in several universities. Discouraged
by Lane's opposition, Dr. Walcott suggested a study organization to determine what
should be done in the circumstances.
"On June 26, 1918, was organized, in the Smithsonian Institution, the National
Parks Educational Committee, consisting largely of university presidents and professor
as far west at Utah and California, together with representatives of leading conserva-
tion organizations including the Camp Fire Club, the Audubon Society and the Sierra
Club. The committee numbered, I think, about 72 members, nearly all much interested.
With Mr. Mather's permission and considerable interest, I ran this committee, as
secretary, from my desk in the Service. It was all to the ultimate good of this Servi
"With $84 collected as postage money, I conducted a lively correspondence, as a
result of which, on May 29, 1919, the educational committee merged into the National
Parks Association, creating it, and I resigned from government service to take charge.
"This brings us, you see, up to the point where you begin your Rockefeller report
In fact, nature guide work in California had already come to our attention, and Enos
Mills had engaged in it in the Rockies. There was talk of applying it in the Nationa
parks, but I think nothing was done till the California Fish and Game people (doesn't
that mean you?) took the initiative.
"I have written this at length to go into the Service files. From it, I hope
that you will find what you need for your popular account of educational beginnings
in national parks."
Sincerely yours,
/s/ Robert Sterling Yard.
2
Davis
Davis
and his two-page article in the Sun describing
Davis had already developed a strong interest
the event was for years remembered as a feat
in economic questions, and many of the articles
of reportorial skill. His experiences both in
that he sent to the Times from Germany dealt
Guam and in the Philippines, where he was
with the economic conditions of that country
present at the capture of Manila, were graphi-
during the war. These articles are said to have
cally described in Our Conquests in the Pocific,
aroused the admiration of James A. Farrell,
published in 1899. A year later, while gathering
sponsor of the National Foreign Trade Council,
news both for the Sun and Harper's Weekly
with the result that Davis was asked to become
during the Chinese Boxer Rebellion, he wit-
secretary of the council-a post he held until
nessed the looting of Peking and of Tientsin.
the time of his death. During this period he con-
Of some of his experiences in China, as the
tributed articles on economics and foreign trade
allies were moving their forces out of the coun-
not only to the Times, but to the Far Eastern
try, he wrote most interestingly in a series of
Review, the Bankers Magazine, the Proceedings
articles in Harper's Weekly entitled "Reporting
of the Academy of Political Science, and other
a Cosmopolitan War" (July 27/, Aug. 3, IO,
journals. He was a delegate from the United
1901). In 1904 during the Russo o/Japanese War,
States to the first Pan-American Postal Con-
he represented the New York Herald.
gress which met at Buenos Aires in 1921, and
With no more wars for the present to report,
in 1930 he asked President Hoover to recom-
in 1907 he settled in Washington, D. C., where
mend an appropriation of $1,500,000 for air-
he served until 1912 as local correspondent for
mail service to South America. He died of heart
the New York Times and the Philadelphia Pub-
disease at Bronxville, N. Y. He was married
lic Ledger. During this period he made two un-
on Apr. 6, 1899, to Jessie Bates Johnson of Bing-
important excursions into/ the realm of fiction:
hamton, N Y., who with two children, Margaret
At the Emperor's Wish, a Tale of the New Japan
and Oscar King, survived him.
(1905) and The Storm-Birds (1910), the latter
[Sources include: Who's Who in America, 1930-31
done in collaboration with Reginald Schroeder.
N. Y. Times, Jan. 25, 1913, Jan. 6, 1930 Elmer Davis,
But his chief interest/ during his Washington
Hist. of The N. Y. Times, 1851-1921 (1921) F. M.
O'Brien, The Story of the Sun (1928) ; obits. in the
residence was politics/ A stanch Republican, he
N. Y. Times and N. Y. Herald Tribune, June 4, 1932
had edited with John K. Mumford in 1901
obit. of Joshua B. Davis in the Baldwinsville Gazette
The Life of William McKinley, which contained
and Farmers' Jour., Aug. 29, 1889. The names of
Davis and his wife appear together on a gravestone in
"copious extracts from the late President's pub-
Riverview Cemetery, Baldwinsville.]
lic speeches, messages to Congress, proclama-
NELSON F. ADKINS
tions and other state papers." In 1908 he pub-
lished William Howard Taft, the Man of the
DAVIS, WILLIAM MORRIS (Feb. I2,
Hour, a campaign biography. During all this
1850-Feb. ,1934),geographer,geologist,teacher,
time he had been intimate with Theodore Roose-
was born in Philadelphia, Pa., the son of Ed-
velt, and with the formation of the Progressive
ward Morris and Maria (Mott) Davis. On his
party in 1912 he became secretary and publicity
maternal side he was descended from James and
chief of the Progressive National Committee, as
Lucretia (Coffin) Mott [qq.v.]. His boyhood
well as director of the party headquarters in
was spent in an intellectual home environment
Washington. In a volume of political reminis-
colored by frequent associations with many of
cence entitled Released for Publication (1925),
the foremost liberals of the day. Until he was
he reviewed his connections with Roosevelt from
eleven he was taught by his mother. Through
1898 to 1918, giving what he calls the "inside
1861 and I862 he attended grammar school in
political history of Theodore Roosevelt and his
West Medford, Mass., and thereafter, until 1866,
times."/ A great admirer of Roosevelt, he re-
a private school in Philadelphia. At the age
garded his friendship with the former President
of sixteen he entered the Lawrence Scientific
as one of the great experiences of his life.
School of Harvard University, graduating in
A few years later he resumed his work as
1869 with the degree of B.S., magna cum laude,
foreign correspondent. He spent the year 1915
and a year later received the degree of mining
in China gathering news for the Chicago Trib-
engineer summa cum laude. His discovery of
une, and in 1916 and 1917 he represented the
the star "T Coronae Borealis" on May I2, 1866,
New York Times in Berlin. While in Berlin,
was indicative of his marked scientific ability.
by dispelling certain illusions regarding the al-
After traveling for a year in Europe he accom-
leged mistreatment of Germans in America, he
panied Prof. Raphael Pumpelly [q.v.] on an ex-
Was in large part responsible for the release of
cursion to the iron and copper districts of Lake
many Americans then being held in Germany.
Superior, and Prof. Josiah D. Whitney [q.v.] on
229
D.A.B. Supp. 1
Davis
Davis
an expedition to the Rocky Mountains of Colo-
and geography. Travels in Europe, the Near
rado, learning on these trips the practical appli-
East, Africa, Canada, and the United States, and
cation of theory in the field. From 1870 to 1873
in the Pacific Ocean, afforded him a wider ac-
he served a scientific apprenticeship at the Na-
quaintance with professional geographers and
tional Observatory in Córdoba, Argentina, and
geologists and opportunity for detailed field study
acquired some fluency in Spanish and a wider
of many areas. During the early part of this
experience in astronomy and biology. The sum-
period he was engaged mainly in a study of land-
mer of 1873 was spent in Europe.
forms, especially glaciers and coral reefs, and
From 1873 to 1876 he was engaged with his
in developing his major contribution-the sci-
father in commercial affairs, for which he never
ence of geomorphology. Association with the
was temperamentally suited. In 1876 he became
work of leading European geographers and geol-
assistant in geology under Nathaniel S. Shaler
logists, and with the American physiographer's,
[q.v.] at Harvard. He accompanied him on field
John W. Powell, Grove K. Gilbert, and Thomas
trips to Tennessee, Kentucky, and the valleys
C. Chamberlain [qq.v.], to whom he acknowl-
of the Hudson and Connecticut rivers, and the
edged a special debt, gave stimulus and aid to
geology of the last-named became the field of
his prolific contributions to the sciences.
his geological work for a considerable time (see
Davis was Harvard visiting professor at the
annual reports of the director of the United
University of Berlin in 1908-09 and at the Sor-
States Geological Survey, especially "The Trias-
bonne in I9II-I2, in each of which he lectured
sic Formation of Connecticut," Eighteenth An-
in the language of the country. In 1912 he pub-
nual Report,
1896-1897, 1898, Pt. II, pp.
lished in German his often-quoted and some-
I-192). His work under Shaler, particularly in
times misinterpreted classic contribution, Die
charge of the geology laboratory, so indicated
erklärende Beschreibung der Landformen (Ber-
to him his lack of training that he applied him-
lin, 1912, 2nd ed., 1924). This and subsequent
self to developing teaching methods, and he ac-
related studies gave rise to two opposing schools
quired a high degree of ability in interpretation
of thought with respect to the genesis, develop-
and description, especially through the use of
ment, and classification of landforms, the Davi-
block diagrams, maps, and models. In 1877-78
sian or American and the Penckian or German
he made a trip around the world, and the follow-
(see Walter Penck: Die Morphologische Analyse,
ing year he was appointed instructor in geology
Stuttgart, 1914; O. D. von Engeln: Geomor-
in Harvard, being given complete charge of a
phology, Systematic and Regional, New York,
course in physical geography and meteorology.
1942; and Otto Maull: Geomorphologie, Leip-
In 1885 he was made assistant professor of phys-
zig, 1938). In I9I2 Davis also served as leader
ical geography and in I800. professor. Summer-
of the transcontinental excursion sponsored by
school courses in geology in association with
the American Geographical Society, in which
Shaler, Jay B. Woodworth, Albert P. Brigham
most of the leading physiographers and geog-
[qq.v.], and others, from about 1879 to 1890,
raphers of the time participated (see his Guide-
contributed to his mastery of that science. His
book for the Transcontinental Excursion of I9I2,
frequent publications were masterpieces of de-
1912). He resigned the Sturgis-Hooper Pro-
scription and geographical analysis. He was con-
fessorship in 1912 and was appointed professor
stantly directing his efforts toward a rational,
emeritus. During the First World War, as chair-
in contrast with the empirical, treatment of sci-
man of the geography committee, geology and
ence. It was during this period that he evolved
geography division, of the National Research
the concept of "the cycle of erosion" (see Jour-
Council, he was responsible for the publication
nal of Geology, January-February 1923) and
of A Handbook of Northern France (1918),
found the need for and fathered new terminology,
and about the same time he prepared for the
such as "peneplain," "mature," and "subsequent."
National War Council of the Young Men's
In addition to his other activities he carried on
Christian Association Excursions around Aix-
field study during the summers, and in 1883 and
les-Bains. During the period 1920-34 his pub-
1891 visited the Rocky Mountain region, during
lications were numerous and significant, among
which time he also worked for the United States
which were his classic landform studies of coral
Geological Survey.
reefs and atolls (see The Coral Reef Problem,
His appointment to the Sturgis-Hooper Pro-
1928, and Les Côtes et les Récifs Coralliens de
fessorship of Geology at Harvard in 1898 per-
la Nouvelle Caledonie, Paris, 1926).
mitted him greater time for research and travel.
From 1925 to 1934 he spent most of his time
It opened the second half of his career, in which
on the Pacific Coast, where he lectured at vari-
he profoundly affected the sciences of geology
ous universities. He also continued to publish
230
Davis
Davison
the products of his numerous field trips and re-
Wyman; third, Aug. I3, 1928, to Lucy L. Ten-
searches, especially in the field of geomorphology.
nant. He died of heart disease at Pasadena, Cal.
His interest in oceanography induced him to
[Isaiah Bowman, in Geographical Rev., Apr. 1934;
prepare a study of submarine valleys, published
A. P. Brigham, in Geographen-Kalendar vol. VII
posthumously as "Submarine Mock Valleys"
(1909), a biog. in English with a German translation;
C.F Brooks, in Bull. of the Am. Meteorological Soc.,
(Geographical Review, April 1934). Less than
Mar. 1934; Kirk Bryan, in Annals of the Asso. of Am.
two months before his death, he gave an address,
Geographers, Mar. 1935; Sci. Monthly, Apr. 1934;
Jour. of Geography, Apr. 1934; Nature (London), June
(The Faith of Reverent Science" (Scientific
1934; Bull. of the Geographical Soc. of Phila., Oct.
Monthly, April 1934), before the American As-
1912; Science, May II, July 20, 1934; Pan-American
Geologist, Aug. 1934; Geographical Jour. (London),
sociation for the Advancement of Science.
July 1934; Vera E. Rigdon, "The Contributions of
To meteorology Davis contributed a useful
William Morris Davis to Geography in America," 1934,
manuscript doctoral thesis in the Lib. of Univ. of Neb.;
authoritative textbook, Elementary Meteorology
Am. Men of Sci. (5th ed., 1933) ; N. Y. Times, Feb.
(1894), and through teaching and publication
7, 1934; Who's Who in America, 1932-33.]
analyzed, organized, and clearly presented a re-
HERMAN R. FRIIS
finement of what was a highly specialized and
unorganized science. To geomorphology and ge-
DAVISON, GREGORY CALDWELL
blogy he contributed a wide range of studies,
(Aug. 12, 1871-May 7, 1935), naval officer and
reflecting his keen historical sense, the formu-
inventor, eldest of the six children of Dr. Alex-
lation and elaboration of profound and new doc-
ander Caldwell and Sarah (Pelot) Eppes/Davi-
trines and ideas, such as the "cycle of erosion,"
son, was born in Jefferson City, Mo. Is father's
and a developmental system of landforms classi-
family traced its descent through Maj./William
fication. He always considered himself a geog-
Davison, merchant, of Winchester, V., and the
rapher indeed, he is largely responsible for hav-
emigrant of the same name, a British army officer
ing made a science of geography in America
and a native of Dublin, Ireland. His mother,
through his mastery of landscape description,
who was twice married, was born at Abbeville,
skilful and precise presentation of facts, and ex-
S. C., a Pelot, of Swiss Huguenot extraction.
ceptional accomplishment in the preparation of
In May 1888 Gregory was appointed naval cadet
maps and block diagrams. To the teaching of
at Annapolis and four years later was graduated
geography he contributed frequent articles on
fifteenth in a class of forty, standing near the
methodology and the effective use of illustra-
top of his class in physics and mathematics. After
tions, and by his own teaching he set an example
two years' required duty /afloat-on board the
and inspired his students and colleagues. He
San Francisco-he was made an ensign, July I,
was the author of over five hundred books and
1894. In this rank he served with the Castine,
periodical publications.
on special service, and in the South Atlantic,
The honors and degrees he received and the
1894-96. In the latter year he went to the torpedo
memberships in foreign and American scientific
boat Cushing as second in command, and thence
societies and on editorial boards that he held
to Torpedo Boat No. 6. During the Spanish-
were numerous. He was awarded the Cullum
American War Davison served on board the
medal, American Geographical Society, 1903;
Oneida in Cuban and Florida waters. While with
the Hayden medal, Academy of Natural Sci-
the New York, flagship of the North Atlantic
ences, Philadelphia, 1918; the Patron's medal,
Station, he in /1900, as first assistant engineer
Royal Geographical Society, 1919; and the Pen-
officer, remodeled her engines, with the result
rose medal, Geological Society of America, 1931.
that she exceeded her trial speed record set ten
Among the many societies to which he belonged
years previously. It was at this time that he
were the National Academy of Sciences, the
aided Marconi in making the first radio trans-
American Association for the Advancement of
mission between ships and shore. In 1900 he
Science, and the American Philosophical So-
was promoted lieutenant; and in 1906, lieutenant
ciety; he was also corresponding member of the
commander.
Deutsche Meteorologische Gesellschaft, Royal
On Nov. I2, 1900, Davison was ordered to
Geographical Society, London, Société de Géo-
command the torpedo boat Rodgers. He had now
raphie, Paris, Imperial Geographical Society of
found his forte, and his future service in the
Petersburg, and Sociedad Antonio Alzate of
navy was chiefly with torpedo boats, destroyers,
lexico.
and ordnance. Work on torpedoes and gun de-
Davis was married three times: first, Nov. 25,
sign at the Bureau of Ordnance was his chief
879, to Ellen B. Warner, by whom he had three
employment, 190I-02. He commanded the tor-
ons, Richard Mott, Nathaniel Burt, and Ed-
pedo boat Barney, 1902-03; the torpedo boat
ard Mott; second, Dec. 12, 1914, to Mary M.
flotilla at the Norfolk navy yard, 1903; and the
23 I
581.974
R186f
ra of Mount Desert Island, Maine.
CONTENTS.
A
PRELIMINARY CATALOGUE
PA
PREFACE
OF THE
GENERAL OUTLINE OF PLAN OF CATALOGUE.
NTS GROWING ON MOUNT DESERT
I. INDIGENOUS PLANTS
II. INTRODUCED PLANTS
III. SYNONYM8
AND THE ADJACENT ISLANDS.
IV. ARRANGEMENT AND NOMENCLATURE
V. CITATION OF AUTHORS
VI. FORMS
VIL TERMS DENOTING RELATIVE OCCURRENCE
BY
VIII PLANTS NOT REPRESENTED IN THE HERBARIUM
EDWARD L. RAND AND JOHN H. REDFIELD.
IX ABBREVIATIONS
X
GEOGRAPHICAL NOMENCLATURE
INTRODUCTION.
I. MOUNT DESERT AND ITS FLORA
With a Geological Introduction
II. THE MAP OF MOUNT DESERT ISLAND
List of Corrections
Br WILLIAM MORRIS DAVIS,
III. BOTANICAL NOMENCLATURE OF THE CATALOGUE
AND A NEW MAP OF MOUNT DESERT ISLAND.
OUTLINE OF THE GEOLOGY OF MOUNT DESERT.
INTRODUCTION
THE GRANITE BELT
THE PRE-GRANITIC ROCKS
THE POST-GRANITIC ROCKS
THE GREAT DENUDATION
CAMBRIDGE:
THE GLACIAL INVASION
JOHN WILSON AND SON.
POSTGLACIAL HISTORY
University Press.
1894.
6
CONTENTS.
FLORA: CATALOGUE OF PLANTS.
PHANEROGAMIA, OR FLOWERING PLANTS.
DICOTYLEDONES, OR EXOGENOUS PLANTS
75
ANGIOSPERMEE : POLYPETALE
75
GAMOPETALE
107
PREFACE.
APETALA
139
GYMNOSPERMEE
149
MONOCOTYLEDONES, OR ENDOGENOUS PLANTS
150
CRYPTOGAMIA, OR FLOWERLESS PLANTS.
PTERIDOPHYTA
THE
territory covered by this Catalogue of Plants
184
comprises the Island of Mount Desert and the ad-
BRYOPHYTA
190
MUSCI
joining islands, the more important of which are the
190
HEPATICA
Cranberry Isles, Bartlett Island, Thompson Island, and the
219
THALLOPHYTA
Porcupine Islands. The Duck Islands, lying some miles
227
CHARACKE
seaward southerly from the Cranberry Isles, are also in-
227
ALGE
cluded for convenience, although having no close con-
227
LICHENES
250
nection geographically with the rest of the territory.
Politically it comprises the towns of Eden, Mount Desert,
SUMMARY
275
Tremont Cranberry Isles, a small part of Trenton, and a
APPENDIX.-LIST OF EXCLUDED SPECIES
277
part of Long Island Plantation, in which the Duck Isl-
ands are included. All of this territory, with the ex-
ception of the Duck Islands, is shown on the map that
INDEX
281
has been prepared to accompany this Catalogue.
In 1880 the Champlain Society an association of college
students formed for the purpose of field work and study
in various branches of natural science, established its
camp on the shores of Somes Sound at Wasgatt Cove,
Mount Desert Island. This Catalogue of Plants repre-
sents the final results of work begun by its botanical
department, while the introductory article on the Ge-
ology of Mount Desert represents the work of its geo-
logical department. Two years later one of the authors,
John H. Redfield, began independent investigation of
8
PREFACE.
PREFACE.
9
the Island flora. In 1888 the Champlain Society allowed
wise would have been locked up in the herbaria and
its botanical work to pass into the hands of the other
note-books of unknown workers in the same territory.
author, Edward L. Rand, who, however, had been con-
Specimens of every plant in this list, with very few
nected with the work from its beginning. Soon after-
exceptions, will be found preserved in the Mount Desert
wards the authors consolidated the results of all the
Herbarium, at present kept in Cambridge, Mass. These
botanical work on the Island, so far as they were able,
exceptions, most of which are either Alg or Lichens,
and henceforth carried on the work together, with such
are denoted by an asterisk prefixed to the name of the
assistance as could be procured from other botanists.
species. For specimens of plants thus marked, as well as
Although more or less incomplete, and somewhat hastily
for other plants from collectors now unrepresented, we
prepared, this Catalogue is now presented, at the request
shall be most grateful. The Philadelphia Academy of
of many interested in the subject, as a preliminary con-
Natural Sciences, furthermore, has an almost complete
tribution to a Flora of Mount Desert Island. This is
duplicate set of the Phanerogams and Pteridophyta; and
done with the hope that it may serve as a means of excit-
Dr. Carl Warnstorf of Neuruppin, Germany, has a dupli-
ing interest in the undertaking, and thus make possible
cate set of the Sphagna. Duplicates from the Herbarium
a more complete catalogue in the near future.
have also been distributed among various public and pri-
So far as the study of its flora is concerned, Mount De-
vate herbaria of the country.
sert has no history. We are told by the early explorers
Much care has been taken to make the Catalogue reli-
that wild roses and beach peas were abundant, and that
able. Very few plants have been admitted to the list
is all. No botanists native to the Island - if any there
except on the authority of an undoubted specimen, and in
were or are - have given us information as to its plants.
every case of exception only on a positive affirmation by a
All such information has come from such botanists as have
specialist or other botanist of high repute as to the
chanced to go there from a distance, usually during the
authenticity and identity of the lost specimen. More-
summer months only. Even of these the known list is
Over, we have had the kind assistance of many of the
not long, and only few antedate the beginning of syste-
leading botanists of the country in the determination of
matic work in 1880. It has, furthermore, been extremely
specimens in difficult families and genera, and in cases
difficult to discover the names of these botanists, and to
of doubtful determination, as well as in the criticism and
consult their notes and collections, although the authors
correction of our manuscript. Prof. L. II. Bailey has
have, endeavored in many ways to accomplish this. The
given his help in Carex and Rubus; Mr. M. S. Bebb, in
result naturally has been far from satisfactory. In spite
Salix; Prof. William Trelease, in Rumex and Epilobium;
of all these discouragements, however, the work on the
Dr. Thomas C. Porter, in Solidago, Aster, and Mentha;
Flora has been carried on with perseverance. It is now
hoped that from the very fact of the publication of pres+
1 Any correspondence relating to the Flora may be addressed to Edward
L. Rand, 740 Exchange Building, Boston, Mass., or to John H. Redfield, 216
ent results help may be obtained for the future that other-
West Logan Square, Philadelphia, Penn.
10
PREFACE.
PREFACE.
Mr. John K. Small, in Polygonum; Prof. F. Lamson
fresh-water Algx and the Fungi, and it has seeme
Scribner, in Gramine; Dr. L. M. Underwood, in Isoetes
for the present to omit the latter altogether f1
and in Hepatic; Mr. George E. Davenport, in Filices;
Catalogue. It is hoped that in the near futu
Dr. T. F. Allen, in Characex ; Messrs. Frank S. Collins
attention may be given to increasing in a marked
and Isaac Holden, in Algx; Dr. Carl Warnstorf, Prof. D.
our knowledge of this part of the Island flora.
C. Eaton, and Mr. Edwin Faxon, in Sphagnum; Mrs.
E. G. Britton and Dr. Charles R. Barnes, in the other
July 1st, 1894.
Mosses; Dr. J. W. Eckfeldt, Miss Mary L. Wilson, and
Miss Clara E. Cummings, in Lichenes; and Dr. B. L.
Robinson, Dr. N. L. Britton, Dr. Thomas Morong, Mr.
Walter Deane, and Mr. M. L. Fernald, in various other
determinations. The article on the Geology of Mount
Desert has been kindly contributed by Prof. William M.
Davis, of Harvard College. To these and to all others
who have done 80 much to add to the value and accuracy
of this Catalogue, to the various collectors whose names
appear therein, and to President Charles W. Eliot of
Harvard University, through whose interest and kindness
the publication of our work has been made possible, we
extend our sincere thanks.
Acknowledging, as we have at the outset, the incom-
pleteness of this Catalogue in many of its divisions, we
issue it at the present time to assist those interested in
the plants of the Island to the acquirement of a better
knowledge of its flora. With this end in view, therefore,
it has seemed well to include, for the benefit of specialists,
even manifestly incomplete lists of some of the Crypto-
gams. The list of Vascular Cryptogams (Pteridophyta),
the Ferns and their allies, is fairly complete; the lists of
Mosses and Liverworts are well advancing towards com-
pletion, and the same is true of the lists of Lichens and of
the marine Algm. Very little work, however, has been
done thus far in the collection and determination of the
Bulletin of the Museum of Comparative Zoölogy
AT HARVARD COLLEGE.
the
7/2/07
VOL. XLII.
GEOLOGICAL SERIES, Vol. VI. No. 1.
AN EXCURSION TO THE PLATEAU PROVINCE OF UTAII
AND ARIZONA.
By W. M. DAVIS.
WITH SEVEN PLATES.
CAMBRIDGE, MASS., U.S.A.:
PRINTED FOR THE MUSEUM.
JUNE, 1903.
JUN
5
1903
No. 1. - An Excursion to the Plateau Province of Utah and
Arizona. By W. M. DAVIS.
TABLE OF CONTENTS.
Introduction
1
The Section near Antelope Wash
30
The Sevier-Torowcap Fault
4
The Topography of the Colorado
Previous Statements
4
Canyon
31
The Fault at Upper Kanab
5
The Cross-Section of the Canyon
31
The Jurassic Sandstones
8
Amphitheaters in the Canyon
Kanab Canyon
9
Walls
33
The Fault at Pipe Spring
12
The Profile of Sharp Cusps
34
The Moccasin Fault
14
General Relations of Amphithe-
Erosion in the lipe Spring
aters and Cusps
34
District
15
The Great Terraces
36
Connection of Sevier and Toro-
Refreshed Cliff Profiles
36
weap Faults
17
Revived Erosion of the Pink
The Toroweap Fault at the Grand
Cliffs
38
Canyon
18
The Valley of the Virgin
39
Camping on the Esplanade
21
The Fresh-water Tertiaries
42
General Features of the Espla-
Previous Statements
42
nade
21
Eocene of the High Plateaus
The View from Vulcan's Throne
23
of Utah
43
The Hurricane Fault
26
The Green River Basin, Wyoming
45
Previous Statements
20
Bibliography
49
The Section near Coal Spring
27
Explanation of Plates
50
Introduction.
IN the summer of 1902. the writer made his third visit to the region of the
Colorado canyon.
The results of the first visit in 1900 have already been
published (a, b); 1 the results of the second visit in 1901 were of relatively
small import and are here presented along with those of the third.
The
last excursion was undertaken partly as a means of providing oppor-
tunity in field work for some of our advanced students in geology at
Harvard, two of whom, Messrs. Ellsworth Huntington and J. Walter
1
Dates, letters, or page numbers in parenthesis refer to the bibliography at the
close of the article.
VOL. XLII. - NO. 1
1
2
BULLETIN MUSEUM OF COMPARATIVE ZOOLOGY.
DAVIS: THE PLATEAU PROVINCE OF UTAH AND ARIZONA.
3
Goldthwait, were enabled by the generous contributions from several
friends of the geological department to spend five weeks in the plateaus
north of the canyon. An abstract of their report has been published
in the Journal of Geology and a fuller statement of their results will form
a later member of this Bulletin.
P.H
Our itinerary, shown by a broken line with numbers for dates on
Figure 1, was as follows : - From Provo by rail to Marysvale, July 12
31%
Marysvale by wagon to Kanab, July 13 to 17 ; Kanah, in saddle
with wagon outfit, to Mt. Trumbull and the Colorado canyon at Toro-
weap, July 18 to 21 ; on the esplanade of the canyon, July 22 from
15
Rt
the canyon to Toquerville, July 23 to 29 ; about Toquerville with
wagon, July 30 to August 5. On the latter date I left my companions
29T
at St. George to continue their study of the Toquerville district, and
went by wagon and rail to Salt Lake City, and thence to Nevada and
Oregon, as will be described in a later number of this Bulletin.
26
The observations made in 1900 led to certain departures from conclu-
sions previously published, especially as to the time of the production
UTAH
ARIZIONA
of the great north-south faults by which the platean province is traversed.
It was believed that the greater part of the faulting had been accom-
P.S
plished before the uplift of the region by which the erosion of the Colorado
18
canyon was initiated; that is, during the plateau cycle of erosion, so-
called because the removal of a great thickness of rocks from the broad
area of the plateaus north and south of the canyon was then effected
(a,p.119). It was further thought that during the canyon cycle of erosion
24+
extensive areas of weak Permian rocks were stripped from the uplifted
20
region while the Colorado river was corroding its canyon (p. 139) ; and
23
it was suspected that the western boundary of the uplifted region lay
along the line of the Grand wash fanlt, on which a relatively late move-
ment, long after an earlier movement, served to place the plateau region
on the east above the Basin region on the west (1. 148).
The first of these conclusions will liere be further substantiated ; but
at the same time it will be shown that modern faulting of large amount
has taken place on the Hurricane fault fifty miles and more north of
50
the canyon. Additional evidence will be presented as to the stripping
of weak Permian strata from the plateaus north of the canyon during
the canyon cycle. Perhaps the most important result of the summer's
FIGURE 1.
work bears on the recent movement along the Grand wash fault, which
Route map. The numbers alongside of the broken line showing the route followed indicate
is now promoted from the rank of a supposition to that of a reasonable
the dates in July (14-31) and August (1 to 5), 1902, when certain points were passed.
certainty, as will appear from the work of niy student companions. Sev-
The abbreviations are as follows -A, Grand View Hotel ; B, Bright Angel Hotel.
These two points, south of the canyon, were visited in the summer of 1901. FA, Fre-
cral collateral problems are discussed, as appears in the table of contents.
donia ; G. St. George; KB, Kanab; P11, Panguitch; l. S., Pipe spring; R, Ranch;
T, Toquerville.
Joshua L. Chanberlain (Ed.) 1900
64
UNIVERSITIES AND THEIR SONS: Harvard In werity
COOLIDGE, Archibald Cary, 1866-
Latin Orient Works. He is a member of the Ameri-
Born in Boston, Mass., 1866; graduated at Harvard;
can Historical Society, the Massachusetts Historical
studied in Berlin, Paris, Baden; diplomatic service
Society, and the Somerset Club.
at St. Petersburg, Paris and Vienna; Asst. Prof. of
History at Harvard; member of the American Histori-
cal Society, and of the Massachusetts Historical
DAWES, Thomas, 1757-1825.
Society.
A
RCHIBALD CARY COOLIDGE, Ph.D.,
Born in Boston, Mass., 1757; graduated at Harvard,
1777; member of the Constitutional Conventions of
Assistant Professor of History at Harvard,
1780, 1789 and 1820; Judge of the Supreme Court of
is the son of Joseph Randolph (great-grandson of
Mass, 1792-1803; Judge of the Municipal Court, Bos-
Thomas Jefferson) and Julia (Gardner) Coolidge,
ton, 1803-1823; Judge of Probate, 1823-1825; fellow of
and was born in Boston, Massachusetts, March 6,
American Academy; died in Boston, 1825.
1866. He graduated at Harvard in 1887, and
T
HOMAS DAWES, A.M., Overseer of Har-
vard, was born in Boston, Massachusetts,
July 8, 1757, son of Thomas Dawes (1731-1809), a
leading patriot of Boston during the Revolution.
He was graduated at Harvard in I777, and under
the inspiration of his father and of the times, at once
became active in public affairs. In 1780 he was a
member of the Constitutional Convention, and in
the Convention of 1789, which adopted the Federal
Constitution, he was also a delegate. In 1792 he
was appointed Judge of the Supreme Court of Mas-
sachusetts, and for ten years served in that office.
From 1803 to 1823 he was Judge of the Municipal
Court of Boston and from the latter year until his
death he officiated as Judge of Probate. It is said
of Judge Dawes that his literary productions were
popular, and his witticisms proverbial." He was
a
fellow of the American Academy and was an Over-
seer of Harvard from 1810 to 1823. He died in
Boston, July 22, 1825.
DAVIS, William Morris, 1850-
ARCHIBALD CARY COOLIDGE
Born in Philadelphia, Penn., 1850; educated at public
then studied at Berlin University, and at the École
and private grammar schools and at Lawrence Scien-
tific School and at the Hooper Mining School of Har-
des Sciences Politiques in Paris, and at Freiburg in
vard; was Assistant in the Argentine National
Baden, receiving the degree of Doctor of Philosophy
Observatory; Assistant and Instructor in Geology at
at the latter Institution in 1892. He spent several
Harvard; Assistant Professor of Physical Geography
years abroad travelling extensively and obtaining a
at Harvard and since 1890 Professor of Physical Geog-
raphy at this College ; is member of the National
glimpse of diplomatic service at St. Petersburg,
Geographic Society, the Geological Society of America,
Paris and Vienna. At St. Petersburg he served as
the American Academy of Arts and Sciences, fellow
Secretary of Legation without appointment in 1890-
of the American Association for the Advancement of
91, and at Vienna was Secretary of Legation by
Science and corresponding member of other societies.
appointment in 1893. For several years he has
W
ILLIAM MORRIS DAVIS, S.B., M.E.,
taught history at Harvard, and now holds the posi-
Professor of Geology at Harvard, was born
tion of Assistant Professor in that subject. Dr. Cool-
in Philadelphia, Pennsylvania, February I-2, 1850.
idge has donated to Harvard many hundred volumes
His father and mother were both of Quaker descent,
relating to Slavic history, and with his father, J. R.
the former Edward Morris, being a member of the
Coolidge, he gave in 1900 the Riant Collection of
families of Davis and Evans in Eastern Pennsylvania,
UNIVERSITIES AND THEIR SONS
while his mother, Maria Mott Davis, was the daugh-
Geographical Society of Berlin, and corresponding
ter of James and Lucretia Mott, the former being
member of the Geographical Societies of London,
descended from Long Island Quakers and the latter
Paris, Munich and Philadelphia, of the Geological
from Nantucket Quakers. Mr. Davis received his
Society of Edinburgh, and of the German Meteoro-
early education at the grammar school at West Med-
logical Society. He married, November 25, 1879,
ford, Massachusetts, and at a private school in Phil-
Ellen Bliss Warner, of Springfield, Massachusetts, and
adelphia. In 1869 he received the degree of
has three children : Richard Mott, Nathaniel Burt
Bachelor of Science at the Lawrence Scientific
and Edward Mott Davis.
School at Harvard and one year later was given the
degree of Mining Engineer, at the Hooper Mining
School of the same University. "Three years were
DENNETT, John Richard, 1837-1874.
then spent in the Argentine National Observatory
Born in Chatham, N. B., 1837 graduated at Har-
vard, 1862; Editor Harvard Magazine while in College;
Superintendent of a plantation in the South during
the Civil War; contributor and afterwards one of the
Editors of the New York Nation; Assistant Professor
of Rhetoric at Harvard, 1869-1872; died in Westboro,
Mass., 1874
J
OHN RICHARD DENNETT, Assistant Pro-
1
fessor of Rhetoric at Harvard, was born in
Chatham, New Brunswick, in 1837 and was fitted
for College in the High School of Woburn, Massa-
chusetts, to which place his parents removed during
his childhood. He was graduated at Harvard in
1862, and soon after went to Beaufort, South
Carolina, to take charge of a plantation. Shortly
after the close of the Civil War he made a compre-
hensive tour of the Southern States in the interest of
the New York Nation, and contributed to that paper
a series of interesting letters upon the political con-
ditions and prospects of the South. On his return
North he became connected with the editorial staff
of the New York Nation, and in 1869 accepted the
Assistant Professorship of Rhetoric at Harvard, in
which he officiated until compelled to resign by
WILLIAM, M. DAVIS
reason of failing health in 1872. Mr. Dennett's
journalistic talents and rhetorical abilities were
at Cordova under Dr. B. A. Gould. Since 1876
strikingly manifested while he was yet. an under-
Professor Davis has. been connected with the Har-
graduate at Harvard. During his College course he
vard Faculty, for the first nine years as Assistant and
edited the Harvard Magazine, and his Class Day
Instructor in Geology, for the next five years as
poem was a production of such unusual merit as to
Assistant Professor of Physical Geography, from
bring forth the especial commendation of James
1890 to 1899 as Professor in the last-named branch
Russell Lowell for its rare poetic qualities. He died
and in 1899 was elected to the Sturgis-Hooper Pro-
at the early age of thirty-seven years, in Westboro,
fessorship of Geology. He is the author of text-
Massachusetts, November 26, 18
books on Meteorology and Physical Geography, and is
a member of numerous societies, including the Amer-
ican Academy of Arts and Sciences, Boston, the Bos-
DUNBAR, Charles Franklin, 1830-1900:
ton Natural History Society, the Geological Society
Born in Abington, Mass., 1830 educated at Phillips-
of America, the National Geographic Society, besides
Exeter Academy and Harvard; received the degree
being a fellow of the American Association for the
of A.B. in 1851; studied W in the Harvard Law
Advancement of Science, honorary member of the
School and in the office of Hoar, Gray & Bangs;
5
UNH LIBRARY
3 4600 00816 4185
GEOGRAPHICAL
ESSAYS
BY
WILLIAM MORRIS DAVIS
STURGIS-HOOPER PROFESSOR OF GEOLOGY, HARVARD UNIVERSITY
EDITED BY
DOUGLAS WILSON JOHNSON
ASSISTANT PROFESSOR OF PHYSIOGRAPHY, HARVARD UNIVERSITY
GINN AND COMPANY
BOSTON . NEW YORK . CHICAGO . LONDON
551.4
D265
EDITOR'S NOTE
An endeavor has been made in this volume to meet the grow-
ing demand for an edition of Professor Davis's most important
geographical essays. Since it was not possible to include within
the limits of a single volume all essays which students of geog-
raphy desire to see reprinted, the editor was asked to select a
limited number, and to prepare them for publication. He can
hardly expect that his choice will meet with unanimous approval,
but he believes it will appear that the selections herewith pre-
COPYRIGHT, 1909
sented are fairly representative of the author's contributions to
By WILLIAM MORRIS DAVIS
the science of geography.
ALL RIGHTS RESERVED
For sake of uniformity in style, method of treatment, etc.,
89.6
minor modifications have been made in many of the essays, SO
that they do not always conform exactly to the text as originally
published. A large number of the illustrations have been re-
drawn, while a few have necessarily been omitted. In special
(cases portions of the text have been materially revised to bring
them into accord with recent discoveries, or to eliminate matter
inappropriate for publication under the present circumstances.
Such alterations as have been made have received the author's
approval. The original form of any essay may be found by con-
sulting the citations given in the Table of Contents.
The essays admit of a natural classification into two main
groups : those concerned chiefly with the teaching of geography,
included in Part One, Educational Essays and those dealing
with the principles of the science of geography, more especially
be athenxum Dress
GINN AND COMPANY PRO-
that branch of the science known as physiography, included in
PRIETORS BOSTON U.S.A.
iii
iv
EDITOR'S NOTE
Part Two, Physiographic Essays. Under each part the essays
are grouped according to subject-matter rather than in the order
of their publication. A more recent essay precedes an older
CONTENTS
essay on the same general subject, whenever it appears desirable
PART ONE - EDUCATIONAL ESSAYS
that the older essay should be read with a full knowledge of the
PAGE
author's latest opinions.
I. AN INDUCTIVE STUDY OF THE CONTENT OF GEOGRAPHY
3
Presidential address at the second meeting of the Association of
For the reproduction of the essays in the present form, the
American Geographers, December, 1905. Bulletin American
publishers are indebted to the several publications in whose
Geographical Society (1906), XXXVIII, 67-84.
II. THE PROGRESS OF GEOGRAPHY IN THE SCHOOLS
23
pages the essays originally appeared, and by whose courtesy
First Year Book National Society for the Scientific Study of Educa-
they are reprinted here.
tion (1902), Part II, 7-49.
DOUGLAS WILSON JOHNSON
III. THE PHYSICAL GEOGRAPHY OF THE LANDS
70
Popular Science Monthly (1900), LVII, 157-170.
HARVARD UNIVERSITY
IV. THE TEACHING OF GEOGRAPHY
87
Educational Review (1892), III, 417-426; IV, 6-15.
V. THE EXTENSION OF PHYSICAL GEOGRAPHY IN ELEMENTARY
TEACHING
105
An address delivered before the Middlesex (Massachusetts)
Teachers Club, in Boston, October 8, 1892. School and Col-
lege (1892), I, 599-608.
VI. GEOGRAPHY IN GRAMMAR AND PRIMARY SCHOOLS
115
School Review (1893), I, 327-339-
VII. PHYSICAL GEOGRAPHY IN THE HIGH SCHOOL
129
School Review (1900), VIII, 388-404.
VIII. THE NEED OF GEOGRAPHY IN THE UNIVERSITY
146
Educational Review (1895), X, 22-41.
IX. PHYSICAL GEOGRAPHY AS A UNIVERSITY STUDY
165
(Last four pages omitted in the reprint.) Journal of Geology (1894),
II, 66-100.
X. METHODS AND MODELS IN GEOGRAPHICAL TEACHING
193
A lecture delivered before the Scientific Association of Johns Hop-
kins University on February 13, 1889. The American Naturalist
(1889), XXIII, 566-583.
XI. PRACTICAL EXERCISES IN PHYSICAL GEOGRAPHY
210
Compiled from two essays on same subject, one published in the
Proceedings Fifth Annual Conference New York State Science
Teachers Association (1900), the other published in National
Geographic Magazine (1900), XI, 62-78.
XII. FIELD WORK IN PHYSICAL GEOGRAPHY
236
(First four pages omitted in reprint.) Journal of Geography (1902),
I, 17-24, 62-69.
y
V1
CONTENTS
PART TWO - PHYSIOGRAPHIC ESSAYS
PAGE
XIII. THE GEOGRAPHICAL CYCLE
249
Geographical Journal (1899), XIV, 481-504.
XIV. COMPLICATIONS OF THE GEOGRAPHICAL CYCLE
279
Eighth International Geographic Congress, 150-163.
XV. THE GEOGRAPHICAL CYCLE IN AN ARID CLIMATE
296 -
Journal of Geology (1905), XIII, 381-407.
XVI. PLAINS OF MARINE AND SUB-AÉRIAL DENUDATION
323
Bulletin Geological Society of America (1896), VII, 377-398.
XVII. THE PENEPLAIN
350
Originally written in reply to a paper by Professor R. S. Tarr on the
same subject. Reprinted with numerous minor changes. American
Geologist (1899), XXIII, 207-239.
XVIII. BASE-LEVEL, GRADE, AND PENEPLAIN
381
Journal of Geology (1902), X, 77-III.
XIX. THE RIVERS AND VALLEYS OF PENNSYLVANIA
413
National Geographic Magazine (1889), I, 183-253.
GEOGRAPHICAL ES
XX. THE RIVERS OF NORTHERN NEW JERSEY WITH NOTES ON
THE CLASSIFICATION OF RIVERS IN GENERAL
485
National Geographic Magazine (1890), II, 81-110.
XXI. RIVER TERRACES IN NEW ENGLAND
514
Bulletin Museum of Comparative Zoology (1902), XXXVIII,
281-346.
XXII. THE SEINE, THE MEUSE, AND THE MOSELLE
587
National Geographic Magazine (1896), VII, 189-202, `228-238.
XXIII. THE SCULPTURE OF MOUNTAINS BY GLACIERS
617
Presented in abstract before Sections C and E of the British
Association at Cape Town, August 17, 1905. Scottish Geo-
graphical Magazine (1906), XXII, 76-89.
XXIV. GLACIAL EROSION IN FRANCE, SWITZERLAND, AND NORWAY 635
Proceedings Boston Society Natural History (1900), XXIX, 273-322.
XXV. THE OUTLINE OF CAPE COD
690
Proceedings American Academy of Arts and Sciences (1896), XXXI,
303-332.
XXVI. THE MOUNTAIN RANGES OF THE GREAT BASIN
725
Bulletin Museum of Comparative Zoology (1903), XLII, 129-177.
INDEX
773
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Author : Davis, William Morris, 1850-1934.
Title : An excursion to the plateau province of Utah and Arizona.
Published : Cambridge, Mass., Printed for the Museum, 1903.
Locations/Orders : Availability
Location : Museum Comp Zoology
i
MUS 4890 Holdings Availability
Description : 50 p. profiles, 7 plates. 25 cm.
Series : Bulletin of the Museum of Comparative Zoölogy at Harvard College, V. 42 [no. 1] Geological series, V.
6, no. 1
Subject : Geology -- Utah.
Geology -- Arizona.
Other Titles : Bulletin of the Museum of Comparative Zoology : V. 42, no. 1.
Bulletin of the Museum of Comparative Zoology. Geological series ; V. 6, no. 1.
HOLLIS Number : 005039327
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Author : Davis, William Morris, 1850-1934.
Title : Additional papers, 1885-1951.
Locations/Orders : Availability
Location : Houghton i b MS Am 1798 Holdings Availability
Description : 7 boxes (3.5 linear ft.)
Description : Organized into the following series: I. Letters to William Morris Davis; II. Letters from William
Morris Davis; III. Other letters; and IV. Compositions and other papers.
History notes : Davis, an American geographer and geologist, was a world authority on physical geography, a
creator of the science of geomorphology, and called the father of physiography. He taught geology
at
Harvard University (1876-1912), traveled throughout the world, founded the Harvard Travelers Club
and the Association of American Geographers, and also contributed to the fields of astronomy and
meteorology.
Summary : The bulk of the collection is professional correspondence, primarily to Davis from his colleagues.
Letters by him and between third parties also focus on his work as a geographer, geologist, and
professor. The chief correspondent represented is geographer Lawrence Martin. There are
compositions by Davis on geology as well as poems by him. Additionally, there are contracts,
business papers, clippings, and photographs. Finally, there are some compositions by others.
Notes : Some letters to Davis are in German.
Provenance : Transferred from the Geographical Institute, 1955.
Cite as : William Morris Davis Papers (MS Am 1798). Houghton Library, Harvard University.
Finding aids: Electronic finding aid availablehttp://nrs.harvard.edu/urn-3:FHCL.Hough:hou00697
Unpublished printed finding aid available in the Houghton Accessions Records, 1964-1965, under
*64M-265.
Subject Davis, William Morris, 1850-1934.
Subject : Harvard University -- Faculty.
Subject Geomorphology.
Maps.
Physical geography.
World War, 1914-1918 -- Maps
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Author : Davis, William Morris, 1850-1934.
Title : Papers of William Morris Davis, ca. 1878-ca. 1930 (inclusive).
Locations/Orders : Availability
Location : Harvard Archives
i
Harvard Depository HUG 1317 [Family correspondence, reprints, and
biographical material] Holdings Availability
Description : 2 boxes of mss.
History notes : William Morris Davis (1850-1934) earned his Harvard S.B. in 1869. He taught geology and
geography at Harvard.
Summary : Consists of family correspondence, biographical material, reprints, diplomas and medals.
Family correspondence consists of letters from Morris to his parents written while he was a student
at Harvard, 1870, and letters from Morris to his son Edward and daughter-in-law Dorothy, 1932-
1933.
Subject : Davis, William Morris, 1850-1934.
Keyword Subject : Harvard University -- Geology.
Harvard University -- Geography (Field of study)
Harvard University -- Faculty member.
Form/Genre : Diplomas.
HOLLIS Number : 000604252
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Davis, William Morris, 1850-1934. Additional papers: Guide.
Page 1 of 16
MS Am 1798
Davis, William Morris, 1850-1934. Additional
papers: Guide.
Houghton Library, Harvard College Library
VE
THARVARD
Harvard University, Cambridge, MA 02138
C 2003 The President and Fellows of Harvard College
Descriptive Summary
Repository: Houghton Library, Harvard College Library, Harvard University
Location: b
Call No.: MS Am 1798
Creator: Davis, William Morris, 1850-1934.
Title: Additional papers,
Date(s): 1885-1951.
Quantity: 7 boxes (3.5 linear ft.)
Abstract: Primarily professional correspondence of American geographer and geologist William
Morris Davis as well as compositions by him.
Administrative Information
Acquisition Information: *64M-265
Transferred from The Geographical Institute; received: ca. 1955.
Historical Note
Davis, an American geographer and geologist, was a world authority on physical geography, a
creator of the science of geomorphology, and called the father of physiography. He taught geology
at Harvard University (1876-1912), traveled throughout the world, founded the Harvard Travelers
Club and the Association of American Geographers, and also contributed to the fields of astronomy
and meteorology.
Arrangement
Organized into the following series:
http://oasis.harvard.edu/html/hou00697.html
12/4/2004
Datr 1.d
lisilent
kg 506 N213b v.23 11th
1902 14DD ponky
Daly, Reginald Aldworth, 1871
Biographical memoir of Willia
Q141 N2 v.23 11th 1944
Does
pour
NATIONAL ACADEMY OF SCIENCES
OF THE UNITED STATES OF AMERICA
BIOGRAPHICAL MEMOIRS
VOLUME XXIII-ELEVENTH MEMOIR
BIOGRAPHICAL MEMOIR
OF
WILLIAM MORRIS DAVIS
1850-1934
BY
REGINALD A. DALY
PRESENTED TO THE ACADEMY AT THE AUTUMN MEETING, 1944
Wee Daus
WILLIAM MORRIS DAVIS
1850-1934
BY REGINALD A. DALY
William Morris Davis won distinction as geologist, meteor-
ologist, and geomorphologist, but primarily as teacher. He made
personal, outdoor researches in every continent except Ant-
arctica, as well as in island groups of the Atlantic and the Pacific;
yet his international fame rests chiefly on his development of a
system of thought concerning the reliefs, the scenery, of our
planet. His system is the "American" system, but it is appli-
cable to the landscapes of the whole world. His early training
in geology led him to the principle by which he, more than any-
one else, has revolutionized the teaching of, and research on,
the. endlessly varied forms of the lands and coastlines. To
geographers and geologists alike he was an apostle bringing
to them the gospel of method in research and method in the
presentation of the results of research. For him the root of
the matter is evolution, orderly development. Many geologists
had used this principle, so essential to understanding the protean
crust of the earth, but few geographers had used it in describing
land forms. Davis emphasized a mode of thinking and for its
expression he devised a system which has greatly appealed to
teachers and investigators in many foreign countries as well
as in the United States of America. While creating his de-
scriptive method in terms of evolutionary changes, he found
our English tongue sadly deficient. He had to create a new,
necessarily technical language. Every man of science knows
the difficulty of such an invention. Some of his verbal tools
Davis was able to adopt from the literature of earth science,
an immense literature which he thoroughly mastered other vital
terms were his own. The combination has been put to construc-
tive use by geologists and geographers, foreign and domestic,
to an extent encouraging to our pioneer. He lived to see notable
improvement of geographical instruction in grammar school,
high school, college, and university ; improvement in the report-
ing of geographical and geological facts by staffs of the State
263
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XX111
WILLIAM MORRIS DAVIS-DALY
and Federal surveys; and improvement in the discussion of
grandson was to be a crusader, a champion for mental and
"terranes" by the more philosophically-minded historians and
moral probity, was assured by inheritance from parents and
economists.
grandparent.
Knowing that even a long life could not vitalize all the dry
As a boy Davis was retiring, little interested in sports, but
bones of the old geography, Davis specialized on physical geog-
engrossed in his studies. For several years before attending the
raphy, leaving to others the problem of systematizing the in-
local schools he was taught his lessons by his mother. She,
finitely varied responses of organisms to their environment,
like her own mother, knew well the power of words and laid
This other half of geography needs today a clarifying leader
much stress on their correct use; doubtless this early training
like Davis.
had much to do with Davis's rigor in developing a scientific
Davis was born in Philadelphia on February 12, 1850. At
vocabulary for his favorite science and his insistence on pre-
that time his father, Edward M. Davis, a business man, and his
cision of speech and writing by student or professional in-
mother, Maria (Mott) Davis, were members of the Society of
vestigator.
Friends and fully shared the best characteristics and activities
The boy was a good student and showed his mental calibre
of Quakers in full standing. Yet a hatred of injustice, which
by winning the Harvard degrees of Bachelor of Science at the
was to be an outstanding emotion of their son, led them into
age of nineteen and Master of Engineering a year later. He
rebellion against one of the ironclad rules of the Society. Not
immediately accepted a call to the meteorological service of
content with helping to operate the "underground railway" for
the National Observatory of Argentina at Cordoba. After
escaping slaves, Edward Mott enlisted in the Northern Army
three years of that routine work he returned to the United
For this action he was expelled from the Society of Friends
States. After a term as field assistant to Pumpelly in the North-
and soon after his wife resigned from it. To both of them
ern Pacific Survey, he was appointed (1877) to an assistantship
the question of States' rights was quite subordinate to the prob
in geology at Harvard, under N. S. Shaler, with whom he gained
lem of human freedom. To break with the Society's tradition
a permanent love for earth science. In those days promotion
took courage of the kind shown in the remarkable life of
was slow and from 1879 to 1885 he was listed as instructor in
Lucretia Mott, the mother of Maria Mott.
geology at Harvard, where he began a five-year term as as-
Theodore Tilton called Lucretia Mott, born in Nantucket
sistant professor of physical geography in 1885. In 1890 he
Massachusetts, "the greatest woman ever produced in this coun
attained the rank of full professor in the same subject. Nine
try." "She was the real founder and the soul of the woman's
years later he became Sturgis Hooper Professor of geology,
rights movement in America and England. She was the out
a position held until 1912, when he resigned, to be a Harvard
standing feminine worker in the struggle to rid our country
emeritus" for the remaining twenty-two years of his life.
of slavery. She advocated labor unions in a day when they were
He had two leaves of absence. In 1908 he was appointed visit-
proscribed and generally considered illegal. She proscribed
ing professor at Berlin University for a year, and, in 1911,
war, and worked diligently for liberal religion." Her crusad-
visiting professor at Paris for a year, during which he lectured
ing force "had its source in the love of freedom of her seafaring
also at several provincial universities of France.
ancestry, and she feared opposition or the exploration of un-
With his resignation Davis was freed from his responsibilities
charted regions of the mind no more than they feared to venture
as active Sturgis Hooper Professor and found the eagerly-
into unknown seas" (quotations from Anita Moffett in the
sought opportunity to make many postponed field studies both
New York Times Book Review, August I, 1937). That her
in North America and abroad, and also to make personal con-
264
265
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
tact with geographers and geologists and their respective work-
membership in the American Academy of Arts and Sciences,
shops. Because he had a philosophy to expound, he could not
the American Philosophical Society, the National Academy of
refrain from accepting many invitations to lecture at western
Sciences, the Imperial Society of Natural History in Moscow,
universities : California (Berkeley, 1927-1930) ; Arizona (1927
and the New Zealand Institute.
1931) ; Stanford (1927-1932) ; Oregon (1930) ; California In-
The Geological Society of America made him its acting presi-
stitute of Technology (1931-1932). With unfinished manu-
dent in 1906 and full-time president in 1911. He founded the
scripts on his desk at Pasadena he died in harness, on February
Harvard Travelers Club, of which he was president from 1902
5, 1934, seven days before his eighty-fourth birthday.
to 1911, and the Association of American Geographers, of which
The efficiency of Davis as a man of science was in no small
he was thrice elected president (1904, 1905, 1909). For his
part secured by domestic happiness. He was married three times
leadership and scholarliness he was chosen to be an associate
and twice he suffered by the death of a partner. In 1879 he
editor of "Science" and the "American Journal of Science."
married Ellen B. Warner of Springfield, Massachusetts; in 1914,
In 1886 he was awarded the H. H. Warner Medal "for scien-
Mary M. Wyman of Cambridge, Massachusetts; and in 1928,
tific discovery"; in 1895, another from the University of Paris.
Lucy L. Tennant of Milton, Massachusetts, who has survived
Later awards were: the Cullom Medal from the American
him. All three women were truly sympathetic helpmeets, as
Geographical Society (1908) ; a medal from the University of
the present writer knows from forty years of close association
Berlin (1910); a medal from the Harvard Travelers Club
with this man, who needed much freedom from the cares of
(1911) ; a medal from the Geographical Society of Philadelphia
a household while working for and in the world outside,
(1912) the Culver Medal from the Geographical Society of
The science of land forms, so intelligently enriched and or
Chicago (1913) ; the Kane Medal from the Philadelphia Geo-
ganized by Davis is a planetary science; his message was ad.
graphical Society (1913) ; the Hayden Medal from the Phila-
dressed to geographers and geologists of every nation. That
delphia Academy of Sciences (1918) ; the Patron's Medal from
those colleagues recognized the vitality and soundness of his
the Royal Geographical Society, London (1919) the Vega
evolutionary ideas is indicated by the long list of honors showered
Medal from the Swedish Geographical Society (1920) the
on him by foreign as well as American societies. He was elected
Locy Jagos Medal from the Hungarian Geographical Society
to honorary membership in the geographical societies of Am-
(1930) ; and the Penrose Medal from the Geological Society of
sterdam, Berlin, Budapest, Frankfurt, Geneva, Greifswald
America (1931). He became Chevalier of the French Legion
Leipzig, Madrid, Neuchatel, New York, Petrograd, Rome
of Honor. As Exchange Professor to France he was the first
Stockholm, and Vienna, as well as the Royal Society of Natural
American to give regular instruction at the Sorbonne.
History at Madrid, the American Meteorological Society, and
Davis was given four honorary degrees: S.D. by the Uni-
the Scientific Society "Antonio Alzate" of Mexico; to corre
versity of the Cape of Good Hope (1905) and by the University
sponding-membership in the Berlin and Paris Academies of
of Melbourne (1914) ; Ph.D. by the universities of Greifswald
Science and the Accademia dei Lincei; to corresponding-mem
(1906) and Christiania (1911).
bership in the geographical societies of Chicago, London
After his death the California Institute of Technology at
nich, Paris, and Philadelphia, and the geological societies of
Pasadena, where he had made many new friends, dedicated to
Belgium, Liverpool, and London and the German Meteorological
Davis a memorial "Gate of Knowledge," one of the entries to
Society; to foreign-membership in the Academies of Sciences
the grounds of the Institute, whose students and faculty he had
at Christiania, Copenhagen, and Stockholm. He was elected to
stimulated by his courses of lectures.
266
267
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
Work in Meteorology
some of the more dramatic and better understood processes that
Davis's interest in meteorology was doubtless aroused by his
mold the surface of our planet. But the young instructor knew
study of atmospheric conditions in Argentina, from 1870 to
full well that effective, authoritative teaching of geology, the
1873. Soon after his appointment at Harvard he undertook
principal subject of his first instructorship, demanded close
his first pioneering task, the creation of a systematic course on
personal touch with Nature. To get such experience he selected
the science of the atmosphere. This course became noted for its
for field study in detail the Triassic formation of New England
broad scope and for the clear, logical mode of presentation
and New Jersey. On those regions he published fifteen pre-
in these respects it had no rival in America and probably none
liminary papers (1882-1896), and a monographic summary of
anywhere else. Fortunately he was able to put the content of
most of his results in "The Triassic Formation of Connecticut"
the course in the permanent form of his "Elementary Meteor
(1898). This gave the first full account of the Triassic vol-
ology," published in 1894, when the course was turned over to
canic history of the region, announced criteria for proving the
Robert DeCourcy Ward, a capable, Davis-trained student, who
extrusive character of some of the "trap sheets" and the in-
greatly expanded the university offerings in meteorology and
trusive character of others. He also showed how the analysis
added courses in climatology. This development, together with
of topographic forms could be used in explaining the under-
the founding of the Blue Hill Observatory as a Harvard re-
ground, invisible structures of Connecticut and similarly faulted
search institution, was an abiding satisfaction to Davis and in
areas of the earth's crust.
cidentally freed him for other enterprises.
While working on the complex history of the Triassic areas,
The superbly designed and executed "Elementary Meteor
Davis interpolated field investigations: in Columbia County,
ology," for many years the best college text on the subject and
New York, and the Catskills, where he described the northward
still valuable in spite of the enormous increase of meteorological
continuation of the Appalachian structure; on the glacially-
data since 1894, illustrated its author's skill in compiling the
formed drumlins of New England and other regions; on the
best of the world's thought about the physics of the atmosphere
structure and origin of glacial sandplains and eskers; and on
and contained the results of his own direct observations. With
the geological history of Mount Desert Island. In later years
the help of volunteer assistants he carried on such field investi
he studied the origin of the thick and widespread Tertiary
gations as could be prosecuted in New England. The results
formations of the Rocky Mountain region, showing that these
were published in papers on thunderstorms, the sea breeze at
are not lake beds, as had been generally assumed, but are flu-
mospheric convection, and theories of rainfall. Other papers
viatile and alluvial-fan deposits; the origin and erosional history
with novel points of view were published on tornadoes, secular
of the Basin Ranges of the West; the development of the
changes of climate, and the wind systems of the oceans,
EGG
Colorado Canyon; the mechanical conditions leading to the
writings on thunderstorms and the sea breeze are "classic for
formation of limestone caverns; and the nature of geological
teachers of meteorology. Between 1884 and 1893 he published
proof, asking geologists "how do you know you are right ?"-
a question that illustrated the fact that he was as much concerned
forty papers on this general subject.
with the method of scientific thinking as he was in the majestic
Work in Geology
happenings of earth history. Yet Davis must have been con-
Not long after Davis became associated with the inspiring
scious that he made a principal contribution to the philosophy
Shaler, the two men published jointly a handsome volume The
of geology itself. His major contribution to earth science was
trations of the, Earth's Surface" (1881), intended to populariz
the conception of the "erosion cycle.' He applied it to
the
268
269
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
physiographic history of Pennsylvania, New England, the Rhine
and its inhabitants aid SO powerfully in observing and appre-
province, Turkestan, and many other, once-lofty ranges of moun-
ciating the facts of nature."
tains and proved that each of these regions had been reduced
"Geography has today entered well upon its third stage of
progress. The 'causal notion' is generally admitted to be essen-
by slow denudation to a lowland, to an "almost-plain" or "pene-
tial in the study.
Thus understood, geography involves the
plain." He further showed that after completion of a cycle,
knowledge of two great classes of facts: first, all those facts of
many an "old-mountain peneplain" was uplifted and again deeply
inorganic environment which enter into relationship with the
dissected by its rivers. With such demonstrations, phrased in
earth's inhabitants; second, all those responses by which the
the terms of his new geographical vocabulary, Davis made more
inhabitants, from the lowest to the highest, have adjusted them-
selves to their environment. The first of these classes has long
vivid than ever before the enormous length of geological time.
been studied as physical geography, although this name has been
No geologist who had carried the logic of the erosion cycle
used as a cover for many irrelevant topics. In recent years
into the interpretation of the major "unconformities" visible
there has been a tendency to compress the name into the single
in the strata of the earth's crust was greatly surprised when,
word 'physiography.'
"The second of the two classes of facts has not yet reached
later, the results of radioactivity in rocks gave a minimum age
the point of being named, but perhaps it may come to be called
of about two billion years to that crust.
ontography. Ecology, to which increasing attention is given by
biologists, is closely related to what I here call ontography, yet
Work in Geography
there is a distinction between the two, in that ecology is concerned
Davis gave much thought to the question as to the content
largely with the individual organism, while ontography is in-
of scientific geography, a subject which, because of the world-
tended to include all pertinent facts in structure, physiology, in-
dividual, and species.
wide problems of both war and peace, is likely to be in long-
"Neither physiography nor ontography alone is geography
continued demand in our colleges and universities as well as
proper, for geography involves the relation in which the elements
in secondary schools. In the first yearbook of the National
of its two components stand to each other. Each of the com-
Society for the Scientific Study of Education (1902) he wrote
ponents must be well developed before geography can be taken
up as a mature study."
"Geography as a mature subject is capable of a higher develop
ment than it has yet reached. In this connection it will be well
Davis held that "teachers of geography should be better
to review briefly the three stages of development recognizable in
taught"; that the subject should be treated more scientifically
the progress of our venerable subject. Until within about a hun-
both here and abroad; that it is far more than the "location of
dred years the content of geography consisted of a body of
uncorrelated facts concerning the earth and its inhabitants. The
things" that emphasis on principles rather than on items can-
facts were described empirically, and as a rule very imperfectly
not fail to foster the "intelligence as well as the memory" of
Their location was noted, but their correlations were overlooked
pupils in secondary schools that even in such schools the causal
it had not indeed been clearly made out that correlations existed.
notion should be stressed-"h and "why" as well as "where"
This blindly inductive first stage was followed by a second stage
which was opened by Ritter's exposition between the earth and
and "what," about things as we find them. "Elementary geog-
its inhabitants such relationships as were noted had to be
raphy may still deal with the salient facts and place man con-
explained on the old doctrine of teleology-the adaptation of the
spicuously in the foreground; more advanced geography may
earth to man-instead of on the modern principle of evolution
include examples of greater complexity, by always selecting
the adaptation of all the earth's inhabitants to the earth. It is
important rather than trivial matters; but the investigator must
this principle which characterizes the third stage of progress, and
study the trivial items along with the greater ones, and all must
along with it goes a principle of almost equal importance; namely
that all the items which enter into the relation between the earth
be duly scrutinized, described, and classified."
271
270
WILLIAM MORRIS DAVIS-DALY
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
The delay of the subject to reach mature treatment did not
In another place he wrote:
surprise Davis, who regarded it as "perhaps the most complex
"In whatever way a new mass is offered to the wasting forces,
of all sciences." Although he did not mention it, not the least
let us call the forces that uplift it constructional forces and the
forms thus given, constructional forms. Let all the forces of
of the complications in human geography is man's free will,
wasting be called destructional forces let the sea-level surface,
SO often obscuring his responses to physiographic controls.
down to which a sufficiently long attack of the destructional
Thus for more than one reason Davis himself did comparatively
forces will reduce any constructional form, be called the ulti-
little in illustrating his fundamental principle of relationship
mate baselevel ; and let the portion of geological time required
for the accomplishment of this task be called a geographical cycle.
between organisms and environment. He wisely restricted him-
Construction, destruction, baselevel and cycle are our primary
self to spade work on the inorganic side of the vast subject.
terms." (Journal of Geology, vol. 2, 1894, p. 72.)
In his chosen field Davis worked on the principle that, while
It should be noted that "cycle" is here used in the figurative
geology is the study of the past in the light of the present,
sense of a long period of time. The "plain" of extreme old age
physiography is the study of the present in the light of the
could never attain the form of the youthful stage, the greatly
past. The one science complements the other and it is no acci-
multiplied branches of the master rivers and also the inter-
dent that his influence on geological research has been at least
stream areas having individual slopes quite different from the
as great as his influence on geographical research.
general slope of the young plain, both in magnitude and azimuth.
On many occasions he told of his deeply-felt indebtedness
Thus at the ultimate stage of development of the ideal cycle we
to American geologists, particularly Lesley, the staff of the
have an almost-plain with a relief which, though gentle, is vastly
Geological Survey of Pennsylvania, and Powell, Gilbert, Dut-
more varied than the relief of the young plain. To this final
ton and Holmes of the great western surveys. It was while
form Davis gave the name "peneplain," which, like "cycle,"
reading their published writings that "geography gained a new
has won a permanent place in the vocabulary of physiographers
interest" for Davis. That interest culminated in the development
and geologists.
of his most famous idea, that of the "cycle of erosion." He
Similarly, Davis worked out the ideal cycle as a means of
visualized a structural unit in the terrestrial landscape and then
vividly describing the erosional changes suffered by terranes of
deduced the topographic results of erosion of this unit by rivers
much greater variety of initial relief, such as mountain ranges
born on its original surface or developed on the unit during the
and volcanic provinces. With sufficient study any actual unit
later, systematic evolution of its river system.
of the earth's topography can be interpreted in terms of the
erosion cycle, with its three dominating ideas, structure, process,
"The sequence of forms assumed by a given structure, the dur or
and stage.
ing its long life of waste is determinate, and
early
Nevertheless Davis knew well that the scheme of a simple
forms are recognizably different from the mature forms
young and the old forms. A young plain is smooth. The same region
cycle can rarely suffice for a full scientific description of land
at a later date will be roughened by the channeling of its larger
forms. He saw that at any stage of its history a topographic
streams and by the increase in number of side branches, until
unit may be affected by uplift or subsidence, with corresponding
it comes to 'maturity,' that is to the greatest variety or differen
effect on the power of eroding streams and on the fashioning
tiation of form. At a still later date the widening of the valleys
of reliefs. Thus the deductive scheme was enlarged to the
consumes the intervening hills, and the form becomes tamer
conception of multiple cycles, separated by "interruptions" due
until in 'old age' it returns to the simple plain surface of 'youth
to changes of level. Then, too, the landscape in question may
(National Geographic Magazine, vol. I, 1888, p. 15).
273
272
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
have had its drainage system affected by change of climate or by
ally selected fully agrees with the actual landscape before him.
volcanism-complications to which he gave the technical name
"accidents."
scription is thus greatly abbreviated."
concisely and effectively named in accordance with it; and de-
When the proper type is thus selected, the observed landscape is
In the Proceedings of the American Philosophical Society
(1902) Davis further explained his mode of thought as teacher
As he put the case in 1894, "one of the chief aids to sharp
and investigator in the following words:
outsight is clear insight." To illustrate, he cited the need of
The geographer "must generalize in order to bring the observ
special training for the maker of topographic maps.
able items within the reach of descriptive terms, and as soon as he
generalizes, the use of idealized types is practically unavoidable
Such types have long been in current use, but they have been
and the topographer must appreciate his subject before he
"Even the best surveys are necessarily sketched in great part;
too few and too empirically defined for the best results. They
sketch it. He must have a clear insight into its expression; can his
need to be greatly increased in number, and at the same time
outer eye must be supplemented by his inner eye."
therefore strive to complete a deductive geographical scheme
Let us
they must be correlated with structure, process, and time: for
only by following the path of nature's progress can we hope to
until it shall at last be ready to meet not only the actual
store our minds with types that shall imitate nature's products
variety of nature, but all the possible variety of nature."
It may be fairly urged that the larger the store of types a geog
Davis gave still another summary of the method he recom-
rapher possesses, and the more careful and numerous the com
parisons with nature by which the types have been rectified the
mended to the geographer who aspired to be truly scientific.
better progress can the geographer make in new fields of
The savage may do little more than observe natural happenings.
observation.
The barbarian may go a step further and invent hypotheses in
"But the geographer who adopts the explanatory methods in
explanation of those events; although his hypotheses are gen-
whole-souled fashion will find himself called upon not only to
erally wild, he may be said to have a two-faculty approach to
imagine a large series of type forms; he must also call into
exercise his deductive faculties and employ them to the fullest
Nature. The modern, well-trained naturalist takes four steps.
if he would make the best progress in the newer phases of his
He observes, invents, deduces, and verifies; he deduces the
subject, however purely inductive he has imagined it to be
In
consequences of each hypothesis and then goes back to Nature
setting up a store of types, there is need of deducing one type
to improve his deductive scheme and to verify the correct
from another at every step; and it may be confidently urged
hypothesis if he has been fortunate enough to create it. He
whoever hesitates to recognize this principle will fail of His
effort to describe through explanation. But as a matter of fact
has the four-faculty approach to Nature. Two generations of
geography has some time been more deductive than geographer
workers in earth science have benefited by Davis's insistence
have supposed it to be; and the newer phase of the science is not
on the value of multiple hypotheses, even "outrageous" hypothe-
characterized so much by introducing deduction for the first
ses, in search for the truth about the outdoor world. By such
time, as by insisting on its whole-souled acceptance as an essen
thinking all around the subject, that is, by inventing all of the
tial process in geographical research.
"It is only by giving the fullest exercise to the faculties of
more reasonable, conceivable solutions to the problem at issue,
imagination and deduction that the cycle of erosion becomes
the investigator is put on the alert. His field record becomes
serviceable. Here the geographer who hesitates is lost.
automatically charged with crucial observations and kept free
"Thus comparing the partial view of the landscape, as seen
from a load of hit-or-miss, unessential observations. Valuable
the outer sight, with the complete view of the type as seen by
as it is, the scheme of the erosion cycle is not so important for
his inner sight, [the geographer determines, with great savini
of time and effort, just where his next observations should be
research in earth science as the underlying philosophy, which
made in order to decide whether the ideal type he has provision
makes deduction no whit inferior to induction in the tool-chest
of the naturalist.
274
275
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
It seems equally clear that the application of Davis's method
version of a "glacial cycle," this to include evolutionary stages
of thinking about land forms is of great worth in the training
quite different from, though in some instances analogous to,
of young students. That method is based on the exercise of
the systematic stages demonstrated in regions exposed to normal
the imagination, the highest faculty of the mind it is the faculty
climatic conditions. From his field studies of the New England
of seeing things as they are and not as they appear to be
and other coastlines, supplemented by examination of large-
To develop it in the youth of school and college is the most
scale maps of continental and island shores the world over,
precious privilege of the teachers, and for this purpose few
Davis aided by his pupil, F. P. Gulliver, showed how shoreline
high school subjects are comparable with the evolutionary treat
forms can be systematized and scientifically described in the
ment of landscapes.
terms of the "cycle of marine erosion."
In 1889, five years after his first announcement of the cycle
Two masterly, advanced courses in physical geography, one
idea, Davis published the most remarkable of all of its many
on the United States and the other on Europe, claimed the un-
applications. The subject of this study is entitled "The River
ading admiration of those who listened. Illustrated with a
and Valleys of Pennsylvania." In this masterpiece of acute
host of large-scale topographic maps of States and European
reasoning and close observation in a complicated terrane he
countries, these lectures showed the solid worth of Davis's
traced the influence of a whole set of differing geological
philosophy, though in scholarly fashion he gave full weight to
tures on the development of highly varied land forms and
the opinions and methods of other investigators on the two
the associated river system. The results of this path-breakin
continents. Probably because of the difficulty of adequately
research make this early paper a classic, the conclusions
eproducing the maps around which the discussion centered,
which stand fast after more than half a century has added
the material of these unique lectures was never published. To
our knowledge of the Pennsylvanian region.
pread his gospel Davis relied chiefly on what he used to call
Other broad units of the earth's relief were similarly treated
the rapid-fire gun," propagandizing with hundreds of papers,
in scores of later papers. At first their author went into the
number of which were written in French and German and
more easily accessible fields which were already covered
by
rinted in Europe. To the teachers in secondary schools he
reasonably accurate topographic maps: for example, northern
offered his elementary "Physical Geography" (1898) and a
New Jersey, southern New England, and Virginia, Then
econd book, "Practical Exercises in Physical Geography"
a result of many visits to Europe and travels in central Asia
1908), but the only comprehensive statement of his matured
South Africa, Australia, and New Zealand, he tested, far and
philosophy was published in German with the title "Die Er-
wide, his art of describing land forms genetically, in terms 01
lärende Beschreibung der Landformen" (1912). In English
structure, process and stage. As he himself expected, he found
e have a convenient assembly of twenty-six among the more
new complications, but none that could not be fitted into the gen
important papers dealing with methods of teaching geomorphol-
eral scheme, so long as each. individual region is affected by
gy and with the general idea of the erosion cycle. This vol-
the normal climate. Arid regions, however, demanded different
me of nearly 800 pages was edited by the late Douglas W. John-
treatment, and, aided by the writings of Passarge and other
on, fellow member of the National Academy of Sciences, with
Davis worked out a scheme for "the desert cycle. His per
he title "Geographical Essays" (1909).
sonal inspection of the great topographic changes wrought
Not the least merit of Davis's papers and books is their pro-
mountain glaciation in central France, the Alps, Norway
use illustration with block diagrams, which tell his story with
our western Cordillera led him to an incomplete but illuminating
xxtraordinary clarity and conciseness. His sureness of pen-
276
277
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS-VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
stroke and his sense of values in selecting the essential features
tion and verification, but in the opinion of the present writer
of the thousand landscapes he pictured entitle him to the name
Davis failed to give adequate consideration to some of his prem-
artist. In this art no geographer nor geologist has ever rivaled
ises, including the geological dates when the reef foundations
him. Everyone who saw him do it marvelled at his simultaneous
were prepared and when the wave-resisting species of corals be-
use of both hands when drawing block diagrams on the black-
came abundant in the tropical ocean. Nor was sufficient attention
board-with amazing speed and practically without erasures.
paid to the relatively enormous areas and remarkable flatness of
In 1912 Davis resigned from the professorship of geology
the lagoons inside atoll and barrier reefs-features which are
which he had held for thirteen years, after having been Harvard's
almost universal and not to be expected on the Darwin-Dana
leading geographer for fourteen years. Thus for nearly thirty
hypothesis. It may further be remarked that this hypothesis is
years he had been a bridge-builder between the two sciences. It
not supported by the findings at test bore-holes in Bermuda and
was natural that he should be attracted to the problem of coral
at Michaelmas Cay and Heron Island inside the Australian Great
reefs, which is obviously in the border field. In 1914 a grant
Barrier Reef.
from the Shaler Memorial Fund of his university enabled him
Notwithstanding such failure to secure the premises on which
to visit many islands in the Fiji, New Hebrides, Cook, Loyalty,
the author of "The Coral-Reef Problem" based his own conclu-
and Society groups as well as Oahu, New Caledonia, and a long
sions, this book will long remain the Bible for geologists and
stretch of the Queensland coast inside the Great Barrier Reef of
geographers who need a richly illustrated handbook summarizing
Australia. In 1923 he added to his field experience by travel
the facts known about these marvelous structures of the coral
among the reef-bearing islands of the Lesser Antilles. For
seas, or are interested in the relation of the reef controversy to
twelve years his time was largely spent on the study of his own
the fundamental question as to the strength. and. stability of the
observations, of the multitude of island charts issued by the
earth's crust.
hydrographic offices of the world, and on the voluminous litera
Personal Characteristics
ture on the controversial subject of reef origin. At intervals he
published the results of his correlations, producing twenty-eight
Davis had a wonderful capacity for continuous labor. Great
papers and a book on the Antilles. In 1928 there appeared his
physical endurance helps to explain his keen zest for life as well
weighty monograph, entitled "The Coral-Reef Problem," giving
as his success in systematizing a world-embracing science. It
his complete views concerning the relative merits of the many
took zeal and courage to attempt wholesale reform of the geog-
hypotheses which have been offered as solutions to the reef
raphy taught before his time; both qualities were confirmed
problem.
as he saw his heresies become gradually accepted principles.
Davis was fascinated by the beauty and apparent cogency of
His favorite tool was logic. Although at heart he was capable
the Darwin-Dana view that atolls and barrier reefs are best re
of deep emotion, he would rarely allow emotion to appear in
garded as the products of slow subsidence of the foundations on
his writings or in his college lectures. Partly for this reason
which these structures are built, and at first (1915) thought the
the writings did not appeal to the general public, nor the lectures
subsidence hypothesis to be alone competent in explanation
to the rank and file of Harvard students. Davis was some-
Later he accepted the idea of "Glacial controls" as useful in
times severely critical of student or colleague who, in order to
accounting for the "platform foundations" and crowning reefs ii
lighten style of presentation, used simile, metaphor, or other
the marginal areas of the earth's coral-reef zone. His treatment
figure of speech which could in the least obscure orderly expres-
of the problem was dominated by the double principle of deduc
sion of the thought. Rigorous with himself, he was rigorous
278
279
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS--VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
with his students. He detested sloppiness and made disciplined
KEY TO ABBREVIATIONS USED IN THE BIBLIOGRAPHY
thought and precision the outstanding aims of his courses in both
Am. Ac. Pr. = American Academy of Arts and Sciences Proceedings
college and graduate school. Yet he was sympathetic with honest
Am. Assn. Pr. = American Association Proceedings
endeavor and spent much time and energy helping special stu-
Am. Assn. Adv. Sc. Pr. = American Association for the Advancement
dents who through no fault of their own, had not been properly
of Science Proceedings
prepared for imaginative and logical attack on scientific problems.
Am. G. = American Geologist
Am. Geog. Soc. Bull. = American Geographical Society Bulletin
By his Quaker upbringing Davis was endowed with a high
A'm. Geog. Sp. Pub. = American Geographical Special Publication
ethical standard. As we have already noted, his family was
Am. Geophys. Tr. === American Geophysical Union Transactions
forced to leave the Society of Friends, but Davis kept one con-
Am. J. Sci. = American Journal of Science
crete relic of that early association. Even into old age he ad-
Am. Met. J. = American Meteorological Society Journal
dressed each member of his own family with the pronoun "thee."
Am. Nat. = American Naturalist
Perhaps this habit of speech was rooted so deeply because of a
Am. Ph. Soc. Pr. = American Philosophical Society Proceedings
An. Rep. Astron. Obs. Harvard Coll. = Annual Report of the Director
scene witnessed during his plastic childhood. Then he heard a
of the Harvard Astronomical Observatory
Quaker boy, fighting with another boy who was not of the
An. Géog. = Annales de Géographie
Friends, intersperse his blows with the taunt "Thee little. You,
Assn. Am. Geog. An. = Association of American Geographers Annals
thee!" The influence of his forbears was particularly shown in
Atl. Mo. = Atlantic Monthly
Biog. Mem. Nat. Acad. Sci. = Biographical Memoirs, National Academy
Davis's craving for fairness and justice in the world and in his
of Sciences
religious tolerance. He used to say "Who am I to 'tolerate
Boll. R. Soc. Geog. = Bollettino Royal Società Geografica
anybody's belief I. want to respect it even if I cannot agree.
Boston Soc. N. H. Pr. = Boston Society of Natural History Proceedings
He affiliated himself with the Unitarian church. Two months
Brit. Assn. Adv. Sci. Rep. = British Association for the Advancement of
after his death his last paper, "The Faith of Reverent Science,
Science Report
Bull. Volcanologique = Bulletin Volcanologique
was published. He there declared his ideal for the human race
Calif. J. Mines and Geol. = California Journal of Mines and Geology
progress ever upward "to a truly Christian standard."
Conn. Sch. Doc. = Connecticut School Document
Ed. Rev. = Educational Review
Eng. Mo. J. = Engineers Monthly Journal
Franklin Inst. J. = Franklin Institute Journal
Geog. Anzeiger = Geographischer Anzeiger
Geog. J. = Geographical Journal
Geog. Rev. = Geographical Review
Geog. Soc. Phila. Bull. = Geographical Society of Philadelphia Bulletin
Geog. Teacher = Geography Teacher
G. Assn. Pr. = Geologists Association Proceedings
G. Mag. = Geological Magazine
G. Rundschau = Geologische Rundschau
G. Soc. Am. Bull. = Geological Society of America Bulletin
G. Soc. 'Am. Pr. = Geological Society of America Proceedings
Ges. Deutsch. Naturf. u. Ärtze = Gesellschaft Deutscher Naturforscher
und Ärtze
Ges. Erdk. Berlin Zs. = Gesellschaft Erdkunde Berlin Zeitschrift
Goldthwaite's Geog. Mag. =Goldthwaite's Geographical Magazine
280
28I
NATIONAL ACADEMY BIOGRAPHICAL MEMOIRS--VOL. XXIII
WILLIAM MORRIS DAVIS-DALY
The Geographic Cycle. Paper Read at the VII Intl. Geog. Congress of
Field Work in Physical Geography. J. Geog. I : 17-24, 62-9.
Berlin. Verhandl. d. vii Internat. Geog. Kongr. Berlin. 1899 (1900).
The New England States. Boston. Supplement to Frye's Complete
22-31.
Geography. [Also 1895 edition.]
Glacial Erosion in France, Switzerland and Norway. Boston Soc. N. H.
The Progress of Geography in the School. Chicago, pp. 49. (In National
Pr. 29: 273-322.
Society for Scientific Study of Education. Ist Yearbook, Pt. II :
Glacial Erosion in the Valley of the Ticino. Appalachia ix: 136-56, pls.
River Terraces in New England. Harvard Coll. Mus. C. Z. Bull. 7-49.) 38
15, 16.
(g S 5) : 281-346.
History of the Cincinnati Anticline (discussion). G. Soc. Am. Bull.
Systematic Geography. Am. Ph. Soc. Pr. 4I: 235-59.
II: 604-5.
Local Illustrations of Distant Lands. I. A Temporary Sahara. J. Sch.
The Terraces of the Westfield River, Mass. Am. J. Sci. (4) 14: 77-94.
Geog. 4. no. 5: 171-5.
1903
Notes on the Colorado Canyon District. Am. J. Sci. (4) IO: 25I-9.
Block The Basin Ranges of Utah and Nevada (Abst.) J. G. II : 1201.
Note on River Terraces in New England. (Abst.) G. Soc. Am. Bull.
301; G. Soc. Am. Bull. 14: 551 ; Eng. Mo. J. 75: 153.
Mountains of the Basin-Range Province. (Abst.) Science n.s. 17:
12: 483-4.
Peneplains of Central France and Brittany. (Abst.) G. Soc. Am. Bull. 12:
The Blue Ridge in Southern Virginia and North Carolina. (Abst.) J. G.
II: 121.
481-3.
Physical Geography in the High Schools. The School Review 8: 388-404,
The The Blue Ridge of North Carolina. (Abst.) Science n.s. 17: 220.
449-56.
Development of River Meanders. G. Mag. (4) IO: 145-8.
The Physical Geography of the Lands. Pop. Sci. Mo. 57 : I57-70.
Effect of Shore Line on Waves. (Abst.) Science n.s. 15: 88; G. Soc.
Physiographic Terminology with Special Reference to Land Forms. Sci-
Am. Bull, 13: 528.
ence II : 99.
An Excursion to the Plateau Provinces of Utah and Arizona, Harvard
Practical Exercises in Geography. Nat. Geog. Mag. II : 62-78.
Coll. Mus. C. Z. Bull. 42 (g S. 6) : I-50.
The Fresh-Water Tertiaries at Green River, Wvo. (Abst.) Science n.s.
1901
17: 220-221 ; G. Soc. Am. Bull. 14: 544; J. G. II: 120.
The Causes of Rainfall. J. N. E. Waterworks Assn. 15: 338-50.
The Mountain Ranges of the Great Basin. Harvard Coll. Mus. C. Z. Bull.
An Excursion in Bosnia, Hercegovinia, and Dalmatia. G. Soc. Am. Bull.
42 (g S. 6) : 129-77.
3: 21-50, pl. I-4.
Practical Exercises in Physiography. J. Geog. 2: 516-20.
An Excursion to the Grand Canyon of the Colorado. Harvard Coll. Mus.
The Question of Seminars. Harvard Grad. Mag. 8.
C.Z. Bull. 38 (g S 5) : 107-201 ; (Abst.) G. Soc. Am. Bull. 12: 483; G.
A The Scheme of Geography. Geog. J. 22: 413-23. London. pp.
Mag. (4) 8: 324; Science n.s. 13: 138.
The Geographical Cycle. Int. Cong. Geog. VII, Verh. Pt. 2: 221-31,
213-44. Stream Contest Along the Blue Ridge. Geog. Soc. Phila. Bull. 3:
Local Illustrations of Distant Lands. J. Sch. Geog. 5: 85-8.
Walls of the Colorado Canyon. (Abst.) Science n.s. 15: 87; G. Soc. Ain.
Maps of the Mississippi River. J. Sch. Geog. 5: 379-82.
Bull. 13: 528.
Note on River Terraces in New England (Abst.). G. Soc. Am. Bull. 12:
1904
483-5.
Peneplains of Central France and Brittany. [Abst.] G. Soc. Am, Bull
A Glacial Flat-Topped Range in the Tian-Shan. Appalachia IO
Erosion in the Sawatch Range. Colo Appalachia IO: 277-84.
12: 481-3, pls. 44-5.
Practical Exercises in Physical Geography. Proceedings Annual Confer
Geography in the United States. Am. G. 33 156-85; Am. Assn. 392-404. Adv. Sc.
Pr. 53.
ence N. Y. State Science Teachers Association, Albany, II pp.
Les enseignements du Grand Canyon du Colorado. La Géographie, 4
The Relations of the Earth Sciences in View of Their Progress in the
Nineteenth Century. J. G. 12: 669-87.
339-35I.
A Summer in Turkestan. G. Soc. Am. Bull. 36: 217-28.
1902
Base Level, Grade and Peneplain. J. G. 10: 77-III.
1905
Elementary Physical Geography. Boston. Ginn and Co. vviii + 40T pp
The Bearing of Physiography Upon Suess' Theories. Am. J. Sci. (4) 19:
[Also 1926 printing.]
265-73; (Abst.) Int. Cong. Geog. VIII, Rp.: 164.
292
293
Catalog #:
GRCA
14865
Object:
Letter
Description:
Letter to Pete Berry from William Davis. One sheet, typed
back and front.
Dated Cambridge, Mass, 28Mar1901. Requests info on trip to
Cataract Canyon, "home of Supai Indians", such as time needed, difficulty,
horses or wagons. Wonders about also getting to Red Butte, Aubrey Cliff's, with
Berry as guide. Possible trip in July, white paper, black type. Also see GRCA
14866 and 14875.
Manufact. Date:
03/28/1901
Catalog #:
GRCA 14866
Object:
Letter
Description:
letter from William Davis to Pete Berry, from Cambridge,
Mass, 28Apr1901. Answering Berry's letter of April 6. Afraid it's impossible
to make trip to Aubrey Cliffs, but hopes to get to Red Butte and possibly
Cataract Canyon. Will sent word in June to give more definite number of party
size. On white half sheet. Typed in black ink. Signed in blue ink. Also see
GRCA 14865 and 14875.
Manufact. Date:
04/28/1901
Catalog #:
GRCA
14875
Object:
Letter
Description:
Letter from William Davis, Cambridge, Mass. to Pete Berry.
On 1/2 sheet, typed, signed in black ink. Dated 31Jul1901. Says he's arrived
home safe. Enjoyed trip to Grand Canyon, Grandview Hotel. Will send as many
friends as possible. Is missing box of photo film, possibly lost on trail or in
yard. Also tells Berry that if he can help "in your relations to the Santa Fe
RR. , or otherwise" he should write. See GRCA 14865-66.
Manufact. Date:
07/31/1901
Catalog #
GRCA
59048
Object:
Report
Description:
"Miscellaneous papers on Grand Canyon Physiography" by
William Morris Davis. Includes "An Excursion to the Grand Canyon of the
Colorado" and "An Excursion to the Plateau Province of Utah and Arizona". Black
and white photos, illustrations, hardcover.
Manufact. Date:
May1901; June1903
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Davis, Wm M. (1850-1934)
Details
Series 2