North America
rred to relate to the geography of fisheries, forestry, mining, commerce, agriculture, etc. In discussing each of these themes, the control exerted by natural
a view of political adjustments not usually taken and in a way perhaps pessimistical, which may awaken opposition, and also because it contains a summary of the results of a long series of struggles among various nations for the possession of the North American continent. Of greater moment than the rivalries of nations for territory, as is also outlined, is the conflict between two radically different principles of govern
re the territorial limits of nations. For this reason the characteristics of boundaries a
ATION OF
ified, at least provisionally, in six groups. We may term these groups coast boundaries, astronomi
ion of a country bordering on the "high seas" is a line one marine league seaward from the margin of the land, and following its meanders. As an international dividing line the one-league limit seldom, if ever, becomes important, since the nice adjustment of the width of an arm of the s
y astronomers, and if the monuments or other marks employed to show the positions of such lines are removed they can be accurately relocated. The lines referred to are prin
by the boundary between Canada and the continental portion of the United States from near the Lake of the Woods westward to the coast of the continent, which, as finally decided in a treaty between Great Britain and the United States in 1846, is the forty-ninth parallel of
ey pass. They can be located with precision and their courses accurately marked by monuments. For these reasons astronomical boundaries, when clearly de
coast-lines, etc. They may divide a fruitful valley in a most arbitrary and inconvenient manner between two nations with widely different laws and customs, or cross a navigable river at several localities, and intersect a coast or lake shore so as to initiate complex conditions in respect to harbours, navigation, customs duties, etc. In these and still other ways boundaries coinciding with lines of latitude and longitude are apt to bring about detrimental commercial and other relatio
ution of governmen
illed geodesists, it cannot be located even approximately by miners, trappers, f
dent that its far-reaching and perhaps highly complex influences on the development of neighbouring peoples are likely to be such that the natural resou
ce between nations and states; collectively, such boundaries, typically represented by a river without islands, flowing between well-defined and permanent banks, may conveniently be termed water boundarie
e of the St. Lawrence River, and divides medially several of the Great Lakes and their connecting streams. The south boundary of the United States is
part, the middle line of the Hudson and of New York Bay, etc., with several qualifications, including exclusive jurisdiction by New York over all the waters of the Hudson to the west of Manhattan Island to the low-water line on the New Jersey shore, subject, however, to certain rights of property and of jurisdiction of the State of New Jersey, etc
ns inexperienced in the method of surveying. Coinciding, as they generally do, with definite geographical divisions, they do
as a boundary, the question as to which of two channels is really the larger or the deeper may not permit of definite answer. Streams are subject to many changes, and what is the main channel one year may become of secondary rank the next year, or a river, as not infrequently happens, may shift its course bodily, and thus furnish grounds for contention as to the ownership of the territory transferred from one of its banks to the other. The distributaries of streams,
ownership of certain islands in the Strait of Georgia; the immediate subject of contention being whether "the channel which separates the continent from Vancouvers Island," as the statement reads in the Webster-Ashburton treaty, 1846, passes to the east or to the west of t
jectionable. The difference lies in the nature of the streams themselves, and illustrates the fact that, with water boundaries as with other classes of dividing lines betwee
p crest-lines, are in reality broad plateaus or great domes, deeply dissected by stream erosion. In such instances it is frequently difficult to decide where the crest of the range is located. Indeed, as is not infrequently the case, there is no definite and tangible crest-line. Although it is sometimes assumed that the crest-line coincides with the water-parting, or the divide, between the head branches of streams flowing in oppo
wing to the Atlantic and those discharging into the Pacific. Post-treaty surveys, as they may suggestively be termed, have shown that in the portion of the Andes in question streams rising well to th
direction or another according to the strength and other qualifying conditions of the opposite-flowing streams. Then, too, an uplift which seems to a casual observer to be a single mountain range, may in reality be highly complex, and no continuous crest-line be discoverable. In short, the sweeping statemen
even by persons unskilled in the art of surveying, and for this and other reasons has much to commend it; yet, without an accurate knowledge, and most of all an accurate topographic map of the region t
ty. Then, too, the process of head-water corrasion pertaining to essentially all streams, and of stream capture, or the acquiring by one stream, through the process o
and serves its purpose well; but the satisfaction it has given is to be qualified by the fact that, for the most part, it is situated in a
in commendable features in common; they are easily located, readily defined by natural features of the earth's surface, and in general
aries, the ones here considered are imaginary lines, and, in part, might with propriety be included in that class, since they are capable of being located by astronomical methods; but they serve our purpose better if considered in a group by themselves. The class of boundaries here referred to includes straight lines connecting two points; l
t of the District of Columbia, a rectangle 10 miles square was chosen and marked on the ground by means of monuments as the site of the capital of the United States. Another illustration is furnished by the eastern boundary of California, as defined in its constitutio
of straight lines, not of great length, or small geometrical figures, are difficult of precise location, even by ski
s the one hundred and third meridian of west longitude, but owing to errors in the first survey was wrongly marked on the ground by monuments. The monuments, however, having been accepted as indicat
effort is made to adjust them to the natural conditions of the immediate territory they traverse; but, for the purpose of expressing a still greater weakness inherent in them, they are here specially designated as impracticable boundaries. This, as is to be hoped, temporary cl
stance of 10 marine leagues therefrom." The region through which the line described would pass, if surveyed, was almost entirely unknown at the time the treaty referred to was made, but, as has since been discovered, it is exceedingly rugged, and contains many mountains ranging from 10,000 to 18,000 feet high, besides a multitude of glaciers and many extensive fields of perpetual snow. To survey and mark on the ground the boundary indicated in the tr
Characterist
mage to
shire, which is a line parallel to the Merrimac River, and distant from it 3 miles on the north. In this case, although the distance of the line designated from the one to which it is to be drawn parallel is
he desirability of accurate geographical knowledge, and still more of an adequate appreciation of the difficulties
ter several subsequent adjustments, was determined as indicated roughly on the accompanying map. Throughout
e north and south from Ause Sableu on the said coast to the fifty-second degree of north latitude, and all the islands adjacent to that part of the said coast of Labrador." This line is still unsurveyed. From the fift
y for some 900 miles, namely, the middle of the Rio Grande, or its deepest channel, when there is more than one, to where the river crosses
of Mexico, the republics of Central America, etc., are indicated approximately on the accompanying map. These lines
ICAL
ction and final disappearance of Spanish and French dominion from the continental mainland. The broad, indefinite territory once belonging to Spain, which in the sixteenth century seemed destined to expand still more and possibly embrace the whole of the two Americas, has been diminished from time to time, until as a result of the recent Spanish-American War her flag no longer waves over any portion of the New World. The French territory,
anadian boundary, together with Alaska, Cuba, San Domingo and Haiti, and Porto Rico. The provinces, islands, etc., still controlled by European powers are Canada, Newfoundland, Bermuda, and all of the West Indies except the islands just referred to, which are more definitely designated in the table on page 424. The population of the American republics is in the neighbourhood of 97,000,000, and of the European dependencies somewhat less than 7,000,000.
ese, since about 1870, have arrived in large numbers, but their immigration to the United States is now restricted. Of the nations of Europe, the strongest influx has come from Great Britain, France, Germany, Spain, and Italy. To a marked degree this westward migration has been along parallels of latitude, but the migratory streams
lands. To the south of the United-States-Mexican boundary, but beginning in the southwestern portion of the United States, and including also the greater part of the population of the West Indies,
forests, mines, fisheries, etc. More than this, even if all material wants are supplied from within its own border, intellectual desires demand outside stimuli. The ideal nation should therefore touch the ocean, in order to have avenues for travel open to its peop
ines are entirely arbitrary, so far as relation to soil, climate, mineral and timber resources, fisheries, etc., are concerned. The line separating Alaska and Canada is mainly a meridian of longitude, which passes through a rich mining district. The southern boundary of Canada is for the most part a parallel of latitude dividing agricultural, mining, and timber lands. The material advancement of the inhabitants on the opposite sides of these unnatural dividing lines is retarded by them and
ntellectual decline, is sadly illustrated by the subdivision of the West Indies. In an admirable account of the Caribbean region by R. T. Hill, in whic
e island of St. Martin, not as large as an average county in the United States, is divided into two principalities, the French and the Dutch, each of which maintains an administrative force as large as that of the State of Texas. Then, as we sail down the eastern islands, hardly a score in number, and within sight of one another, aggregating in area less than our little State of Delaware, about 2,000 square miles, we find five foreign and no less than a dozen distinc
a should be the shore boundary, except at the 30-mile-wide Isthmus of Panama. To the geographer North America presents an example of a region containing within itself essentially all of the elements necessary to a high industrial, social, educational, and ethical development of its inhabitants. The industrial needs are met by a range of products, whether of soils, mines, forests, or fisheries, as varied or nearly so as is presented by the entire earth. Although the continent is broadest at the far north, where climatic extremes prohibit a dense population, yet in the temperate region,
litical subdivisions during the year 1900, is indicated, as nearly as
OF NORTH AM
a in square mil
an Gov
of Alaska and Porto Ric
67,005 1
[8] 63,40
[9] 7,22
a 49,200
10] 45,25
a[11] 23,
ent of Colombia
o[13] 20,5
3] 9,24
,000 1,
- -
n governments 4,6
ll held by Euro
f Great Britain
,653,946
and Labrador
da 19
mas, Jamaica, etc
onduras 7
- -
ited Kingdom 3,7
an
nd St. Pie
loupe, Martinique,
- -
France 1,1
nm
mas, St. John, and S
ll
in in part, St. Eusta
- -
an governments 3
=== =
America 8,412,
of Porto Rico is 3,600 square miles; its population (1899), 953,243. Hawaii, n
In
In
In 1
In 1
In 1
ing the island Sant
ERA
us of the Un
ors. Published by Kegan Paul, Tr
Canada and Newfoundland, by S. E. Dawson. Vol. ii, The United States,
the other West India Islands. Th
. United States Geological Survey, Bulletin
N
ines,
Wash., hei
tains, brief ac
d for bri
12, 21. Work of, in
opulation of, 424.
ography o
ns of
coast
mercial Co
Sound, ori
ands, topogr
rief account
ef account
an syst
A., cited,
flora,
nments, enumer
life, 2
nal val
ains, brief acc
the aborigi
ite,
ns, description of,
period,
Maya hou
matic prov
c life r
rious gover
au, brief acco
os, 34
l boundarie
in, 62-64. Forest, b
ns, 60,
atic provinc
rders o
dvancemen
ief account
nds, topogr
Wash., hei
N. B., he
orge, refere
s, absence of
tt Dee
t compl
ndy, tide
Pola
account of,
explorat
a and popula
a Mount
ea, dept
ief account
f Californi
rations,
f account o
of, 275-278. Map sh
ndians, lod
s of Dakot
rovince, 201-203.
., Mo., he
lassification
s, area and pop
on Dee
ief account
, 225
a, bounda
system,
pulation of, 424. B
of Western
f Indians b
Ranges, 168. Ro
Hatteras, continenta
epth of wat
n, tide
, N. M., hei
rundu
, submarine topo
ief account
account of, 147-158. Ig
canaden
ite, 3
f account
in Pacific
nations, 424. Of
ica, Indians
, T. C., c
lime secre
ological hi
ake, Wash
Bay, orig
saw pl
inds, 115
daries, 408-418. Geolo
ys,
214. Elements
provinces
38. Fields,
plains
es, 409. Mount
phy of,
River lav
l geology
lings of Indi
f mineral subst
rainage, exa
ines with foreign
description of, 8
, cited, 26
nental shelf, 6. Reefs
ndum
rea and popul
brief account of, 1
W., cit
opulation of, 42
the aborigi
s, ocea
es, 20
sses,
, cited, 36
D., cit
. M., ci
J. W., c
lley, Ca
ng continent
the West In
f account
ary of, 416. Ba
merged cha
as,
possessio
es,
., cited, 15
, brief acco
undaries,
Eskim
er-valleys,
., cited, 13
geology
Tex., brief acc
do, brief accou
a mari
Bay, Alaska,
g of the word,
of the t
count of, 365-376
ries,
al studies
tion, 2
Atlantic coas
ns,
n Pacific f
, 215
inental shelf
W. M., c
y of India
ption of, 217-2
flora
sessions of
ng animal
destruction of,
the India
atural
Penins
stribution of a
gy, 2
K., cited, 1
ount of, 314-316. Extent
, Wash., hei
sand
referenc
351-352. Mounta
palace, Uxm
e Colorado, 134-1
., cite
o, referen
account of, 18. Basin,
map o
es,
ef account
ief account
e, Utah,
California
St. Law
he continen
ea and popula
of Mexico, continental
ap of west c
ief accoun
eam
lume, etc.
Indian
and popula
urs,
S. D., elev
an Isl
and populat
F. V., c
. W., ci
, A., ci
tains, Uta
W. H., ci
hy Valley,
, brief accou
ed, 22, 169, 220
possessio
, cited, 390,
ea and popul
Ore., hei
W. T., c
e by Indian
ns, 387-394. In
submerged chan
A. von,
T. H., c
rbons,
ts due to, 50-51. Su
is on continen
Montre
of, 316-326. Terranes, econ
le boundari
t of, 376-406.
United States and
ning of the
ief account
e sheets
untain,
res, 3
houses o
ractised by
, referenc
ds, 3
ars,
erms,
., referen
terrace
a., submerged
ent, refer
eak, Nev., h
t., Ore., he
W. D., ci
-tree
ayka
a, life
t., Me., he
s, 37
ny penep
F. H., c
, Alaska, i
ry of, 418. Topo
ths, 13
brief accou
enclose
ges, 3
poken in A
s, brief account of
., cited
x, L., ci
ental shelf, 10-16
d life-zon
ones,
Bank, brief
acado, El
lackfoot I
Yukon, hei
of Iroquoi
n, Tenn., secti
ountai
climatic pro
ascent of Mt.
anadens
River, del
., Alaska, h
olia
p of coas
es peculiar to A
ssification
t., N. H., h
N. Y., hei
l,
., cited, 3
tts, bound
es terr
house
culture
re., 153-155.
a, 27
s, the
mephiti
H., cited, 1
ver, bounda
324. Terranes, economic
ism, natu
opulation of, 424.
ns of
a,
of birds
etained by
map of, 53. River
e Bay
, definit
f account o
H., cited
413-414. Sheep, brief
, 27
n, cited,
ox, 2
nk, refere
life rea
thic,
syste
J. S., c
ick, mount
, boundary in r
, mountains
opulation of, 424. Conti
rights
on over La
ire, bound
of, 411-412. Subsid
ry of, 411-412.
ea and popula
ki?ld c
life re
me Mount
untains, W
marbl
ak,
position
he aborigin
er,
a Mount
, descriptio
238-249. Mountai
lithi
, 220
and populat
ntains,
ies,
definitio
ia, bounda
. A., ci
eum, 3
c divisions,
plateau,
32-233,
Ore., hei
y winds,
life,
treeless
inum
ristics of, 253.
ption
ic plu
, life in the sea ne
bear
ol, 419-424. Ge
of North Am
rea and popul
d by European g
, submerged c
, work of in Car
ed, 90, 104, 124,
ief account
s, brief acco
. H., refer
nodon
India
los,
sin, 158-161.
of,
Lake, Ne
., photograph of,
esa, N.
ts of Califor
in Alas
f the Meso
s, Ameri
sed by Indi
deltas
ief account of, 122
H. D., c
an Company, 37
, height of, 166. Elev
volcan
ountains, Mo.,
t., Wash., he
N. B., tid
, 55-56. River, subm
retained by
, 34
ea and popul
te Island,
area and popu
Bay, Cal., o
Islands,
s Park,
ills,
one, 3
lina Islan
z Island,
area and popu
a Island,
C. S., ci
C., maps com
penepla
or Indian
P. L., ci
Ore., heig
ns, 1
lls of Dakota, 117. Look
unt of, 306-316. Terranes, ec
242, 244-246. Semp
ah penep
lanca, N
och, menti
ains, Cal., brief a
ee De
346. P
ns of New
f account o
. M., refere
er possessi
gnum
me music,
untains,
hanges in coast-li
orest plain
river chan
rainage, exa
es of coa
nt mounta
-pine
drainage, exa
ver, submerged
, N. B., he
l mounta
e, Cal.-N
c,
ap of co-tidal
Indians,
s of California co
C, cit
storms,
-30. in r
r-lin
Indian
y of coas
does,
limatic prov
hent, refer
, 254-257. Plains, bri
province, 186-191.
ief accoun
H. W., c
. B., cite
Ore., heig
om, possessi
d population of, 424.
f Indians b
c Survey, referen
n, reference t
climatic pro
tan, panora
firs of, 241. Moun
C. R., c
voyage
f, referen
a creep
mountains
oes, 3
. R., cite
ef account
F., cit
Mt., N. H.,
ies, 411-413.
an hurric
d population of, 424. French
ns of
division o
winds
D., cit
. C., ci
Nev., heig
ns, N. H., fo
t., N. Y., h
J. D., ci
., Cal., he
Bailey,
lanetary
a Lake, N
ef account
w pin
Valley, C
l shelf bordering,
ver, del
i,
E
f Corr
k pages have been delete
ndered consistent on a
f such pairs when repeat
isher's errors were co
Corre
ous and silici
bbean[Ca
and the Carribean[
nown[better known] por
rd and resist
ho]!" is no m
tation[precipita
], Lake Louise
s phase of volcani
southestern[southe
thus exposed
more criticial
th remarkable unf
d with moderate s
calente[cali
vilization
to the family Mu
lar[peculiar] ho
plaiting] of bas
[Subsoil], i
[Mephitis] me
quelon], retaine
Fran?ois] Mountai
lóvioff], I. M.,
lens], Mt., Wash.
ti], brief acco
to be