Modern GeographyNewbigin, Marion I. (Marion Isabel)
Science
Modern Geography
Newbigin, Marion I. (Marion Isabel)
Geography
We must connect these facts directly with the peculiar distribution of
land and water in the northern hemisphere, which made free intercourse
possible, alike for the land animals and for man. The importance of this
intercourse may be suggested in a few words. When a group of organisms
is limited, from whatever cause, to a particular zone of the earth's
surface, the members of the group tend to acquire characters fitting
them for this restricted area. But if the area is open, constantly or
periodically, to incursions of organisms from adjacent areas, then, with
the widening of the environment, and the greater intensity of the
struggle for existence, evolution is quickened and new characters
appear. The men of the Eurasian continent learnt, on the fierce
battle-grounds of that continent, lessons which enabled them to conquer
without difficulty the more isolated human groups of the southern
hemisphere. The fact that they took south with them the mammals of the
north, who also have thriven at the expense of the native forms, shows
that the hold of the southern animals upon their habitat was no less
precarious than that of man himself.
One other point is worth notice in connection with the distribution of
land and water over the surface of the globe. We have seen that the
northern hemisphere is the region where organic evolution has been most
marked. It is, as it were, a great biological laboratory. On the other
hand, in the southern hemisphere, which has fewer land masses to
interfere with the circulation of the atmosphere, many physical
phenomena occur in a more marked and orderly fashion than to the north.
The westerly winds of the south blow with a force and a constancy which
makes it impossible to compare them with the more variable westerlies of
the north. Even the ocean currents of the south seem to show more
constancy than those of the north. If the northern hemisphere is a great
biological laboratory, the southern may be described as a physical one,
and one of the great interests of the further exploration of the
Antarctic is that it will probably cast light upon some important
meteorological problems. (See Dr. W. S. Bruce's volume on _Polar
Exploration_.)
The distribution of land and water, with all its effects on climate and
on the distribution of life, is, as we have seen, caused by the main
features of the relief of the earth, by the existence of vast
depressions in which the water accumulates, and of relative elevations
from which it flows. But the minor details of relief, hill and valley,
ocean depth and continental shelf, are also important, and exercise a
very marked effect upon distribution. They therefore demand in their
turn some consideration.
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