The Popular Science Monthly, June, 1900: Vol. 57, May, 1900 to October, 1900Various
Science
The Popular Science Monthly, June, 1900: Vol. 57, May, 1900 to October, 1900
Various
Science -- Periodicals; Technology -- Periodicals
The sufficient justification of the demand that has now arisen for
explanation and correlation in the study of land forms is found in the
repeated experience that until an explanatory description of a region
can be given, one may be sure that some of its significant elements
pass unnoticed; and until the controls that it exerts on living forms
are studied, one may be confident that its geographical value is but
half measured. A sentence from Guyot’s Earth and Man may here be taken
as a guide: “To describe, without rising to the causes, or descending
to the consequences, is no more science than merely and simply to
relate a fact of which one has been a witness.” There could hardly
be devised a more concise and searching test of good work than this
quotation suggests. The causes, in so far as the physical geography of
the lands is concerned, have been learned chiefly through the study of
geology; yet it does not by any means follow that all geologists are
possessed of such knowledge of these causes as will constitute them
geographers. The consequences have been learned through the study of
evolutionary biology; yet a distinct addition to the usual discipline
of biology is required in order to apprehend its geographical
correlations. The limited space allowed to this article will require
that further consideration of the consequences be excluded, in order to
give due consideration to the causes.
One of the preparatory steps in the century’s advance was taken
by the German geographer, Ritter, who, near the beginning of the
century, advocated a new principle that may be illustrated by the
change in the definition of geography from “the description of the
earth and its inhabitants” to “the study of the earth in relation
to its inhabitants;” but advance beyond this beginning was for
a long time obstructed by certain ancient beliefs. Theological
preconceptions as to the age of the earth and the associated geological
doctrine of catastrophism, although attacked by the rising school of
uniformitarianism, were then dominant. They gave to the geographer
a ready-made earth, on which the existing processes of change were
unimportant. Furthermore, the belief in the separate creation of every
organic species led to the doctrine of teleology, which maintained the
predetermined fitness of the earth for its inhabitants, and of its
inhabitants for their lifework. All this had to be outgrown before
geographers could understand the slow development of land forms and the
progressive adaptation of all living beings to their environments. Yet
the beginning that Ritter made was of great importance, and it would
have led further had it not happened that for many decades professors
of geography in Europe brought chiefly a historical training to their
chairs, to the almost entire neglect of physical geography. In the
last thirty years there has been a reaction from this condition in
Germany and France, but Italy, with many professors of geography in her
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