The water-courses of these various great tracts of land are all
determined by the formation of the surface, but the amount of water
which is carried into the oceans by the rivers of any district is
always in proportion to the amount of vegetation in that district; thus
in Europe, Asia, and America, the number and extent of these correspond
with the great fertility of the soil, while the northern and western
part of Africa--the Great Desert--give off scarcely any of adequate
extent, the Nile appearing to receive its supply from the central parts
further south. The reason of it is this: wherever there is vegetation,
either in the form of grassy prairies or forests, there is also a great
reduction of temperature from the radiation and evaporation, and the
consequent formation of rain, dew, or snow, which falling on the ground
produces streams, &c.
Excepting the great tracts of land named, and islands too numerous to
be mentioned, the whole surface of the earth is covered with water,
the great divisions of which (called Oceans) are, the Arctic Ocean, to
the north of Europe, the Atlantic, between America, Europe, and Africa,
the Pacific between Asia and America, and the Indian Ocean between
Africa and Australia.
The foregoing is a very bare outline of the land and water covering the
surface; it may suffice, however, to call to mind the main features
of the earth as it is now disposed. There can be little doubt that
the great variety of climate, whether hot or cold, moist or dry, is
one of the greatest sources of happiness that can be well imagined;
it stimulates to research, travel, and inquiry into the works of God;
every change experienced tends to make man search for further change,
every new scene makes him compare it with others; and the acquirement
of a knowledge of places, and a general idea of the whole world,
expands his mind enables him to appreciate the good gifts he has
received, and affords a source of satisfaction beyond almost any other
kind of enjoyment.
THE WATERS.
[Illustration: SEA-COAST.]
Public-domain text, read in full here on John Shaqi.
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