Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
In speaking of continents and islands, it may be as well to remark at
the outset that all the land existing, or which probably has at any
time existed, consists of islands great or small. It is all surrounded
by the ocean. Two of the greater masses of land are, however,
sufficiently extensive to be regarded as continents, and from their
very extent and consequent permanence may be considered as the more
special homes of the living beings of the land. Two other portions of
land, Australia and the Antarctic polar continent, may be regarded
either as smaller continents or large islands, but partake of insular
rather than continental characters in their animals and plants. All the
other portions of land are properly islands; but while these islands,
and more especially those in mid-ocean, cannot be regarded as the
original homes of many forms of life, we shall find that they have a
special interest as the shelters and refuges of numerous very ancient
and now decaying species.
The two great continents of America and Eurasia have been the most
permanent portions of the land throughout geological time, some parts
of them having always been above water, probably from the Laurentian
age downward, though at various times they have been reduced to little
more than groups of islands. On them, and more especially in their
more northern parts, in which the long continuance of daylight in
summer seems in warm periods to have been peculiarly favourable to the
introduction of new vegetable and animal forms, and to the giving to
them that vigour necessary for active colonization, have originated the
greater number of the inhabitants of the land.
Public-domain text, read in full here on John Shaqi.
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