The Story of the Earth and ManDawson, John William, Sir
Science
The Story of the Earth and Man
Dawson, John William, Sir
Human beings -- Origin; Paleontology
Taking England as an example, all before the Roman invasion is
pre-historic, and with regard to this pre-historic period the evidence
that we can obtain is chiefly of a geological character. The
pre-historic men are essentially fossils. We know of them merely what
can be learned from their bones and implements embedded in the soil or
in the earth of the caverns in which some of them sheltered
themselves. For the origin and date of these deposits the antiquary
must go to the geologist, and he imitates the geologist in arranging
his human fossils under such names as the "Paleolithic," or period of
rude stone implements; the "Neolithic" or period of polished stone
implements; the Bronze Period, and the Iron Period; though inasmuch as
higher and lower states of the arts seem always to have coexisted, and
the time involved is comparatively short, these periods are of far
less value then those of geology. In Britain the age of iron is in the
main historic. That of bronze goes back to the times of early
Phoenician trade with the south of England. That of stone, while
locally extending far into the succeeding ages, reaches back into an
unknown antiquity, and is, as we shall see in the sequel, probably
divided into two by a great physical change, though not in the abrupt
and arbitrary way sometimes assumed by those who base their
classification solely on the rude or polished character of stone
implements. We must not forget, however, that in Western Asia the ages
of bronze and iron may have begun two thousand years at least earlier
then in Britain, and that in some parts of America the Palaeolithic
age of chipped stone implements still continues. We must also bear in
mind that when the archæologist appeals to the geologist for aid, he
thereby leaves that kind of investigation in which dates are settled
by years, for that in which they are marked merely by successive
physical and organic changes.
Turning, then, to our familiar geological methods, and confining
ourselves mainly to the Northern Hemisphere and to Western Europe, two
pictures present themselves to us: (!) The physical changes preceding
the advent of man; (2) The decadence of the land animals of the
Post-pliocene age, and the appearance of those of the modern.
Public-domain text, read in full here on John Shaqi.
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