The historians' history of the world in twenty-five volumes, volume 01 : $b Prolegomena; Egypt, Mesopotamia
History
The historians' history of the world in twenty-five volumes, volume 01 : $b Prolegomena; Egypt, Mesopotamia
World history
Cuvier, the great contemporary of Laplace, no doubt accepted the
nebular hypothesis as a valid explanation of the origin of the world,
but he held to the conception of about six thousand years for the
age of man as rigidly as did any Middle Age monk. Cuvier was the
first to demonstrate that certain fossil skeletons belonged to no
existing species of animal. In other words, he believed that races of
great beasts had once inhabited the earth, but no longer have living
representatives. This, however, did not suggest to him that the earth
had long been peopled, but only went to show, as he believed, that
a great catastrophe, as the universal flood was supposed to have
been, had actually taken place. It remained for Charles Lyell, the
famous English geologist, working along the lines first suggested by
another great Englishman, James Hutton, to prove that the successive
populations of the earth, whose remains are found in fossil beds, had
lived for enormous periods of time, and had supplanted one another on
the earth, not through any sudden catastrophe, but by slow processes of
the natural development and decay of different kinds of beings.
Following the demonstrations of Lyell there came about a sudden change
of belief among geologists as to the age of the earth, until, in our
day, the period during which the earth has been inhabited by one kind
of creature and another is computed, not by specific thousands, but by
vague hundreds of thousands or even millions of years.
The last refuge for champions of the old chronology was found in the
claim that man himself had been but about six thousand years upon the
earth, whatever might be true of his non-human forerunners. But even
this claim had presently to be abandoned when the researches of the
palæontologists had been directed to the subject of fossil man.
The researches of Schmerling, of Boucher de Perth, of Lyell himself,
and of a host of later workers demonstrated that fossil remains of man
were found commingled in embedded strata and in cave bottoms under
conditions that demonstrated their extreme antiquity; and in the course
of the quarter century after 1865, in which year Lyell had published
his epoch-marking work on the antiquity of man, the new idea had made
a complete conquest, until now no one any more thinks of disputing
the extreme antiquity of man than he thinks of questioning the great
age of the earth itself. To be sure, no one pretends any longer to
put a precise date upon man’s first appearance. The new figures take
on something of the vagueness that characterise the estimates of the
Babylonians; but it is accepted as clearly proven that the racial
age of man is at least to be numbered in tens of thousands of years.
The only clues at present accessible that tend to give anything like
definiteness to the computations are the researches of Egyptologists
and Assyriologists.
Public-domain text, read in full here on John Shaqi.
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