The History of Creation, Vol. 1 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural CausesHaeckel, Ernst
Philosophy
The History of Creation, Vol. 1 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural Causes
Haeckel, Ernst
Evolution; Heredity; Human beings -- Origin
It is only by having regard to the great weight of Cuvier’s authority,
and to the mighty potency of human indolence, which is with difficulty
induced to depart from the broad and comfortable way of everyday
conceptions, and to enter upon new paths not yet made easy, that we can
comprehend how it is that Lamarck’s Theory of Descent did not gain its
due recognition until 1859, after Darwin had given it a new foundation.
The soil had long been prepared for it by the works of Charles Lyell,
another English naturalist, whose views are of great importance for the
natural history of creation, and must accordingly here be briefly
explained.
In 1830 Charles Lyell published, under the title of “Principles of
Geology,” a work in which he thoroughly reformed the science of Geology
and the history of the earth’s development, and effected this reform in
a manner similar to that in which, thirty years later, Darwin in his
work reformed the science of Biology. Lyell’s great treatise, which
radically destroyed Cuvier’s hypothesis of creation, appeared in the
same year in which Cuvier celebrated his triumph over the
nature-philosophy, and established his supremacy in the domain of
morphology for the following thirty years. Whilst Cuvier, by his
artificial hypothesis of creation and his theory of catastrophes
connected with it, directly obstructed the path of the theory of natural
development, and cut off all chance of a natural explanation, Lyell once
more opened a free road, and brought forward convincing geological
evidence to show that Cuvier’s dualistic conceptions were as unfounded
as they were superfluous. He demonstrated that those changes of the
earth’s surface, which are still taking place before our eyes, are
perfectly sufficient to explain everything we know of the development of
the earth’s crust in general, and that it is superfluous and useless to
seek for mysterious causes in inexplicable revolutions. He showed that
we need only have recourse to the hypothesis of exceedingly long periods
of time in order to explain the formation of the crust of the earth in
the simplest and most natural manner by means of the very same causes
which are still active. Many geologists had previously imagined that the
highest chains of mountains which rise on the surface of the earth could
owe their origin only to enormous revolutions transforming a great part
of the earth’s surface, especially to colossal volcanic eruptions. Such
chains of mountains as those of the Alps or the Cordilleras were
believed to have arisen direct from the fiery fluid of the interior of
the earth, through an enormous chasm in the broken crust. Lyell, on the
other hand, showed that we can explain the formation of such enormous
chains of mountains quite naturally by the same slow and imperceptible
risings and depressions of the earth’s surface which are still
continually taking place, and the causes of which are by no means
miraculous.
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