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
After this general glance at the monistic cosmogeny, or the
non-miraculous history of the development of the universe, let us now
return to a minute fraction of it, to our mother earth, which we left as
a ball flattened at both poles and in a fiery fluid state, its surface
having condensed by becoming cooled into a very thin firm crust. The
crust, on first cooling, must have covered the whole surface of the
terrestrial sphere as a continuous smooth and thin shell. But soon it
must have become uneven and hummocky; for, since during the continued
cooling, the fiery fluid nucleus became more and more condensed and
contracted, and consequently the diameter of the earth diminished, the
thin cold crust, which could not closely follow the softer nuclear mass,
must have fallen in, in many places. An empty space would have arisen
between the two, had not the pressure of the outer atmosphere forced
down the fragile crust towards the interior, breaking it in so doing.
Other unevennesses probably arose from the fact that, in different
parts, the cooled crust during the process of refrigeration contracted
also itself, and thus became fissured with cracks and rents. The fiery
fluid nucleus flowed up to the external surface through these cracks,
and again became cooled and stiff. Thus, even at an early period there
arose many elevations and depressions, which were the first foundations
of mountains and valleys.
After the temperature of the cooled terrestrial ball had fallen to a
certain degree, a very important new process was effected, namely, the
_first origin of water_. Water had until then existed only in the form
of steam in the atmosphere surrounding the globe. The water could
evidently not condense into a state of fluid drops until the temperature
of the atmosphere had considerably decreased. Now, then, there began a
further transformation of the earth’s crust by the force of water. It
continually fell in the form of rain, and in that form washed down the
elevations of the earth’s crust, filling the depressions with the mud
carried along, and, by depositing it in layers, it caused the extremely
important neptunic transformations of the earth’s crust, which have
continued since then uninterruptedly, and which in our next chapter we
shall examine a little more closely.
Public-domain text, read in full here on John Shaqi.
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