Vestiges of the Natural History of CreationChambers, Robert
Science
Vestiges of the Natural History of Creation
Chambers, Robert
Creation; Evolution (Biology)
The earth and all its various substances have at present a certain volume
in consequence of the temperature which actually exists. When, then, we
find that its matter and that of the associate planets was at one time
diffused throughout the whole space, now circumscribed by the orbit of
Uranus, we cannot doubt, after what we know of the power of heat, that
the nebulous form of matter was attended by the condition of a very high
temperature. The nebulous matter of space, previously to the formation
of stellar and planetary bodies, must have been a universal Fire Mist, an
idea which we can scarcely comprehend, though the reasons for arriving at
it seem irresistible. The formation of systems out of this matter
implies a change of some kind with regard to the condition of the heat.
Had this power continued to act with its full original repulsive energy,
the process of agglomeration by attraction could not have gone on. We do
not know enough of the laws of heat to enable us to surmise how the
necessary change in this respect was brought about, but we can trace some
of the steps and consequences of the process. Uranus would be formed at
the time when the heat of our system’s matter was at the greatest, Saturn
at the next, and so on. Now this tallies perfectly with the exceeding
diffuseness of the matter of those elder planets, Saturn being not more
dense or heavy than the substance cork. It may be that a sufficiency of
heat still remains in those planets to make up for their distance from
the sun, and the consequent smallness of the heat which they derive from
his rays. And it may equally be, since Mercury is twice the density of
the earth, that its matter exists under a degree of cold for which that
planet’s large enjoyment of the sun’s rays is no more than a
compensation. Thus there may be upon the whole a nearly equal experience
of heat amongst all these children of the sun. Where, meanwhile, is the
heat once diffused through the system over and above what remains in the
planets? May we not rationally presume it to have gone to constitute
that luminous envelope of the sun, in which his warmth-giving power is
now held to reside? It could not be destroyed—it cannot be supposed to
have gone off into space—it must have simply been reserved to constitute,
at the last, a means of sustaining the many operations of which the
planets were destined to be the theatre.
Public-domain text, read in full here on John Shaqi.
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