The Mosaic History of the Creation of the World: Illustrated by Discoveries and Experiments Derived from the Present Enlightened State of Science; With Reflections, Intended to Promote Vital and Practical ReligionWood, Thomas
Religion
The Mosaic History of the Creation of the World: Illustrated by Discoveries and Experiments Derived from the Present Enlightened State of Science; With Reflections, Intended to Promote Vital and Practical Religion
Wood, Thomas
Bible and science; Cosmology; Creation; Religion and science
It is particularly deserving notice, that, after the creation of
caloric, the atmosphere was the next regular production. If heat
had not previously existed, could the atmosphere have been formed?
The Creator, having first impressed certain principles on matter,
impregnating it with repelling forces and systematical attractions,
proceeded with his work according to these radical and fixed laws.
One of the general laws discovered by Dr. Black, and which is laid
down as a chemical axiom, is, that “Whenever a body _changes_ its
state, it either combines with caloric, or separates from caloric.”
“The most probable opinion concerning the nature of caloric,” says Mr.
Dalton, “is that of its being an elastic fluid of great subtlety, whose
particles repel one another, but are attracted by all other bodies.
Every kind of matter has its peculiar affinity to heat, by which it
requires a certain portion of the fluid, in order to be in equilibrium
with other bodies at a certain temperature.”[55] It is now generally
supposed, adds Mr. Parkes, that the air owes its elasticity to the
caloric which it contains; and, that if it could be deprived entirely
of this, it would lose its elastic form. The expansibility of the air
is effected by the operation of caloric: for being rarefied by heat,
it occupies a larger space than otherwise it would. It is extremely
probable, says Lavoisier, that air is a fluid naturally existing in a
state of vapor; or, as we may better express it, that our atmosphere
is a compound of all the fluids which are susceptible of the vaporous
or permanently elastic state, in the usual temperature, and under the
common pressure.[56]
Public-domain text, read in full here on John Shaqi.
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