Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
We see, for instance, the purest rock crystal affected by exposure
to the weather, its lustre tarnished, and the polish of its surface
impaired, but we know nothing of the power by which these operations
are performed. Thus also, in the precautions which the mineralogist
takes to preserve the fresh fracture of his specimens, we have a proof
how indiscriminately all the productions of the fossil kingdom are
exposed to the attacks of their unknown enemies, and we perceive how
difficult it is to delay the beginnings of a process which no power
whatever can finally counteract.
95. The mechanical forces employed in the disintegration of mineral
substances, are more easily marked than the chemical. Here again water
appears as the most active enemy of hard and solid bodies; and, in
every state, from transparent vapour to solid ice, from the smallest
rill to the greatest river, it attacks whatever has emerged above the
level of the sea, and labours incessantly to restore it to the deep.
The parts loosened and disengaged by the chemical agents, are carried
down by the rains, and, in their descent, rub and grind the superficies
of other bodies. Thus water, though incapable of acting on hard
substances by direct attrition, is the cause of their being so acted
on; and, when it descends in torrents, carrying with it sand, gravel,
and fragments of rock, it may be truly said to turn the forces of the
mineral kingdom against itself. Every separation which it makes is
necessarily permanent, and the parts once detached can never be united,
save at the bottom of the ocean.
96. But it would far exceed the limits of this sketch, to pursue
the causes of mineral decomposition through all their forms. It is
sufficient to remark, that the consequence of so many minute, but
indefatigable agents, all working together, and having _gravity_ in
their favour, is a system of universal decay and degradation, which
may be traced over the whole surface of the land, from the mountain
top to the sea shore. That we may perceive the full evidence of this
truth, one of the most important in the natural history of the globe,
we will begin our survey from the latter of these stations, and retire
gradually toward the former.
Public-domain text, read in full here on John Shaqi.
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