Leisure hours among the gemsHamlin, Augustus C. (Augustus Choate)
Science
Leisure hours among the gems
Hamlin, Augustus C. (Augustus Choate)
Gems; Precious stones
Here, then, we may behold one of the strangest antitheses to be seen
in the whole mineral kingdom, for we have a simple and singular
mineral composed of the meanest of elements, yet whose different forms
illustrate the extremes of hardness, and may also be considered to
represent the antipodes of material treasures.
The crystallized and transparent variety, when it occurs in its
greatest perfection, and especially with the rare colors of red, blue,
and green, forms indeed the most beautiful of all the decorative stones
yet known to man. For it not only far exceeds all others in degree of
hardness, but it also surpasses them in its extraordinary brilliancy
and the wonderful display of the prismatic colors, especially by
artificial light, which charm it alone possesses of all the gems and
precious stones.
Although it is widely distributed over the world, and has been known
to man for many centuries, yet its distribution, its deposition, its
geological age, are not only puzzling themes to the mineralogist, but
they are yet subjects of startling interest to the philosopher.
The origin of the stone has long been a subject of inquiry among
experimentalists, and it has received more attention from them than
all the other gems reckoned together. As for our humble opinion, after
long consideration of this multitude of hypotheses, we are inclined
to assert the diamond to be the product of decomposition of vegetable
material, and derived from one of the numerous chemical compounds of
carbon and hydrogen. We find some of these forms generated wherever
vegetable matter is decomposed under water, and in the gem strata of
the diamond placers we may observe abundant evidence of material for
metamorphosis. If we admit the origin of the gem to be from vegetable
matter, or derived from any transformations of organic débris, we then
reduce the history of the diamond to a simple problem; for it is quite
easy to explain, or rather imagine, the required chemical change under
the action of electricity or telluric magnetism, and all along the true
gem formations the phenomena of the earth’s vitality in this respect
are remarkable.
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