Scientific American Supplement No. 822, October 3, 1891Various
Science
Scientific American Supplement No. 822, October 3, 1891
Various
Science -- Periodicals
There can be but little doubt that this vein is a capital example of
hydrothermal fusion, whereby in original gneissic strata, at a
moderate temperature and considerable depth, through the action of
contained water, with the physical accompaniment of plication, a
solution of the country rock has been accomplished. And the cooling
and recrystallization has gone on so slowly that the elements of
granite have preserved a physical isolation, while the associated
silicates formed in the midst of this magma have attained a supremely
close and compact texture, owing to the favorable conditions of slow
growth giving them gem consistencies. The further development of the
vein may reveal interesting facts, and especially the following
downward of the rock mass, which we suspect will contract into a
narrower vein. At present the order of crystallization and separation
of the mineralogical units seems to have been feldspar, mica, garnet,
beryl, quartz.
In the artificial preparation of crystals it is invariably found that
perfect and symmetrical crystals, and crystals of large size, are
produced by slow, undisturbed cooling of solutions; the quiet
accretion permits complete molecular freedom and the crystal is built
up with precision. Nor is this all. In mixtures of chemical compounds
it is presumable that the separate factors will disengage themselves
from each other more and more completely, and form in purer masses as
the congelation is slowly carried on. A sort of concretionary affinity
comes into play, and the different chemical units congregate together.
At least such has been the case in the granitic magma of which Mr.
Wilson now possesses the solidified results. The feldspar, the quartz,
the mica, have approximately excluded each other, and appear side by
side in unmixed purity. And does it not seem probable that this
deliberate process of solidification has produced in the beryls, found
in the center of the vein at the points of slowest radiation, the
glassy gem texture which now makes them available for the purposes of
art and decoration?
* * * * *
THE STUDY OF MANKIND.
Public-domain text, read in full here on John Shaqi.
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