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Ch. 4: Cleavage of Gemstones

Ch. 4: Cleavage of Gemstones Page of 118 Ch. 4: Cleavage of Gemstones Text size:minus plus Restore normal size   Mail page  Print this page
24                             PRECIOUS STONES
instance : very often, in a certain cavity, fluorspar has existed originally, but, through some chemical means, has been slowly changed to quartz, so that, as crystals cannot be changed in shape, we find quartz existing—undeniably quartz—yet possessing the crystals of fluorspar ; therefore the quartz becomes a pseudomorph, the condition being an example of what is termed pseudomorphism. The actual cause of this curious chemical change or substitution is not known with certainty, but it is interesting to note the conditions in which such changes do occur.
It is found that in some cases, the matrix of a certain shaped crystal may, after the crystal is dissolved or taken away, become filled by some other and foreign substance, perhaps in liquid form; or a crystalline substance may become coated or " invested" by another foreign sub­stance, which thus takes its shape ; or actual chemical change takes place by means of an incoming substance which slowly alters the original substance, so that eventu­ally each is false and both become pseudomorphs. This curious change often takes place with precious stones, as well as with other minerals, and to such an extent that it sometimes becomes difficult to say what the stone ought really to be called.
Pseudomorphs are, however, comparatively easy of isolation and detection, being more or less rounded in their crystalline form, instead of having sharp, well-defined angles and edges; their surfaces also are not good. These stones are of little value, except in the specially curious examples, when they become rare more by reason of their curiosity than by their utility as gems.
Some also show cleavage planes of two or more
Ch. 4: Cleavage of Gemstones Page of 118 Ch. 4: Cleavage of Gemstones
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