The chemistry, properties and tests of precious stonesMastin, John
Science
The chemistry, properties and tests of precious stones
Mastin, John
Precious stones
These are well-known examples of simple cleavage, in one definite
direction, though in many instances there are several forms and
directions of cleavage, but even in these there is generally one part or
line in and on which cleavage will take place much more readily than on
the others, these planes or lines also showing different properties and
angular characters, which, no matter how much fractured, always remain
the same. It is this "cleavage" which causes a crystal to reproduce
itself exactly, as explained in the last chapter, showing its parent
form, shape and characteristics with microscopic perfection, but more
and more in miniature as its size is reduced.
This may clearly be seen by taking a very small quantity of such a
substance as chlorate of potash. If a crystal of this is examined under
a magnifying glass till its crystalline form and structure are familiar,
and it is then placed in a test-tube and gently heated, cleavage will at
once be evident. With a little crackling, the chlorate splits itself
into many crystals along its chief lines of cleavage (called the
cleavage planes), every one of which crystals showing under the
microscope the identical form and characteristics of the larger crystal
from which it came.
The cleavage of minerals must, therefore, be considered as a part of
their crystalline structure, since this is caused by cleavage, so that
both cleavage and crystalline structure should be considered together.
Thus we see that given an unchangeable crystal with cleavage planes
evident, it is possible easily to reproduce the same form over and over
again by splitting, whereas by simply breaking, the form of the crystal
would be lost; just as a rhomb of Iceland spar might be sawn or broken
across the middle and its form lost, although this would really be more
apparent than real, since it would be an alteration in the mass and not
in the shape of each individual crystal. And given further cleavage, by
time or a sudden breaking down, even the mass, as mass, would eventually
become split into smaller but perfect rhombs.
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