Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
=The essential nature of crystals.=—A crystal we are accustomed to
think of as something transparent bounded by sharp edges and angles,
our ideas having been obtained largely from the gem minerals. This
outward symmetry of form is, however, but an expression of a power
which resides, so to speak, in the heart or soul of the crystal
individual—it has its own structural make-up, its individuality. No
more correct estimates of the comparison of crystal individualities
would be obtained by the study of outward forms alone of two minerals
than would be gained by a judgment of persons from the cut of their
clothing. Too often this outward dress tells only of the conditions by
which both men and crystals have been surrounded, and but little of the
power inherent in the individual. Many a battered mineral fragment with
little beauty to recommend it, when placed under suitable conditions
for its development, has grown into a marvel of beauty. Few minerals
are so mean that they have not within them this inherent power of
individuality which lifts them above the world of the amorphous and
shapeless.
[Illustration:
FIG. 10.—Comparison of a crystalline with an amorphous substance when
expanded by heat and when attacked by acid.]
Just as the real nature of a person is first disclosed by his behavior
under trying circumstances, so of a crystal it is its conduct under
stress of one sort or another which brings out its real character. By
way of illustration let us prepare a sphere from the mineral quartz—it
matters not whether we destroy the beautiful outlines of the crystal or
employ a battered fragment—and then prepare a sphere of similar size
and shape from a noncrystalline or amorphous substance like glass. If
now these two spheres be introduced into a bath of oil and raised to a
higher temperature, the glass globe undergoes an enlargement without
change of its form; but the crystal ball reveals its individuality
by expanding into a spheroid in which each new dimension is nicely
adjusted to this more complex figure (Fig. 10).
Public-domain text, read in full here on John Shaqi.
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