Volcanoes: What They are and What They TeachJudd, John W. (John Wesley)
Science
Volcanoes: What They are and What They Teach
Judd, John W. (John Wesley)
Volcanoes
It is found convenient by geologists to designate those rocks which
have consolidated in deep-seated portions of the earth's crust
as Platonic Rocks, confining the name of Volcanic rocks to those
consolidating At the surface; but Plutonic and Volcanic Rocks shade
into one another by the most insensible gradations.
When the crystals embedded in granitic rocks, and in some lavas, are
examined with the higher powers of the microscope, they are frequently
seen to contain great numbers of excessively minute cavities. Each of
these cavities resembles a small spirit-level, having a quantity of
liquid and a bubble of gas within it. In fig. 7 we have given a series
of drawings of these cavities in crystals as seen under a high power
of the microscope. In No. 1 a group of such cavities is represented,
one of which is full of liquid, while two others are quite empty; the
remaining cavities all contain a liquid with a moving bubble of gas.
In No. 2 two larger cavities are shown, containing a liquid and a
bubble of gas; and it will be seen from these how varied in form these
cavities sometimes are. In Nos. 3, 4 and 6 the liquid in the cavities
contains, besides the bubbles, several, minute crystals; and in No. 6
we have a cavity containing two liquids and a bubble.
In the largest of such cavities the bubble is seen to change its
place so as always to lie at the upper side of the cavity, when the
position of the latter is altered, just as in a spirit-level. But in
the smallest cavities the bubbles appear to be endowed with a power of
spontaneous movement; like imprisoned creatures trying to escape, these
bubbles are seen continually oscillating from side to side and from end
to end of the cavities which enclose them. In fig. 8 a minute cavity
containing a liquid and bubble is shown, the path pursued by the latter
in its wonderful gyrations being indicated by the dark line. These
cavities are exceedingly minute, and so numerous that in some crystals
there must be millions of them present; indeed, in certain cases, as
we increase the magnifying power of our microscopes, new and smaller
cavities continually become visible. It has been estimated that in some
instances the number of these minute liquid-cavities in the crystals of
rocks amounts to from one thousand millions to ten thousand millions in
a cubic inch of space.
[Illustration: Fig. 8--Minute Liquid-cavity in a Crystal, with a moving
Bubble. (The path of the bubble is indicated by the dark line.)]
[Sidenote: NATURE OF LIQUIDS IN CAVITIES.]
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