Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
Crystals are formed in liquids as they cool or evaporate and can no
longer hold the minerals in solution. Crystals start about a center or
nucleus, and molecule by molecule, the orderly arrangement is increased
and the crystal grows, there being no size which is characteristic. If
free in the liquid the crystal grows perfectly on all sides, but if
crystals are growing side by side, there comes a time when they
interfere with each other. Then the free faces continue to grow and the
orderly internal arrangement is maintained, though externally there is
interference.
Tetragonal system
In the second or tetragonal system one axis (the c axis) is different
from the other two, but all three are still at right angles with each
other. This is saying scientifically that the lines of force are greater
or less in one direction than in the other two, but they act at right
angles to each other. The a and the b axes are equal and anything that
happens to one of these two must happen to the other, but need not
happen to the c axis. Thinking of the molecules that arrange themselves
under this system of forces, it is clear that the simplest form will be
a square prism, _i.e._, front to back, and from side to side the numbers
of molecules will be equal, but up and down there will be a greater or
lesser number. If the eight corners of this prism were cut, and these
corner faces increased in size until they met, the resulting octahedron
would be longer (or shorter) from top to bottom than from side to side
or front to back, but the measurement from front to back would be equal
to the one from side to side. In this system we may have the vertical
edges of the prism beveled, and not have to bevel the horizontal ones,
or we may bevel the horizontal edges and not the vertical ones. There is
no dodecahedron in this system or in any other system than the
isometric. The forms in this tetrahedral system are really a combination
of the four sides of the square prism with such modifications as equally
affect them all, with two ends which may be flat, or pyramidal, or
modified pyramidal faces.
Orthorhombic system
Public-domain text, read in full here on John Shaqi.
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