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Ch. 1: Form of Minerals
Page
of 515
Text size:
FORM OF MINERALS.
47
without reference to the relative magnitude of the derived axes.
By multiplying the principal axis by any rational number
m,
greater or less than 1, a series of pyramids arise, whose general sign is mP, and their limits the prism and pinacoid, the whole series being contained in this formula,
which is
the fundamental series, the lateral axes always remaining unchanged. From each member a new series may, however, be developed in two directions by increasing one or other of the lateral axes. When the macrodiagonal is thus multiplied by any number
η
greater than 1, and planes drawn from the distance
η
to the polar edges, a new pyramid is produced, named a macropyra-mid, with the sign
the mark ov«r the Ρ pointing out the axis enlarged. Wher
a ma-
crodome results, with
the sign
If the shorter axis is multiplied, then bra-
chypyramids and brachydomes are produced with the signs
ì
So also from the prism
on the one
side, numerous macroprisms
with the limiting ma-
Page
of 515
Table Of Contents
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Feuchtwanger. Treatise on Precious Stones.
Contents & Preface
Ch. 1
: Introduction
Ch. 1
: Form of Minerals
Ch. 2
: Minerals: Phys. Prop.
Ch. 3
: Minerals: Chem. Prop.
Ch. 4
: Classification of Minerals
Ch. 5
: Gem Properties
: Diamond
: Sapphire
: Topaz
: Emerald
: Aquamarine
: Garnet
: Tourmaline
: Quartz
: Iolite
: Opal
: Amber
: Other Gems
: Illustrations, Index, Appendix
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