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
By streak is meant the color of the mineral when powdered. For some
minerals, especially metallic ores, it is of great importance, for it
remains constant, though the color of the surface of the mineral changes
materially. It is most readily determined by rubbing a corner of the
mineral on a piece of unglazed porcelain. Small plates, known as “streak
plates” are made for this purpose.
Luster
The luster of a mineral is the appearance of its surface by reflected
light, and it is an important aid in determining many minerals. Two
types of luster are recognized; metallic, the luster of metals, most
sulphides and some oxides, all of which are opaque on their thin edges;
and non-metallic, the luster of minerals which are more or less
transparent on their thin edges, and most of which are light colored.
The common non-metallic lusters are; vitreous, the luster of glass;
resinous, the appearance of resin; greasy, oily appearance; pearly, the
appearance of mother-of-pearl; silky, like silk due to the fibrous
structure; adamantine, brilliant like a diamond; and dull, as is chalk.
Color
When used with caution color is of the utmost importance in determining
minerals, especially in making rapid determinations. In metallic
minerals it is constant and dependable; but in the non-metallic minerals
it may vary, due to the presence of small amounts of impurities which
act as pigments. Color depends on chemical composition, and when not
influenced by impurities is termed _natural_; but when the color is due
to some inclosed impurity it is termed _exotic_. In this latter case
caution must be used in making determinations. Many minerals are
primarily colorless, but take on exotic colors as a result of the
presence of small quantities of impurities; for instance, pure corundum
is colorless, but with a trace of iron oxide present becomes red, and is
called the ruby, or with a trace of cobalt becomes blue and is called
sapphire.
CHAPTER III
THE MINERALS
KEY TO THE MINERALS, BASED ON HARDNESS, COLOR, ETC.
OPAQUE COLORS
Color Hardness Streak Remarks Mineral
Public-domain text, read in full here on John Shaqi.
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