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
[Illustration: Tourmaline crystals, growing amid feldspar crystals
in a cavity in granite, from Paris, Me.]
Plate 5
[Illustration: Gold in quartz, from California]
Plate 6
[Illustration: Native silver in calcite]
[Illustration: Argentite, the black masses throughout the white
quartz]
Plate 7
[Illustration: Pyrargyrite as it appears after moderate exposure to
the light.]
[Illustration: Crystal form of Pyrargyrite]
[Illustration: Prousite as it appears after moderate exposure to the
light]
Plate 8
[Illustration: Native copper from Michigan]
[Illustration: Chalcopyrite in tetrahedrons and an occasional
octahedron.]
Plate 9
[Illustration: Chalcocite crystals with the bluish tarnish]
[Illustration: Tetrahedrite crystals]
Plate 11
[Illustration: Cuprite, the red crystals showing characteristic
color, other showing the green tarnish of malachite]
[Illustration: Malachite (green) and azurite (blue), the two
minerals shown together as they very commonly occur]
Plate 12
[Illustration: Limonite]
[Illustration: The crystal form in which goethite is found, _p_ is
the prism faces, _b_ and _c_ are faces formed by beveling the edges
of the prism, _o_ is the pyramidal face characteristic of the ends]
Plate 13
[Illustration: Hematite, Clinton iron ore, oolitic]
[Illustration: Siderite crystals]
Plate 15
[Illustration: Pyrite crystals]
[Illustration: Marcasite in concretionary form with radiate
structure]
Plate 17
[Illustration: Galena in crystals]
[Illustration: Pyromorphite crystals (green)]
Plate 19
[Illustration: Sphalerite, some the normal yellow and some crystals
with the reddish tinge. (White is dolomite)]
[Illustration: Zincite]
Plate 21
[Illustration: Smithsonite in yellow crystals]
[Illustration: Franklinite in octahedral crystals]
Plate 24
[Illustration: Arsenopyrite, showing crystals massed so as to be
incompletely developed]
[Illustration: Realgar as it usually occurs in powdery
incrustations]
Plate 25
[Illustration: Large crystal of stibnite, the light colored face is
the one parallel to which cleavage occurs]
[Illustration: Niccolite as a vein in slate]
Plate 26
[Illustration: Cobaltite, silver color, with pink tinge]
[Illustration: Smaltite, pink is cobalt bloom]
Plate 27
[Illustration: Carnotite from southwest Colorado]
[Illustration: Cinnabar]
Plate 31
[Illustration: Amethyst, not however deep enough colored for gems]
[Illustration: Jasper, with botryoidal surface]
Plate 32
[Illustration: Banded Agate from Brazil]
Plate 33
[Illustration: Common Opal from Arizona]
[Illustration: Siliceous sinter or Geyserite from The Yellowstone
Park]
Plate 35
[Illustration: A group of Microcline crystals from Pike’s Peak,
Colo.]
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