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: A piece of gypsum looking on the surface of the
perfect cleavage, and showing the two other cleavages as lines,
intersecting at 66°. Twinning is also shown]
[Illustration: A simple crystal of gypsum]
[Illustration: Twin crystals of gypsum]
Plate 51
[Illustration: Sulphur crystals]
[Illustration: Ice crystals, the top one, the end of a hexagonal
prism; the two lower figures multiple twins as in snow flakes]
Plate 52
[Illustration: The Devil’s Tower, Wyoming, an example of igneous
rock with columnar structure, and resting on sedimentary rocks.
Courtesy of the U. S. Geological Survey]
Plate 53
[Illustration: A coarse granite]
[Illustration: Graphic granite]
Plate 54
[Illustration: Syenite]
[Illustration: Gabbro]
Plate 55
[Illustration: Basalt-porphyry. The large white crystals are
phenocrysts of plagioclase feldspar]
[Illustration: Basalt-obsidian]
Plate 56
[Illustration: Amgydoloid]
Plate 57
[Illustration: The north face of Scott’s Bluff, Neb., showing
sedimentary sandstones above and clays below. The type of erosion is
characteristic of arid regions. Courtesy of the U. S. Geological
Survey]
Plate 58
[Illustration: Breccia]
[Illustration: Conglomerate]
Plate 59
[Illustration: Calcareous shale]
[Illustration: Coquina]
Plate 60
[Illustration: Foramenifera from Chalk; enlarged about 25 diameters]
[Illustration: Encrinal Limestone; fragments of the stems, arms and
body of Crinoids]
Plate 62
[Illustration: _A_ diatomaceous earth magnified 50 times]
[Illustration: _B_ and _C_ two diatoms from the above enlarged 250
times. After Gravelle, by the courtesy of Natural History]
Plate 63
[Illustration: A metamorphic rock, showing the contortion of layers
due to expansion under heat]
Plate 64
[Illustration: A conglomerate partly metamorphosed to a gneiss. Note
the flattened pebbles and the alternation of the intermediate
material to mica scales, etc.]
[Illustration: A typical gneiss]
Plate 66
[Illustration: Phyllite]
[Illustration: A white marble, with black streaks due to graphite]
Plate 68
[Illustration: Claystones, simple and compound]
[Illustration: A line concretion, which on splitting disclosed a
fern leaf of the age of the coal measures]
Plate 69
[Illustration: A septeria from Seneca Lake, N. Y.]
[Illustration: Pisolite]
Plate 70
[Illustration: A geode filled with quartz crystals]
Plate 71
[Illustration: A quartz pebble from the bed of a New England brook]
[Illustration: A pebble of schist and granite from the foot of Mt.
Toby, Mass.]
Plate 72
[Illustration: An iron-nickel meteorite, of 23 lbs. which fell in
Claiborne Co., Tenn.]
[Illustration: An etched slice of an iron meteorite which fell in
Reed City, Osceola Co., Mich.]
Plate 73
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