By John Von Neumann
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Additional resources for Collected works. Vol.6 Theory of games, astrophysics, hydrodynamics and meteorology
Amazonite is a rare blue-green variety of an alkali feldspar called microcline Alkali Feldspars (Fig. 8; L = vitreous. An iridescent play of colors may be seen in some plagioclases, especially labradorite. Parallel, regular striations on a cleavage plane (= twinning) are common in the plagioclase series. Albite (Na-rich) and anorthite (Ca-rich) are the end members Plagioclase Feldspars (Fig. 3; L = vitreous (slightly duller than hornblende); Habit = stubby Augite (pyroxene) (Fig. 8c) Single-chain silicate H = 5–6; CL = 2 at approx.
7). You see a double image when looking through the crystal. If you rotate the crystal, one image will stay fixed and the other will move around it. Smell Some minerals, such as sulfur, possess a distinctive odor. Taste A few minerals have a characteristic taste. Halite tastes salty. Sylvite tastes bitter. Taste is a valid mineral property and can be quite helpful in identifying some minerals. When you work on mineral identification next, be sure to look for special properties. Special Properties Some minerals have special properties, such as effervescence in acid, magnetism, unusual visual properties, or a distinctive smell, taste, or feel.
Cleavage and Fracture Fracture If the broken surfaces of a mineral are irregular and nonplanar, the mineral is said to have fracture. 6). Fibrous: Fracture surface has the appearance of many fine threads lying parallel to each other. 9b right, on p. 28). Hackly: A sharp, irregular surface, the same as jagged. 8b on p. 1, p. 98) may produce a hackly fracture. Uneven/Irregular: General terms that can be applied to the fracture of many different minerals that otherwise defy definition. Parting: Generally not a common characteristic, parting is a roughly planar break in a mineral that is not as well developed as cleavage.
Collected works. Vol.6 Theory of games, astrophysics, hydrodynamics and meteorology by John Von Neumann