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Name: |
Quartz |
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Chem: |
SiO2 - | |||||
Crystal: |
Hexagonal (excellent hexagonal prisms with termination, also massive, and crypto-crystalline varieties) | |||||
Color: |
purple pink |
yellow - orange |
clear |
gray-brown |
crypto- | |
Refrac. Index: |
1.54 - 1.55 |
Birefraction: |
0.009 | |||
Hardness: |
7.0 |
Spec. Grav.: |
2.65 | |||
Fracture: |
conchoidal |
Cleavage: |
none | |||
Environment: |
a rock forming mineral, contact metamorphics, hydrothermal, mesothermal, and epithermal veins | |||||
Association: |
feldspars, pyrite, tourmaline, rutile | |||||
Locals: |
| Largest crystals, Brazil | found virtually everywhere | Ark., USA | | |||||
Misc: |
The name is derived from the German "quarz" of Slavic origin. It was called "krystallos" by the Greeks, but this later became the generic term for crystal. It is used as an oscillator in time pieces and in radio, and was mined extensively in brazil during W.W.II. The material has now been synthesized in the laboratory and is much purer and better for electronic use. | |||||
Gem info: |
Quartz is the most abundant mineral on earth and is
present in many rock types. It is classified by both color
and physical makeup. First there are two physical types: Crystalline: meaning large single crystals of aggregates of individual crystals. Having the hexagonal shape or habitat of the mineral. (Rose quartz is a minor exception as it rarely forms good crystals.)
Cryptocrystalline: masses made up of either
fibrous or granular aggregates of quartz. Both are tough and
compact, and take a good polish when cabbed.
Jasper, Flint, and Chert are names used to describe some of the varieties of granular quartz.
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smoky
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quartz points w/
rutile(closeup) |
agate
banded |
Aventurine |