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within a zone we identify as the crystalline zone. Many of the crystals in this zone are smoky and have mica, rutile, and tourmaline inclusions. An interesting characteristic of many of the crystals in this zone is a tessin habit. This means these crystals grew in higher temperatures around 500º C or 932º F. The tessin habit is one in which the crystal has a wide base that narrows up along the axis to a small point at the termination forming a wedge shape. |
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everywhere. It was very peculiar, however, that we would still find pristine crystals within the alluvium. My guess is that the area is one big ancient mud slide where rounded quartz that were exposed to weathering on the surface were mixed in with the pristine ones that were gouged out of in situ dikes by the alluvium. |
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and chipped surface, indicate that it has been in water where it has collided with other rocks to produce the damage. |
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it only has a slight grey smoky color. This is an example of one of the pristine crystals that can be found within the alluvium. |
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of a dike has become crystallized and is usually covered with m faces and sometimes terminations. |
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