Quartz occurs in a great number of varieties that differ in form and color. Quartz can occur as single crystals, crystals in druses, massive aggregates, and dense nodules. Quartz is colorless, if pure, but can assume any color because of inclusions of other minerals or because of the presence of built-in trace elements.
The more common varieties have been given their own names. The different varieties are commonly classified in two major groups:
One of these major groups is called macrocrystalline, which includes varieties that commonly form visible crystals. When people talk about quartz, they mostly think about macrocrystalline quartz. Some examples of macrocrystalline quartz are shown below:
Individual transparent crystals of euhedral quartz (= nice angular crystals), (largest crystal here is 2.3 cm height).
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A cluster of transparent crystals of quartz (largest crystal 6 cm height). To get crystals like these, they must have free space to grow into.
7 cm height |
4.5 cm height |
The above two images are of transparent macrocrystalline crystals of quartz containing inclusions of the mineral rutile, thereby forming "rutilated quartz." The acicular (needle-like) crystals of rutile, a titanium oxide, form within the structure of the quartz crystal. The "needles" can be golden, black, or other hues.
Citrine is the yellow to orange variety of quartz, with the colors being the result of the presence of iron impurities. This specimen is 8.3 cm height.
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Wonderful article! Lots of good info I needed! Thank you so much! Smoky Quartz
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