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Physical Properties of Star Blue Quartz Chemical Formula Chemical Classification Cleavage Color Crystal System Crystal Forms and Aggregates Fracture Luster Mohs Hardness Specific Gravity Streak Transparency Tenacity SiO2 Silicon Dioxide Indiscernible. Seldom exhibits parting. Colorless, white, purple, pink, brown, and black. Also gray, green, orange, yellow, blue, and red. Sometimes multicolored or banded. Hexagonal Crystals, which are hexagonal in shape, vary in shape and size. Quartz crystals are unique and very identifiable with their pointed and often uneven terminations. Crystals can be in enormous prismatic and stubby crystals, or in pointed aggregates of such crystals. Crystals are usually striated horizontally, and are sometimes doubly terminated. Quartz crystal habits include drusy, grainy, bladed, as linings of geodes, as rounded waterworn pebbles, radiating, as pointy pyramids on a matrix, as dense agglomerations of small crystals, massive, globular, stalactitic, crusty, in nodules, and in amygdules. Conchoidal Vitreous. Transparent, colorless Quartz crystals from a few distinct localities may be adamantine. 7 2.6—2.7 White Transparent to opaque Brittle April’s Mineral—Star Blue Quartz Alabama’s State Gemstone Quartz is an abundant mineral in Alabama rocks. Several varieties of quartz are valuable as gemstones, including the popular amethyst variety. Alabama's state gem is the Star Blue Quartz, (SiO2,) Silicon dioxide. It is one of the most beautiful gemstones on earth, and the cheapest because there are so many. There are also other states with quartz. With the approval of a bill proposed by Senator Don Hale, Cullman County, the star blue quartz was named the official gemstone for the State of Alabama by Act no. 90-203 in 1990. Most quartz is a souvenir of volcanoes, which melt silica, which is then carried by water into crevices, where it crystallizes. Such quartz often includes traces of other minerals picked up by water flowing underground. Crystalline form of silica SiO2, one of the most abundant minerals of the Earth's crust (12% by volume). Quartz occurs in many different kinds of rock, including sandstone and granite. It ranks 7 on the Mohs scale of hardness and is resistant to chemical or mechanical breakdown. Quartzes vary according to the size and purity of their crystals. Crystals of pure quartz are coarse, colourless, transparent, show no cleavage, and fracture unevenly; this form is usually called rock crystal. Impure colored varieties, often used as gemstones, include agate, citrine quartz, and amethyst. Quartz is also used as a general name for the cryptocrystalline and noncrystalline varieties of silica, such as chalcedony, chert, and opal. There is different colored quartz. New Hampshire has smokey, South Dakota rose, Arkansas and Georgia star blue. Quartz is made into glass, eyeglasses, electrical components, abrasives, and gemstone and building stone. Some forms of Quartz, especially the gemstone forms, have their color enhanced. There is a transparent sky blue form of Quartz crystals, as well as a wildly iridescent type that are synthetically colored by irradiation of gold. In some localities, Hematite forms a thin red or brown layer internally in the Quartz crystal, giving it a natural bright red to brown coloring, and sometimes even a mild natural iridescence.