File:Aquamarine in pegmatitic granite 1 (49052222392).jpg
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Summary
| Description |
(~6.0 centimeters across at its widest) Blue = aquamarine Glassy gray = quartz Light orangish-tan = potassium feldspar A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5500 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates. The silicates are the most abundant and chemically complex group of minerals. All silicates have silica as the basis for their chemistry. "Silica" refers to SiO2 chemistry. The fundamental molecular unit of silica is one small silicon atom surrounded by four large oxygen atoms in the shape of a triangular pyramid - this is the silica tetrahedron - SiO4. Each oxygen atom is shared by two silicon atoms, so only half of the four oxygens "belong" to each silicon. The resulting formula for silica is thus SiO2, not SiO4. The simplest & most abundant silicate mineral in the Earth's crust is quartz (SiO2). All other silicates have silica + impurities. Many silicates have a significant percentage of aluminum (the aluminosilicates). Beryl is a beryllium aluminosilicate mineral, Be3Al2(Si6O18). It has a nonmetallic luster, forms sharp, hexagonal crystals, is very hard (H=7.5 to 8), and can be any color. A frequently encountered color is pale bluish-green. Beryl has a glassy luster and no obvious cleavage Transparent beryls are gemstones. The gem name depends on the color: - deep green = emerald - bluish = aquamarine - pink = morganite - rich yellow = golden beryl - red = bixbite - yellowish-green to pale greenish = heliodor - clear/colorless = goshenite Seen here is a nice aquamarine crystal in pegmatitic granite. Pegmatites are very coarsely-crystalline, intrusive igneous rocks. They can form by very slow cooling, but most form by cooling of water-rich magma. Pegmatites can have concentrations of unusual minerals, such as beryl, tourmaline, and uraninite. Locality: unrecorded/undisclosed Photo gallery of beryl: <a href="https://www.mindat.org/gallery.php?min=819" rel="noreferrer nofollow">www.mindat.org/gallery.php?min=819</a> Photo gallery of aquamarine: <a href="https://www.mindat.org/gallery.php?min=289" rel="noreferrer nofollow">www.mindat.org/gallery.php?min=289</a> |
| Date | |
| Source | Aquamarine in pegmatitic granite 1 |
| Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/49052222392 (archive). It was reviewed on 12 November 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 04:17, 12 November 2019 | | 3,084 × 1,691 (3.2 MB) | Ser Amantio di Nicolao | Transferred from Flickr via #flickr2commons |
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