Beryl is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2(SiO3)6. Its well-known varieties include emerald and aquamarine. Naturally occurring hexagonal crystals can reach several meters in size, although terminated crystals are relatively rare. Pure beryl is colorless but is frequently tinted by impurities, with green, blue, yellow, pink and red (the rarest) all possible, and it is an ore source of beryllium. In this atlas it is the mineral species that gemstones such as emerald and aquamarine record.
Beryl is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2(SiO3)6. Its well-known varieties include emerald and aquamarine. Naturally occurring hexagonal crystals can reach several meters in size, although terminated crystals are relatively rare. Pure beryl is colorless but is frequently tinted by impurities, with green, blue, yellow, pink and red (the rarest) all possible, and it is an ore source of beryllium. In this atlas it is the mineral species that gemstones such as emerald and aquamarine record.
Facts
Chemical Formula Chemical Formula Hardness (Mohs)Commonly cited range is 7.5 to 8.0 on the Mohs scale; 7.75, the midpoint, is used here. Hardness (Mohs)Commonly cited range is 7.5 to 8.0 on the Mohs scale; 7.75, the midpoint, is used here. Classification
Strunz Class Strunz Class Crystal System Crystal System Connections
Caused By
Source Pegmatite (Wikipedia)
Crystallizes In System
In Discipline
In the Other Atlases
Mineral Species Of
Also in Divinity Atlas: of this mineral species.
Also in Divinity Atlas: of this mineral species.
Also in Divinity Atlas: of this mineral species.
Also in Divinity Atlas: of this mineral species.
Found In
Also in Geography Atlas: where this subject is found.
Source Geology.com: Beryl mineral and gemstoneArticle textQuote, Article text
Colombia, Zambia, Brazil , and Zimbabwe are major producers of gem-quality emerald
Also in Geography Atlas: where this subject is found.
Source Geology.com: Beryl mineral and gemstoneArticle textQuote, Article text
Colombia, Zambia, Brazil , and Zimbabwe are major producers of gem-quality emerald
Also in Geography Atlas: where this subject is found.
Source Geology.com: Beryl mineral and gemstoneArticle textQuote, Article text
A small amount of emerald is sporadically mined in the United States near Hiddenite, North Carolina
Also in Geography Atlas: where this subject is found.
Source Geology.com: Beryl mineral and gemstoneArticle textQuote, Article text
Colombia, Zambia, Brazil , and Zimbabwe are major producers of gem-quality emerald
Also in Geography Atlas: where this subject is found.
Source Geology.com: Beryl mineral and gemstoneArticle textQuote, Article text
Colombia, Zambia, Brazil , and Zimbabwe are major producers of gem-quality emerald
Sources
1. Beryl (Wikipedia)
Wikimedia FoundationBeryl, lead paragraph
is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2(SiO3)6
Beryl, article text
Well-known varieties of beryl include emerald and aquamarine.
View the Source 2. minerals.net: Beryl
minerals.netColor field
Light to emerald green, light to deep sky-blue, blue-green, yellow, pink, purple, red, orange, brown, colorless, white, and gray. May also be multicolored blue, green, yellow, or white, and may also have deeper color highlights on one crystal end.
Luster field
Vitreous, waxy
View the Source 3. Geology.com: Beryl mineral and gemstone
Geology.comDescriptionQuote, Description
Beryl is a relatively rare silicate mineral
View the Source Pegmatite (Wikipedia)
Wikimedia FoundationCaused By: Fractional Crystallization, PetrologyQuote, Caused By: Fractional Crystallization, Petrology
A typical sequence of deposition begins with microcline and quartz, with minor schorl and garnet. This is followed by deposition of albite, lepidolite, gem tourmaline, beryl, spodumene, amblygonite, topaz, apatite, and fluorite, which may partially replace some of the minerals in the earlier zone.
View the Source Beryl (Wikipedia)
Caused By: Hydrothermal Mineral Deposition, Deposits
Beryl is often associated with tin and tungsten ore bodies formed as high-temperature hydrothermal veins.
Caused By: Metasomatism, Deposits
Beryl is sometimes found in metasomatic contacts of igneous intrusions with gneiss, schist, or carbonate rocks.
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