Mineral
Calcite
Carbonate Minerals
Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate, CaCO3; the other polymorphs are aragonite and vaterite. It is a very common mineral, a major constituent of limestone, the primary mineral in metamorphic marble, and often the main constituent of the shells of marine organisms. Calcite defines hardness 3 on the Mohs scale and has a vitreous luster in crystals. It is white or colorless unless impurities tint it gray, red, orange, yellow, green, blue, violet, brown or black. It fizzes in acid, and groundwater can dissolve or precipitate it, which is how stalactites and stalagmites form in caves. A transparent variety called Iceland spar shows strong birefringence, so objects seen through it appear doubled, and large calcite crystals are used in optical equipment.
Facts
Formation Class Chemical FormulaCaCO3, calcium carbonate 1 Hardness (Mohs)Calcite is the reference mineral that defines the value of 3 on the Mohs scale itself. Classification
Strunz ClassCarbonates and Nitrates 1 Crystal SystemTrigonal (Rhombohedral) 2 UseSculpture and Ornamental 3 Wikipedia 'Calcite' states this use (or use-bearing statement); earth5 pass. Connections
Associated With
Calcite named as one of the most common marine evaporite minerals; cited via evaporite's own registered source since Calcite carries only the generic mineral-wikipedia stub as its own source.
Source Evaporite (Wikipedia)
Skarn typically forms from a carbonate (limestone or marble) protolith, and calcite persists in many skarns.
Caused By
Source Calcite (Wikipedia)
Source Calcite (Wikipedia)
Source Calcite (Wikipedia)
Source EBSCO Research Starters: Hydrothermal solutions and mineralization
Source Calcite (Wikipedia)
Source Calcite (Wikipedia)
Classified As
Crystallizes In System
In Discipline
Source Mineral (Wikipedia)
In the Other Atlases
Mineral Species Of
Also in Divinity Atlas: of this mineral species.
Also in Divinity Atlas: of this mineral species.
Sources
1. Mineral (Wikipedia)
Wikimedia FoundationLead sectionQuote, Lead section
The reaction of acid with carbonates, most commonly found as the polymorph calcite and aragonite (CaCO3), relates to the dissolution and precipitation of the mineral, which is a key in the formation of limestone caves, features within them such as stalactite and stalagmites, and karst landforms.
View the Source 2. Calcite (Wikipedia)
Lead section
Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on scratch hardness comparison.
Infobox: system
Trigonal
Caused By: Sedimentation, Natural occurrence
Calcite is a common constituent of sedimentary rocks, limestone in particular, much of which is formed from the shells of dead marine organisms.
Caused By: Biomineralization, Natural occurrence
Calcite is often the primary constituent of the shells of marine organisms, such as plankton (such as coccoliths and planktic foraminifera), the hard parts of red algae, some sponges, brachiopods, echinoderms, some serpulids, most bryozoa, and parts of the shells of some bivalves (such as oysters and rudists).
Caused By: Diagenesis, Natural occurrence
Bedding parallel veins of fibrous calcite, often referred to in quarrying parlance as beef, occur in dark organic rich mudstones and shales, these veins are formed by increasing fluid pressure during diagenesis.
Caused By: Metamorphism, Natural occurrence
It is the primary mineral in metamorphic marble.
Caused By: Hydrothermal Circulation, Natural occurrence
It also occurs in deposits from hot springs as a vein mineral; in caverns as stalactites and stalagmites; and in volcanic or mantle-derived rocks such as carbonatites, kimberlites, or rarely in peridotites.
View the Source3. Wikidata: Calcite
Wikidata Q171917
4. minerals.net: Calcite
minerals.netColor field
Colorless, white, yellow, brown, orange, pink, red, purple, blue, green, gray, black. May also be multicolored or banded.
Luster field
Vitreous
Description
Calcite is the one of the most common minerals.
View the Source Evaporite (Wikipedia)
Wikimedia FoundationAssociated With: Evaporite, Marine evaporite minerals sectionQuote, Associated With: Evaporite, Marine evaporite minerals section
The most common marine evaporites are calcite, gypsum and anhydrite, halite, sylvite, carnallite, langbeinite, polyhalite, and kainite.
View the Source EBSCO Research Starters: Hydrothermal solutions and mineralization
EBSCO Research StartersCaused By: Hydrothermal Mineral Deposition, Hydrothermal deposit types and gangue mineralsQuote, Caused By: Hydrothermal Mineral Deposition, Hydrothermal deposit types and gangue minerals
Calcite, fluorite, and barite are also common as gangue minerals.
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