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Evaporite

Sedimentary Rocks

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An evaporite is a water-soluble sedimentary mineral deposit caused by the concentration and crystallization that results when enough of the water solvent evaporates from an aqueous solution. Evaporites are formed by chemical sediments, crystallizing out as dissolved salts left behind as water evaporates.

Facts
Kind
Rock 1
Formation Class
Sedimentary, chemical (a water-soluble mineral deposit formed by crystallization as water evaporates from solution) 1
Cross-Tradition Connections

Associated With

Calcite, Materials

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.

Gypsum, Materials

Gypsum named as one of the most common marine evaporite minerals.

Halite, Materials

Halite named as one of the most common marine evaporite minerals.

In Discipline

Geology, Disciplines
Sources
1. Evaporite (Wikipedia)
Wikimedia FoundationLead section
Quote, Lead section
formed by chemical sediments.
View the Source
1. Evaporite (Wikipedia)
Wikimedia FoundationAssociated With: Halite, Marine evaporite minerals section
Quote, Associated With: Halite, Marine evaporite minerals section
The most common marine evaporites are calcite, gypsum and anhydrite, halite, sylvite, carnallite, langbeinite, polyhalite, and kainite.
View the Source
1. Evaporite (Wikipedia)
Wikimedia FoundationAssociated With: Gypsum, Marine evaporite minerals section
Quote, Associated With: Gypsum, Marine evaporite minerals section
The most common marine evaporites are calcite, gypsum and anhydrite, halite, sylvite, carnallite, langbeinite, polyhalite, and kainite.
View the Source
1. Evaporite (Wikipedia)
Wikimedia FoundationAssociated With: Calcite, Marine evaporite minerals section
Quote, Associated With: Calcite, Marine evaporite minerals section
The most common marine evaporites are calcite, gypsum and anhydrite, halite, sylvite, carnallite, langbeinite, polyhalite, and kainite.
View the Source
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