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Dolomite

Image: <bdi><a href="https://www.wikidata.org/wiki/Q56247090" class="extiw" title="d:Q56247090"><span title="mineral collector and dealer">Robert M. Lavinsky</span></a></bdi> (CC BY-SA 3.0)

trigonalcommonCarbonates

Dolomite

CaMg(CO3)2

The image displays a cluster of well-formed, translucent, pinkish-white rhombohedral dolomite crystals, characteristic of the mineral's trigonal crystal system.

Dolomite Physical Properties

Mohs Hardness

3.5

Crystal System

trigonal

Luster

vitreous

Streak Color

white

Cleavage

perfect rhombohedral on {1011}

Fracture

conchoidal

Specific Gravity

2.85

Colors

white, pink, gray, brown, colorless

Transparency

translucent

Type Locality

Tsumeb Mine, Tsumeb, Otjikoto Region, Namibia

Mineral Group

Carbonates

Uses

construction material, magnesium source, soil conditioner, flux in metallurgy, ornamental stone

Associated Minerals

calcite, quartz, pyrite, sphalerite, galena

Rarity

common

Geological Context

Dolomite forms in sedimentary environments, often as a secondary alteration product of limestone (dolomitization) or through direct precipitation in hypersaline conditions, and can also be found in hydrothermal veins.