![Dolomite (Dolostone) (Dolomite [CaMg(CO3)2]) — sedimentary](https://media.rock.id/86dec618-d423-4146-a73e-99540d51f751-compressed.jpg)
sedimentary
Dolomite (Dolostone)
Dolomite [CaMg(CO3)2]
Hardness: 3.5-4; Color: Gray, tan, or buff; Luster: Pearly to sub-vitreous; Crystal structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral; Grainy texture.
- Hardness
- 3
- Color
- Gray, tan, or buff
- Luster
- Pearly to sub-vitreous
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Physical properties
Hardness: 3.5-4; Color: Gray, tan, or buff; Luster: Pearly to sub-vitreous; Crystal structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral; Grainy texture.
Formation & geological history
Formed by the chemical modification of magnesium-rich groundwater acting on lime mud and limestone (dolomitization). Common in the Paleozoic bedrock of the Upper Midwest/driftless area.
Uses & applications
Used as a source of magnesium, in the production of concrete and asphalt, for soil pH correction in agriculture, and as crushed stone for building foundations.
Geological facts
This specimen was found in the 'Driftless Area' of Iowa/Illinois/Wisconsin, a region famous for its unglaciated Paleozoic dolomite bluffs. Dolostone is often more resistant to weathering than limestone, leading to prominent cliff formations.
Field identification & locations
Identify by its reaction to cold dilute hydrochloric acid: it only fizzes when powdered or scratched, unlike limestone which fizzes immediately. Look for rhombohedral crystals in cavities within the rock.
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