A magnesium iron silicate and the primary component of Earth's upper mantle, common in the subsurface but quick to weather at the surface. Its clear green gem variety is peridot, and it also serves industrial uses such as metalworking processes. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Formation ClassNesosilicate, crystallizing early and at high temperature from mafic and ultramafic magma; the dominant mineral of the Earth's upper mantle. 1 Chemical Formula Hardness (Mohs)Commonly cited range is 6.5 to 7.0 on the Mohs scale; 6.5 is used here. Classification
Crystal System Classification UseIndustrial and Abrasive 1 Connections
Associated With
Dunite is composed of at least 90 percent olivine by definition, the most olivine-rich common rock.
Komatiite is defined by its high magnesium content, expressed as abundant olivine, often in spinifex texture.
Olivine is the defining, essential mineral of peridotite.
Source Peridotite (Wikipedia)
Classified As
Crystallizes In System
In Discipline
Source Olivine (Wikipedia)
Sources
1. Olivine (Wikipedia)
Wikimedia FoundationLead section
The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickly on the surface.
Infobox: mohs
6.5-7.0
Lead section
The mineral olivine () is a magnesium iron silicate with the chemical formula (Mg,Fe)2SiO4.
Olivine (Wikipedia), body text
Minerals in the olivine group crystallize in the orthorhombic system
Olivine (Wikipedia), Applications section
The aluminium foundry industry uses olivine sand to cast objects
View the Source Wikidata: Olivine
Wikidata Q22693
Peridotite (Wikipedia)
Wikimedia FoundationAssociated With: Peridotite, Lead sectionQuote, Associated With: Peridotite, Lead section
Olivine is the essential mineral found in all peridotites.
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