BH250-87b

Title

BH250-87b

Subject

Komatiite

Description

Major Minerals: olivine, forsteritic olivine
Minor Minerals: plagioclase, chlorite, magnetite, iddingsite
Texture: spinifex, spinifex not as prominent as BH250-87, sheaves of olivine
Alteration: olivine to iddingsite, olivine to serpentine, olivine to magnetite

Komattite: Komatiite is an ultramafic volcanic rock rich in magnesium (MgO >18 wt.%) that formed from extremely hot, low-viscosity lava during the Archean Eon, over 2.5 billion years ago. With eruption temperatures exceeding 1600°C and magnesium contents reaching up to 30%, komatiites are dominated by olivine and typically occur in Archean greenstone belts. They are rare today due to the cooler modern mantle but provide valuable insights into early Earth’s thermal history. A hallmark feature of komatiites is spinifex texture, a distinctive bladed or skeletal growth pattern of olivine crystals that forms in the rapidly cooled upper margins of lava flows, resembling the spiky Australian Spinifex grass

Coverage

Australia, collected by John Goodge '80

Creator

Bereket Haileab
John Goodge '80

Source

From the rock collection of Bereket Haileab. Sample BH250-87b. Housed at Carleton College in Minnesota.

Contributor

Bereket Haileab
John Goodge '80

Type

Thin section and hand sample

Relation


View on ArcGIS Online here
















Collection

Citation

Bereket Haileab John Goodge '80, “BH250-87b,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/100.

Output Formats