Intrusive igneous rock composed almost entirely 90% of plagioclase feldspar. Common on the Moon. Texture: Phaneritic. Rock type: Igneous Intrusive. Grain size: Very coarse. Minerals present: Plagioclase 90%, Pyroxene minor, Olivine minor. Formation: Forms from accumulation of plagioclase crystals floating in mafic magma chambers. Major component of lunar highlands. Common geological settings: Adirondacks New York , Labrador, Norway, lunar highlands; found in Proterozoic massifs. Common look-alikes and related entries: Gabbro, Marble, Diorite.
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GeoMiner
Last updated
2026-03-30T14:38:09.105519+00:00
Review status
Published; not independently peer-reviewed
Rocks — U.S. National Park Service. Authoritative overview of rock groups, the rock cycle, and geologic processes.
Intrusive igneous rock composed almost entirely 90% of plagioclase feldspar. Common on the Moon.
How can you identify Anorthosite?
Compare several properties rather than relying on colour alone. This entry records rock type: Igneous Intrusive; texture: Phaneritic; grain size: Very coarse; common minerals: Plagioclase 90%, Pyroxene minor, Olivine minor. Confirm an important identification with additional field tests or qualified laboratory work.
How does Anorthosite form?
Forms from accumulation of plagioclase crystals floating in mafic magma chambers. Major component of lunar highlands.
Where is Anorthosite commonly found?
Adirondacks New York , Labrador, Norway, lunar highlands; found in Proterozoic massifs.
What is Anorthosite commonly confused with?
Anorthosite may be confused with Gabbro, Marble, Diorite. Compare multiple diagnostic properties because colour and surface appearance can overlap.
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