an ultramafic composition
Pyroxene is a group of minerals.
Usually pyroxene crystallizes from magma before orthoclase. Pyroxene has a higher melting point than orthoclase, so it will crystallize first as the magma cools and reaches temperatures where pyroxene can form.
The first ferromagnesian mineral to crystallize is usually olivine, followed by pyroxene and amphibole. Among the feldspars, plagioclase feldspar is usually the first to crystallize, followed by potassium feldspar.
Peridotite is made only of olivine and pyroxene
shist
Basalt contains minerals such as plagioclase feldspar, pyroxene, and olivine. Gabbro also contains plagioclase feldspar and pyroxene, but generally has a coarser texture due to slower cooling rates underground.
an ultramafic composition
Ultramafic igneous rocks are comprised mostly of olivine and pyroxene. Examples include peridotite (pegmatic and porphyritic) and komatite.
Gneiss contains the minerals mica, quartz, feldspar, amphibole, garnet, and pyroxene.
A volcanic rock that fits your description is basalt. Basalt is dark-colored, fine-grained, and contains pyroxene minerals such as augite and pigeonite. It forms from the rapid cooling of lava on the Earth's surface.
The rock most likely belongs to the igneous category, such as a basalt that contains pyroxene, olivine, amphibole, and plagioclase feldspar.
Pyroxene is a group of minerals.
Scoria typically contains minerals such as olivine, plagioclase, pyroxene, and magnetite. Additionally, it may also have glassy material resulting from the rapid cooling of the magma during its formation.
No. Pyroxene is a crystalline silicate mineral.
Usually pyroxene crystallizes from magma before orthoclase. Pyroxene has a higher melting point than orthoclase, so it will crystallize first as the magma cools and reaches temperatures where pyroxene can form.
The first ferromagnesian mineral to crystallize is usually olivine, followed by pyroxene and amphibole. Among the feldspars, plagioclase feldspar is usually the first to crystallize, followed by potassium feldspar.