Peridotite is an ultramafic rock (less than 45% silica) and mainly contains the minerals olivene (a magnesium iron silicate - (Mg,Fe)2SiO4) and pyroxene (XY(Si,Al)2O6 where x may be calcium, sodium, iron or magnesium) and so as can be seen from the chemistry of the two primary minerals contains significant amounts of magnesium and iron.
Peridotite, believed to be the substance of the Earth's mantle is an igneous rock. It is mostly composed of olivine and pyroxene.
Peridotite is an intrusive igneous rock.
3.2-3.4 g/cm3
basalts
bumpy
The dominant rock type of the upper mantle is peridotite.
Peridotite is an intrusive ultramafic igneous rock.
peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. Peridotite can be found in the earth's mantle.
icelandic peridotite
A peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. Peridotite is ultramafic, as the rock contains less than 45% silica.
Peridotite is a dense, coarse-grained igneous rock.
The dominant rock type of the upper mantle is peridotite.
Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.
Peridotite.
Peridotite originates from the upper mantle.
Peridotite is an intrusive ultramafic igneous rock.
Peridotite is made only of olivine and pyroxene
A peridotite is a dense, coarse-grained igneous rock
peridotite
peridotite is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. Peridotite can be found in the earth's mantle.
icelandic peridotite
The parent rock of serpentine is called peridotite which is an ultramafic rock