Plutonic igneous rock containing olivine and two pyroxenes, with little or no feldspar
Coarse grained ultramafic igneous rock composed mainly of olivine and pyroxene The mantle is though to be composed primarily of this rock type
Coarse-grained, heavy, igneous rock that contains at least 10% olivine, other iron-and magnesium-rich minerals (generally pyroxenes), and not more than 10% feldspar. Peridotite is the ultimate source of all chromium ore and naturally occurring diamonds, and of nearly all chrysotile asbestos. Nearly all peridotite is more or less altered to serpentine; in warm, humid climates peridotite and serpentine have weathered to soils and related deposits that, though now worked on a relatively small scale, are potential sources of iron, nickel, cobalt, and chromium
A coarsely crystalline, silica poor, igneous rock consisting predominantly of the mineral olivine the Earth's mantle is probably composed largely of peridotite
a rock consisting of small crystals of olivine, pyroxene and hornblende; the major constituent of the Earths mantle