Serpentinite is a metamorphic rock, formed when igneous rocks are oxidised and hydrolysed by water. Serpentinite is a rock composed of one or more serpentine group minerals, the name originating from the similarity of the texture of the rock to that of the skin of a snake. Consists primarily of epidote, actinolite, chlorite, and plagioclase. Serpentine forms from the alteration of ultramafic igneous rocks under low grade metamorphic conditions in the presence of lots of water so any circumstances that provide these conditions will result in serpentinite. Serpentinite is a dense, dark green rock that can contain asbestos. This rock is created with slightly more water than serpentinite, making soapstone softer. It is a metamorphic magnesium rich rock because it is composed of the mineral talc. It consists of serpentine phyllosilicate minerals. Aside from these conditions there is no specific tectonic association associated with serpentinite. Includes rock mapped formerly as Hunting Hill Greenstone. Serpentinite metamorphic rock. Minerals in this group are formed by serpentinization, a hydration and metamorphic transformation of ultramafic rock from the Earth's mantle. Accessory chlorite, talc, and magnetite may be present. A rock composed of one or more serpentine group minerals, e.g., antigorite, chrysotile and lizardite, formed by serpentinization (hydration and metamorphic transformation) of rock consisting almost wholly of ferromagnesian silicate minerals, such as olivine and pyroxene (usually ultramafic igneous rocks). When clay- and aluminum-rich rock is altered by water from geothermal systems, serpentinite is liable to form. Soapstone, also known as steatite, is a rock that is also formed from peridotite. 8.9 Sheared serpentinite with pencil for scale, Marin County, California. Often found in low-grade metamorphic areas, serpentinite is composed of hydrated silicate minerals, particularly phyllosilicates. Serpentinite forms at the expense of olivine- and pyroxene-bearing rocks. Often, as here, serpentinite contains bands of the thin, fibrous, asbestos mineral chrysotile. Serpentine group minerals antigorite, lizardite, and chrysotile are produced by the hydrous alteration of ultramafic rocks. However, there are many kinds of metamorphic rocks, and some of them are more chemically reactive than others. The first is serpentinite. These rocks are composed of many distinct minerals. A hydration and metamorphic transformation of ultramafic rock from the Earth's mantle is called as serpentinization, a group of minerals is formed by serpentinization compose rock 'serpentinite'.. Rock-forming serpentine minerals form flat, cylindrical, and corrugated crystal microstructures, which reflect energetically efficient layering of alternate tetrahedral and octahedral sheets. Blackstone Group - greenstone, amphibolite, serpentinite - Dark-green, massive to foliated metamorphosed gabbroic and basaltic rock interlayered with epiclastic rock; local pillow-structures preserved. Serpentinite forms from the metamorphic alteration of ultramafic silicate rocks, particularly peridotite and pyroxenite, where serpentine minerals replace igneous minerals of olivine and pyroxene. Serpentinite is a metamorphic rock consisting almost entirely of "serpentine group minerals." The alteration is particularly important at the sea floor at tectonic plate boundaries. Template:Use dmy dates Serpentinite is a rock composed of one or more serpentine group minerals. Serpentinite is a metamorphosed ultramafic rock. Soapstone contains talc and chlorite, which can make the rock feel slippery. Serpentinite is a fibrous ± vein-type, nonfoliated, green-black metamorphic rock composed predominantly of serpentine minerals (see serpentine subgroup). 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2020 serpentinite metamorphic rock