Serpentine is actually a general name applied to several members of a polymorphic group. It is believed the common green color is what inspired the name, serpentine, being a similar color and texture to that of a snake. Not a healthy idea, as you’ll soon learn. The source material of serpentinite, peridotite, is a rock made of upwelled magma containing large amounts of iron. Serpentine can range from translucent to opaque, and different opacities of stone can have slight variations in magical power. Ultramafic rock, rich in iron and magnesium, forms within the earth’s mantle and finds its way to the surface … Thus the vegetation on the so-called serpentine landscape is dramatically different from other plant communities, and serpentine barrens contain many specialized, endemic species. and rock are exposed to low temperatures (about 400 to 600 ºC) and metamorphic processes (high pressures) within the earth’s crust. The Greek physician Dioscorides suggested ground-up serpentinite as a prevention for snakebite. California has a greater number of minerals and a wider variety of rock types than does any other state. Serpentine is not just a gemstone, but rather, it is a group of minerals which includes up to 20 different related members. Serpentine is a major rock forming mineral and is found as a constituent in many metamorphic and weather igneous rocks. In other words the serpentine minerals are the major constitutes of the rock serpentinite . Get to know more about Serpentinite rock and characteristics of Serpentinite rock in the next sections. The streak of Serpentinite is white, greenish white or grey. This type of metamorphic rock is low in plant nutrients and high in toxic metals. Consists primarily of epidote, actinolite, chlorite, and plagioclase. All State Rocks. Serpentine is actually the name for this mineral group and Serpentinite is actually the name for the rock group regardless of the type of dominant serpentine mineral. It often colors many of these rocks to a green color and most rocks that have a green color probably have serpentine in some amount. Serpentine rock, so called because the pattern of the rock surface resembles a serpent’s skin, is actually a rock type originally formed from ultramafic rock. Minerals in this group are formed by serpentinization, a hydration and metamorphic transformation of ultramafic rock from the Earth's mantle. Serpentinite is a type of ultramafic rock, consisting predominantly of magnesium silicate and iron oxide minerals. Blackstone Group - greenstone, amphibolite, serpentinite - Dark-green, massive to foliated metamorphosed gabbroic and basaltic rock interlayered with epiclastic rock; local pillow-structures preserved. Most ultramafic rocks, including serpentinite, contain naturally occurring asbestos (NOA) particles The alteration is particularly important at the sea floor at tectonic plate boundaries. Includes rock mapped formerly as Hunting Hill Greenstone. Serpentine isn’t a single type of rock, but rather a suite of minerals, often called the serpentine subgroup. Its name is thought to be derived from its serpent-like green colors. As a general rule of thumb, a translucent stone will have a stronger effect on psychic phenomena, while a more opaque stone has a clearer effect on the measurable, material world, but the differentiation is rather minor. The streak of a rock is the color of powder produced when it is dragged across an unweathered surface. The word serpentine refers to the mottled, snakelike pattern sometimes seen on the rock. Serpentinite is available in black, brown, colourless, green, grey, white colors. Minerals in the serpentine subgroup are usually green or brown, but can also be black, yellow or white. California designated serpentine the official state rock in 1965 (California was the first state to designate a state rock). Template:Use dmy dates Serpentinite is a rock composed of one or more serpentine group minerals. Serpentine is a shiny green and blue rock found throughout California. Serpentine soil is an uncommon soil type produced by weathered ultramafic rock such as peridotite and its metamorphic derivatives such as serpentinite.More precisely, serpentine soil contains minerals of the serpentine subgroup, especially antigorite, lizardite, and chrysotile or white asbestos, all of which are commonly found in ultramafic rocks. Serpentine is a gem-quality hydrated magnesium silicate, usually green, yellowish-green, or brownish-green in color. Minerals and a wider variety of rock, consisting predominantly of magnesium silicate and iron minerals. 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