Amphibolite is a metamorphic rock. It forms when basaltic rock is heated to high temperatures under pressure. Without the added pressure the basaltic rock that would be yielded is green schist.
the oceanic crust being subducted is Basaltic. It goes through changes from pressure and temperature as it ids subducted. It goes from basalt to Amphibolite and finally at 100km depth eclogite. At the 100 km a lot of the water is forced out of the rock allowing the surrounding area to liquidize. Since it is liquid it is less dense then the solid area and rises. as it reached into the Continental or ocean crust it melts the surrounding area, and magma rises forming a volcano.
The halogen found in seawater is bromine.
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Srimp are found in about every ocean.
The veroe is found in the beginning of the bible. It's the trademark.
Amphibolite is often used in construction. Amphibolite is commonly used on the faces of buildings, as well as paving.
Amphibolite can be found in regions with high-grade metamorphic rocks, typically in mountain belts or areas with tectonic activity. Examples include the Appalachian Mountains in the United States, the Scottish Highlands, the Alps in Europe, and some parts of Japan and New Zealand.
An amphibolite is a class of metamorphic rock comprised mainly of amphibole with some quartz and other minerals.
Is mineral amphibolite a felsic, mafic or intermidiate in term of color
Amphibolite is a type of metamorphosed mafic igneous rock. It is composed largely of minerals such as hornblende and plagioclase.
Amphibolite is the metamorphic form of amphibole, also known as hornblende. Amphibolite usually has a black and white, lightly foliated appearance.
Amphibolite is typically formed from the metamorphism of basalt or gabbro, which are both mafic igneous rocks. The high temperatures and pressures during metamorphism lead to the formation of amphibole minerals, giving rise to the rock type known as amphibolite.
Amphibolite is used as a decorative stone in landscaping and construction due to its attractive colors and patterns. It is also used as a raw material in the manufacture of certain types of building materials, such as countertops and flooring tiles. Additionally, amphibolite may be used in road construction and as a component of mineral collections.
Amphibolite typically has a medium to coarse-grained texture with a foliated structure. It consists mainly of amphibole minerals such as hornblende, which gives it a dark color and a shiny appearance.
Amphibole is a group of minerals which can have very different colors. However, most of the time, an amphibolite will be a dark color, like black or very dark green.
Basalt can metamorphose into a rock known as amphibolite. Amphibolite forms when basalt is subjected to high temperatures and pressure, leading to recrystallization of minerals and the development of a new texture.
The minerals in amphibolite are hornblende and plagioclase. Plagioclase are minerals that belong to the feldspar family. Other minerals in amphibolite are garnet, magnetite, quartz, and pyroxene.