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Amphibolite is a metamorphic rock consisting of amphibole. It is formed within the pressure-temperature limits of amphibolite facies usually anywhere from 400 to 500 degrees Celsius.

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โˆ™ 2014-08-21 09:36:47
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Q: How is amphibolite formed?
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What do you do with amphibolite?

Amphibolite is often used in construction. Amphibolite is commonly used on the faces of buildings, as well as paving.


What is amphibolite used for?

Amphibolite is used for constructions and attractive decorations


What is the color of amphibolite?

Amphibolite is the metamorphic form of amphibole, also known as hornblende. Amphibolite usually has a black and white, lightly foliated appearance.


What is the texture of amphibolite?

Amphibolite has a schistose texture, medium to coarse grained and platy.


What minerals are in amphibolite?

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.


What is the parent rock of amphibolite?

Amphibolite can have a number of protoliths including various sedimentary and igneous rocks.


Is amphibolite mineral a felsic mafic or intermidate?

Is mineral amphibolite a felsic, mafic or intermidiate in term of color


What is an amphibolite?

An amphibolite is a class of metamorphic rock comprised mainly of amphibole with some quartz and other minerals.


What is the hardness of amphibolite?

it is 7.9


What is the luster of amphibolite?

earthy


Is amphibolite foliated?

It can be both


What is amphibolite made of?

Amphibolite is a type of metamorphosed mafic igneous rock. It is composed largely of minerals such as hornblende and plagioclase.


Where can amphibolite be found?

in the andes mountains


What type of rock is amphibolite?

Amphibolite is the name given to a rock consisting mainly of hornblende amphibole, the use of the term being restricted, however, to metamorphic rocks.


How does metamorphism affect basalt?

it changes it in to amphibolite and schist


What rock does basalt become after metamorphosis?

amphibolite is 1 of them


What is the color of a amphibolite rock?

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.


Where is amphibolite found?

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.


What does basalt develop into?

When basalt metamorphoses (changes through heat and/or pressure), it becomes amphibolite. Amphibolite is dark-coloured, and resembles dark, glassy crystals fused together. It is heavy, with a slightly flaked structure.


What is metamorphic rocks's names?

quartzite, slate, gneiss, marlbe, migmitite, amphibolite, serpenrinite, eclogite. that's all i have from my school papers. quartzite, slate, gneiss, marlbe, migmitite, amphibolite, serpenrinite, eclogite. that's all i have from my school papers.


10 examples of metamorphic rocks?

Slate, gneiss, skarn, phyllite, amphibolite, schist, quartzite, marble, and granulite are all metamorphic rocks.


3 metamorphic rocks?

Slate, gneiss, skarn, phyllite, hornfels, amphibolite, schist, quartzite, marble, and granulite are all metamorphic rocks.


Examples of metamorphic rock?

Slate, gneiss, skarn, phyllite, amphibolite, schist, quartzite, marble, and granulite are all metamorphic rocks.


What are 12 examples of metamorphic rock?

- Amphibolite - Eclogite - Gneiss - Greenstone - Hornfels - Marble - Migmatite - Phyllite - Quartzite (Metaquartzite) - Schist - Slate - Soapstone


What is the area of Acasta Gneiss?

It is located in the Northern Territories, Canada. If location is what you mean by area. To my knowledge it is the oldest rocks on Earth, formed at the end of the Hadean, some 4.01 Ga. It is highly deformed (20 km2) tonalite and granodiorite associated with amphibolite and ultra-mafic rocks, all lithologies are juxtaposed by high stress in banded rocks.