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Nonfoliated metamorphic rock would be:Quartzite - composed of the mineral quartz; metamorphosed sandstoneMarble - composed of the mineral calcite; metamorphosed limestone
Garnet is a mineral, of the Al SiO3 community, with other contributions as well. Some times used as a minor gemstone. A cubic mineral, found often enough in metamorphosed rocks such as schist.
Igneous rocks are metamorphosed by heat and pressure while still in a solid state. The mineral grains of the igneous rock migrate or reorganize to form the well known banded appearances in rocks like gneiss.
Yes they can, the mineral assemblage in a metamorphic rock reflects and equilibrium state pertaining to the temperatures and pressures to which it has been subject. If the rock is subsequently taken to a different Pressure/temperature environment, an new equilibrium mineral phase will start to develop.
Depends on which one. Diamond is a metamorphosed coal/carbon that is the hardest natural substance known. Marble is metamorphosed limestone that is much softer. It's safe to say that all metamorphosed rocks are harder than they were in their pre-metamorphosed form.
Nonfoliated metamorphic rock would be:Quartzite - composed of the mineral quartz; metamorphosed sandstoneMarble - composed of the mineral calcite; metamorphosed limestone
Slate--metamorphosed shale or mudstone.Phyllite--metamorphosed slate.Quartzite--metamorphosed sandstone.
The 3 basic rock types are igneous, sedimentary and metamorphic rocks, which can all be changed or metamorphosed by heat and pressure.
Metamorphic rocks can undergo further metamorphism through additional heat and pressure. They can also be melted, then cooled, and become igneous rock. They can also erode and become components of sedimentary rocks.
by heat and pressure on the rock
Garnet is a mineral, of the Al SiO3 community, with other contributions as well. Some times used as a minor gemstone. A cubic mineral, found often enough in metamorphosed rocks such as schist.
Igneous rocks are metamorphosed by heat and pressure while still in a solid state. The mineral grains of the igneous rock migrate or reorganize to form the well known banded appearances in rocks like gneiss.
Yes they can, the mineral assemblage in a metamorphic rock reflects and equilibrium state pertaining to the temperatures and pressures to which it has been subject. If the rock is subsequently taken to a different Pressure/temperature environment, an new equilibrium mineral phase will start to develop.
Yes, igneous rocks can be metamorphosed or weathered and eroded.
No, to make a rock a mineral does not have to be in it.
Quartzite is sandstone (sedimentary rock) that has metamorphosed from heat and pressure.
A rock is not a mineral however a rock is made of several minerals