One of the most popular metamorphic rocks is marble. Originally limestone, marble is generally created through regional metamorphism, which is when pressure and heat from where magma is pushing up through the Earth's crust effect rocks which are close by, but not actually touching the magma. Contact metamorphism changes the rocks that do actually touch the magma, this is how shale is usually metamorphosed into gneiss.
Quartzite, marble, and metabasalt are non-foliated metamorphic rocks..................................... i like dots
Slate
An example of foliation is the parallel alignment of minerals in a metamorphic rock, such as schist or gneiss. This alignment results from the pressure and temperature conditions during the rock's formation, creating a layered or banded appearance.
No.
From increased pressure and/or heat. Fluid removal results in hydrous mineral destruction and non-hydrous mineral creation, resulting in rock of a different mineralogy. A metamorphic rock can be further metamorphosed by additional heat and/or pressure into a rock with a higher degree of metamorphism. An example of this would be the metamorphic rock slate changing into the metamorphic rock phyllite.
Shale is a sedimentary rock, not a metamorphic rock.
Gneiss is an example of a metamorphic rock.
No. Gneiss is a metamorphic rock.
Quartzite, marble, and metabasalt are non-foliated metamorphic rocks..................................... i like dots
how is marble an example of metamorphic rock#
Phyllite is an example of a fine-grained foliated metamorphic rock
Metamorphic rock is rock that has changed as a result of constant heat, pressure, or both. One good example is granite.
Slate
When sedimentary rock undergoes enough heat and pressure, it becomes metamorphic rock. A classic example of this is when shale becomes slate.
Alot of them. Basalt, Granite, sandstone, siltstone etc
A metamorphic rock.
in a metamorphic rock you find rock.