If you apply shale with intense heat and pressure. you'll get slate. Now just apply intense heat and pressure to the slate an over time you'll get your schist
it is formed from aouther rock called schist
Schist is a high-grade metamorphic rock.
Schist comes from shale. It is laminated , flaky, and found in parallel layers. The minerals in this rocks that have crystallized from the parent rock are visible.
foliated rocks, defined as "metamorphic rocks with parralel layers or "bands". three examples of these foliated rocks are gneiss, slate, and schist. three examples of foliated rocks are schist, gneiss, and schist.
Marble Gneiss Schist
Schist and gneiss are common rocks that can form after quartzite in the rock cycle. Schist forms from the metamorphism of rocks like shale or mudstone, while gneiss forms from the high-grade metamorphism of granite or other rocks.
A mixture of sand and clay, mudstone, metamorphose (process of changing from one type of rock into a metamorphic rock) into gneiss rocks or schist rocks. The mudstones would change under heat and pressure to make the new Metamorphic rocks.
No, schist is a metamorphic rock formed from the alteration of pre-existing rock under high pressure and temperature. It is characterized by its foliated structure. Clastic sedimentary rocks are formed from the accumulation and lithification of fragments of pre-existing rocks or minerals.
Parent rocks of metamorphic rocks can include sedimentary rocks, igneous rocks, and other metamorphic rocks. Some common parent rocks are shale, granite, and basalt. The mineral composition and texture of the parent rock influence the characteristics of the resulting metamorphic rock.
Schist rocks are commonly mined in regions with high metamorphic activity, such as mountainous areas and along plate boundaries. Countries known for schist mining include the United States, Norway, and regions in the Alps. Mines typically target areas where schist is exposed or easily accessible.
Some examples of metamorphic rocks include marble, slate, schist, and gneiss. These rocks are formed from the alteration of existing rocks due to high pressure and temperature underground.
Schist is a metamorphic rock.