Under the effects of pressure and temperature, shale can either melt into magma, become flattened, or create a bigger mineral.
As you increase the temperature and pressure of Shale it metamorphism occurs. It changes in this order: Shale > Slate > Phyllite > Schist > Gneiss > Migmatite
shale is metamorphic, which means time, pressure and temperature has altered it. Sandstone is sedimentary which means it was formed under water. generally sandstone is younder.
Slate forms from shale under pressure.
Pressure
pressure
Shale that is exposed to high temperature and pressure and turned to slate is an example of the metamorphic process.
As you increase the temperature and pressure of Shale it metamorphism occurs. It changes in this order: Shale > Slate > Phyllite > Schist > Gneiss > Migmatite
Slate forms from shale under pressure.
shale is metamorphic, which means time, pressure and temperature has altered it. Sandstone is sedimentary which means it was formed under water. generally sandstone is younder.
Shale rocks turn into clay. The pressure make shale into clay.
Shale (a sedimentary rock) transforms naturally into slate (a metamorphic rock) after millions of years of burial deep in the crust under high temperature and pressure. It it not possible to artificially transform shale into slate.
Slate is the metamorphic rock that forms from shale after it is exposed to heat and pressure for a llllloooooonnnnnnnggggg time.
Schist is a foliated metamorphic rock. It is formed when mudstone, shale, slate, or phyllite are subjected to higher temperature and pressure.
Shale can metamorphose through heat and pressure into slate.
Slate is so hard because it came from shale that is put under pressure with high temperature. The clay composition of shale converts to mica, making it hard.
mudstone and shale. These can become the metamorphic rock slate if exposed to high pressure and temperature.
Possibly shale, as it goes through a series of metamorphic transitions from slate to migmatite.