the conditions are very high heat (hot enough to melt the rock), and/or very high pressure (to recombine the elements in the rock).
Increased temperatures and or decreased pressures.
Other types of rocks include volcanic rocks (such as basalt and pumice), hydrothermal rocks (like geyserite and travertine), and organic rocks (such as coal and limestone). These rocks form from specific processes or conditions that differ from the formation of igneous, sedimentary, and metamorphic rocks.
Some extrusive rocks such as lava and ejecta form in minutes. Stalactites may form in a few tens of years, but commonly longer. Other rocks may take millions of years, and may have to be recycled through metamorphism to attain their final form.
Petrology is the branch of geology that focuses on the study of the origin, composition, and structure of rocks. It involves understanding how rocks form, their classification, and the processes that lead to their formation and alteration.
Gneiss rocks form from the metamorphism of existing rocks, such as granite or sedimentary rocks, under high temperature and pressure conditions deep within the Earth's crust. This process causes mineral grains in the rock to recrystallize and rearrange, giving gneiss its characteristic banded appearance.
Because of how they form and what conditions they form under.
Increased temperatures and or decreased pressures.
Metamorphic rocks form deep underground under high pressure and heat conditions, typically within the Earth's crust. They can also form at plate boundaries where tectonic forces cause rocks to be buried and subjected to these extreme conditions.
metamorphic rock are used for nothing
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.
Hyperbasal Intrusive Rocks.
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.
Rocks such as gneiss and schist form under high temperature and pressure conditions found a few kilometers beneath the Earth's surface. These rocks are typically a result of metamorphic processes that alter existing rock types like granite or basalt.
Garnets form from the metamorphism of pre-existing rocks under high pressure and temperature conditions. They can also form through the crystallization of fluids in the Earth's crust. Garnets are commonly found in metamorphic rocks like schist and gneiss, as well as some igneous rocks.
Sedimentary rocks such as sandstone and shale can form when materials are squeezed together due to pressure from overlying sediments and compaction. Igneous rocks can also form from intense pressure transforming existing rocks, such as with the formation of gneiss from granite under high pressure and temperature conditions.
Igneous rocks are formed under high heat conditions. Intrusive igneous rocks are formed by the crystallization of magma in the Earth's crust.
The conditions that affect physical stability are heat, temperature, compression, pressure, and the molecular structure.