Ultramafic rocks form in the Earth's crust in the upper mantle, specifically in the mantle portion known as the asthenosphere. These rocks are composed primarily of minerals rich in magnesium and iron, such as olivine and pyroxene. Ultramafic rocks are brought to the Earth's surface through processes like volcanic eruptions or tectonic movements, providing valuable insights into the composition and dynamics of the Earth's interior.
Ultramafic rocks like peridotite and dunite, are igneous rocks that have a very low silica content and very high levels of iron and magnesium. They are therefore more dense than most igneous rock and are found at great depth but appearing on the surface due to volcanic eruption.
Igneous rocks that form below Earth's surface are called intrusive or plutonic rocks. These rocks are formed from the solidification of magma beneath the Earth's crust. Examples include granite, diorite, and gabbro.
There are almost no extrusive rocks on the earths surface because they are all under the earths surface. They are mainly lower than the earths surface.
Tectonic plates are floating on the magma (semi-molten rocks) of the mantle layer. Therefore, they form the crust layer of the Earth.
Processes such as melting, recrystallization, and metamorphism occur deep in the Earth's crust. These processes involve high temperatures and pressures that cause rocks to change their form and composition.
they were and aree forced through earths crust in the form of lava.
Silicon
Extrusive ultramafic rocks are rare in Earth's crust primarily due to their high melting temperatures and the specific conditions required for their formation. These rocks, which are rich in magnesium and iron, typically form deep within the mantle where pressure and temperature are extreme. When they do erupt, they often mix with other materials or undergo crystallization processes that can alter their composition before they reach the surface. Consequently, most ultramafic material remains in the mantle rather than forming extrusive rocks on the crust.
If it finds its way dowm into the earths crust through rock cycle and then is melted and mixes together to form molten magma, it could re-erupt to the earths surface and form an extrusive igneous rock or cool and solidify within the earths crust as an intrusive igneous rock.
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.
a type of rock that forms when magma cools and hardens very slowly deep in earths crust...
Well that will be intrusive igneous rocks, extrusive forms inside the earths crust
Weight causes density, density causes pressure, pressure causes heat. Heat and pressure change rocks into other rocks, which are metamophic.
Ultramafic rocks like peridotite and dunite, are igneous rocks that have a very low silica content and very high levels of iron and magnesium. They are therefore more dense than most igneous rock and are found at great depth but appearing on the surface due to volcanic eruption.
There are actually well over 4,000 known minerals as of 2010; of these, about two dozen form the bulk of the rock of the earth's crust.
i have no clue
yes