Yes and no. Deep inside the Earth implies the core/mantle region and Gneisses do not form there they form towards the base of the continental crust at a depth of 25 to 70 Km. (Which is quit near the surface of the Earth).
Diamonds are formed deep within the earth's mantle.
The type of rocks formed from existing rocks that have been squeezed and heated deep inside Earth's crust are called metamorphic rocks. This transformation occurs through a process known as metamorphism, which alters the mineral composition and structure of the original rocks, known as parent rocks. Common examples of metamorphic rocks include schist, gneiss, and marble.
Intrusive rocks are formed by the cristalization and cooling of magma deep inside the Earth.
No , because it has to be deep inside the earth so it ca be pushed up.
Intrusive rocks are formed by the cristalization and cooling of magma deep inside the Earth.
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.
When magma cools deep inside earth, igneous rockforms.
Granite subjected to high temperature and pressure deep within the Earth without melting would likely undergo a process called metamorphism, and would form a metamorphic rock known as gneiss. Gneiss is characterized by its banded appearance due to the reorganization of minerals under intense heat and pressure.
This rock is likely a type of metamorphic rock called gneiss. Gneiss forms under high heat and pressure conditions deep within the Earth's crust. The alternating layers of dark and light colors are a result of the rock's minerals recrystallizing into bands.
deep inside the earth
If granite is subjected to high temperatures and pressures deep within the Earth without melting, it will undergo metamorphism and transform into a metamorphic rock known as gneiss. This process involves the recrystallization of minerals and the alignment of mineral grains, resulting in a foliated texture. Gneiss typically exhibits distinct banding and variations in mineral composition compared to the original granite.
A volcano is formed when magma from deep inside the Earth rises to the surface and explodes with great force, spreading lava and ash everywhere.