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When put under pressure, granite can change into a metamorphic rock called gneiss. Gneiss forms from the re-crystallization of granite under high temperatures and pressures, resulting in a distinctive banded appearance and different mineral composition.
Granite does not turn into limestone. Granite is an igneous rock originating from volcanic activity. Limestone is a sedimentary rock laid down in the oceans millions of years ago. Limestone does turn into marble when subjected to huge pressures and heat. It is found areas with a lot of seismic activity like Itlay and Turkey.
Yes, granite can change into gneiss through the process of metamorphism. This transformation typically involves high temperature and pressure conditions, causing the mineral composition and texture of the granite to recrystallize into the banded texture associated with gneiss.
Granite becomes Sandstone when water erodes the Granite on Earths surface, and then deposits the sediment.
When a metal is subjected to pressure, the atoms in the metal get closer together, causing the bonds between them to deform. This deformation results in a change in the arrangement of atoms, leading to a rearrangement of the crystal lattice structure. If the pressure is high enough, the metal can undergo plastic deformation and change shape.
When granite is subjected to high heat and pressure, it can change into a metamorphic rock known as gneiss. Gneiss typically exhibits a banded appearance due to the reorganization of minerals within the rock under these conditions.
If granite were subjected to intense heat and pressure, it would likely change to gneiss, a metamorphic rock. Gneiss forms through the recrystallization of minerals in granite under high temperature and pressure conditions.
Granite becomes metamorphic by being subjected to immense heat and pressure, turning into gneiss.
When granite is subjected to heat and pressure, it undergoes a process called metamorphism and can transform into a metamorphic rock called gneiss. The mineral composition and texture of the granite change during this process, resulting in a foliated texture and alignment of minerals in the gneiss.
If enough heat and pressure is applied (40000 to 60000 times atmospheric pressure and 900 to 1300 degrees Celsius), granite or any other allotrope of carbon can be turned into diamond.
Heat and pressure
Granite can change into sandstone through weathering and erosion processes, where the minerals in the granite are broken down into smaller grains and cemented together to form sandstone. Sandstone can then be subjected to heat and pressure, transforming it into quartzite through the process of metamorphism. This involves recrystallization of the minerals within the sandstone, mainly quartz, into a more tightly interlocking crystalline structure, resulting in the formation of quartzite.
When emplaced granite is subjected to pressures and temperatures from mountain building processes due to tectonic plate movements, the component minerals are essentially realigned perpendicularly to the direction of the stress.
When put under pressure, granite can change into a metamorphic rock called gneiss. Gneiss forms from the re-crystallization of granite under high temperatures and pressures, resulting in a distinctive banded appearance and different mineral composition.
Heat and pressure
Through heat and pressure
Granite does not turn into limestone. Granite is an igneous rock originating from volcanic activity. Limestone is a sedimentary rock laid down in the oceans millions of years ago. Limestone does turn into marble when subjected to huge pressures and heat. It is found areas with a lot of seismic activity like Itlay and Turkey.