marble. Through the process of metamorphism, both granite and shale can be transformed into marble when subjected to heat and pressure. This process causes the minerals within the rock to recrystallize, giving marble its characteristic appearance and texture.
Granite is a widely occurring group of intrusive, igneous rocks that form at great depth and pressure under continents. The minerals in granite are primarily quartz, feldspar, and mica.
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.
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.
Groundwater heated by magma can form geysers, where the pressure from steam and boiling water builds up underground until it forcefully ejects through the surface in a powerful spray. This process is what creates geothermal features like geysers and hot springs.
Granite can form from the cooling and solidification of molten magma under high heat and pressure, usually deep within the Earth's crust. Shale, on the other hand, can form from the compaction and cementation of mud and clay particles under relatively lower heat and pressure, typically in shallow marine environments.
marble. Through the process of metamorphism, both granite and shale can be transformed into marble when subjected to heat and pressure. This process causes the minerals within the rock to recrystallize, giving marble its characteristic appearance and texture.
Granite is a widely occurring group of intrusive, igneous rocks that form at great depth and pressure under continents. The minerals in granite are primarily quartz, feldspar, and mica.
When limestone is heated under pressure, it forms marble. This process, known as metamorphism, occurs when the mineral calcite in the limestone recrystallizes into the interlocking calcite crystals that compose marble.
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anthracite coal is the metamorphic form of bituminous coal which is the sedimentary form. in other words it has been heated under pressure.
No. Granite and basalt have different compositions and form under different circumstances.
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.
The products depend upon the pressure. At high pressure HMF alongwith levulinic acid will form. At lower pressure some aromatics could form.
The minerals in sandstone recrystallize when granite first turns into sandstone a gritty sedimentary rock under weathering and erosion and then into the metamorphic rock quartzite under heat and pressure and then it goes all the way throughout the rock cycle and back into its original form of granite a igneous rock and is formed when magma recrystallizes.
Granite turns into Gniess.
Granite is an igneous rock that forms deep underground from the cooling of molten magma. It requires heat and pressure to form, typically found in the Earth's crust.