When gneiss is melted, it undergoes a process known as partial melting, which transforms it into magma. The composition of the resulting magma can vary depending on the minerals present in the gneiss, typically producing a granitic or dioritic magma. As the magma cools and solidifies, it can form igneous rocks, such as granite or diorite, depending on the cooling rate and environmental conditions. This process is part of the rock cycle, where metamorphic rocks like gneiss can be recycled into new igneous formations.
"lava"
It solidifies.
When old rocks are partially melted or squeezed, they can form metamorphic rocks. Examples include gneiss, schist, and marble. These rocks exhibit new textures and compositions due to the heat and pressure they have experienced.
These coins are melted and recycled.
Gneiss usually consists of visible crystals of aligned mineral assemblages.
"lava"
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.
energy is released
It solidifies.
When old rocks are partially melted or squeezed, they can form metamorphic rocks. Examples include gneiss, schist, and marble. These rocks exhibit new textures and compositions due to the heat and pressure they have experienced.
A Gneiss is a Metamorphic rock
Gneiss is foliated.
Ice is melted over 0 0C and salt is melted over 801 0C.
No, gneiss is metamorphic.
Gneiss is foliated and coarse grained
Gneiss is a rock, not a mineral.