marble
The 3 basic rock types are igneous, sedimentary and metamorphic rocks, which can all be changed or metamorphosed by heat and pressure.
granite
Igneous rocks
Igneous rocks
granite
Marble (metamorphosed limestone) Slate (metamorphosed shale) Gneiss (metamorphosed granite)
Nonfoliated metamorphic rock would be:Quartzite - composed of the mineral quartz; metamorphosed sandstoneMarble - composed of the mineral calcite; metamorphosed limestone
Yes, it is possible for granite to contain fossils or shells. This occurs when sedimentary rocks containing fossils or shells are metamorphosed and transformed into granite over time. The original fossils or shells may be preserved within the granite, although they may be altered or distorted due to the intense heat and pressure of the metamorphic process.
Gneiss metamorphosed from shale, sandstone, granite and conglomerate.
The 3 basic rock types are igneous, sedimentary and metamorphic rocks, which can all be changed or metamorphosed by heat and pressure.
Slate--metamorphosed shale or mudstone.Phyllite--metamorphosed slate.Quartzite--metamorphosed sandstone.
No, granite cannot become marble. Granite and marble are two distinct types of rocks formed under different geological conditions. Granite is an igneous rock formed from the cooling of molten rock, while marble is a metamorphic rock formed from the recrystallization of limestone.
Metamorphosed granite, also known as gneiss, forms when granite undergoes high temperatures and pressures deep within the Earth, causing its minerals to reorganize into distinct layers or bands. This process results in a metamorphic rock with a banded appearance and typically a coarser texture than the original granite.
gneiss
preexisting rocks that have been metamorphosed by cooking and crushing.
Deformed, and change into metamorphic rocks.
The metamorphism of granite would likely result in the formation of gneiss, a coarse-grained foliated rock with distinct bands of minerals. The high temperature and pressure during metamorphism would cause the minerals in the granite to recrystallize and align, giving gneiss its characteristic banded appearance.