no its not
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.
A coarsely foliated rock with a banded appearance is called a gneiss. Gneiss forms from the metamorphism of existing rocks, typically granite or sedimentary rocks like shale or sandstone, resulting in distinct banding of different minerals.
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.
When heat and pressure are applied to granite, it transforms into a metamorphic rock called gneiss. Gneiss typically exhibits banded textures and can contain minerals such as quartz, feldspar, and mica that have been reoriented due to the intense pressure and heat.
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.
A type of metamorphic rock similar to granite is gneiss. Gneiss is a foliated metamorphic rock that has a similar composition to granite but displays a banded texture due to the alignment of mineral grains during metamorphism.
Well, friend, banded rocks are often made up of layers of different materials, like sedimentary rocks such as sandstone or shale. Non-banded rocks, on the other hand, can include igneous rocks like granite or basalt, which are formed from cooled magma without distinct layers. Both types of rocks have their own unique beauty and story to tell in the great tapestry of the Earth.
A banded metamorphic rock formed from the re-heating and re-pressuring of granite and similar igneous rocks.
Granite heated under pressure can form a type of metamorphic rock called gneiss. This process causes the minerals in the granite to recrystallize and align in distinct patterns, giving gneiss its characteristic banded appearance.
No. Foliation is a texture most often used to describe the banded, platy, or layered appearance of certain metamorphic rocks.
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.
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.
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.
Yes, the gneiss rocks are usually crystalline. The gneiss rocks are foliated or banded metamorphic rocks that have the same composition as the granite.
Granite is a common non-banded rock that is formed from the slow crystallization of molten magma deep within the Earth's crust. It is a coarse-grained rock composed mainly of quartz, feldspar, and mica minerals.
When granite is subjected to high heat and pressure without melting, it transforms into a type of metamorphic rock known as gneiss. This process involves the recrystallization of minerals within the granite, leading to a banded or foliation structure typical of gneiss. The minerals within the granite, such as quartz and feldspar, may realign and change in composition due to the extreme conditions.
A coarsely foliated rock with a banded appearance is called a gneiss. Gneiss forms from the metamorphism of existing rocks, typically granite or sedimentary rocks like shale or sandstone, resulting in distinct banding of different minerals.