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∙ 13y agoschist and gneiss arefoliated and in gneiss you can see the bands.
Wiki User
∙ 13y agoThe presence of visible minerals aligned in bands or layers would distinguish schist and gneiss from quartzite and marble. Schist and gneiss show foliation due to intense metamorphism, while quartzite and marble are more homogenous in texture.
Schist and gneiss have a banded texture, whereas quartzite and marble have a more uniform appearance. Schist typically contains platy minerals like mica, while gneiss has alternating layers of different mineral compositions. Quartzite is composed mainly of quartz grains, while marble is comprised of recrystallized calcite or dolomite minerals.
Gneiss differs from the rock it was formed from by having distinct layering or banding of minerals, a higher degree of metamorphism, and a more pronounced foliation. The original rock's mineral composition and texture have been fundamentally changed during the process of gneiss formation.
Schist and gneiss are common rocks that can form after quartzite in the rock cycle. Schist forms from the metamorphism of rocks like shale or mudstone, while gneiss forms from the high-grade metamorphism of granite or other rocks.
Gneiss is a metamorphic rock that typically displays ductile behavior due to its layered composition and high temperature and pressure conditions during formation. This means that it is more likely to be deformed without breaking easily compared to brittle rocks like quartzite.
The protolith of a quartzite is a sedimentary rock called sandstone. Quartzite forms when sandstone undergoes metamorphism, typically due to high heat and pressure, causing the quartz grains in the sandstone to recrystallize and merge together.
Schist and gneiss have a banded texture, whereas quartzite and marble have a more uniform appearance. Schist typically contains platy minerals like mica, while gneiss has alternating layers of different mineral compositions. Quartzite is composed mainly of quartz grains, while marble is comprised of recrystallized calcite or dolomite minerals.
gneiss is foliated(layered) so therefore, if you see a black and white gneiss and a similar-colored granite then just see if the gneiss looks like it is layered!
- Amphibolite - Eclogite - Gneiss - Greenstone - Hornfels - Marble - Migmatite - Phyllite - Quartzite (Metaquartzite) - Schist - Slate - Soapstone
Gneiss differs from the rock it was formed from by having distinct layering or banding of minerals, a higher degree of metamorphism, and a more pronounced foliation. The original rock's mineral composition and texture have been fundamentally changed during the process of gneiss formation.
they're all metamorphic
Gneiss has a definite foliation of fabric, granite does not.
quartzite, slate, gneiss, marlbe, migmitite, amphibolite, serpenrinite, eclogite. that's all i have from my school papers. quartzite, slate, gneiss, marlbe, migmitite, amphibolite, serpenrinite, eclogite. that's all i have from my school papers.
Pennsylvania is home to quartzite, slate, marble, phyllite, gneiss, and schist
marble used to be limestone
Schist and gneiss are common rocks that can form after quartzite in the rock cycle. Schist forms from the metamorphism of rocks like shale or mudstone, while gneiss forms from the high-grade metamorphism of granite or other rocks.
Gneiss is a metamorphic rock that typically displays ductile behavior due to its layered composition and high temperature and pressure conditions during formation. This means that it is more likely to be deformed without breaking easily compared to brittle rocks like quartzite.
Sandstone can metamorphose into quartzite.