Gneiss is a metamorphic rock that is formed when heat and pressure is applied to an igneous or sedimentary rock. The old rock does not melt completely but reorganizes it's minerals to form banks of foliation giving it the light/dark bands. Gneiss is formed when you have a parent rock that is rich in silica. Since most of the continental crust is silica rich, gneiss it a common rock. It is the highest grade of metamorphic rock in the metamorphic sequence. The sequence goes like this: slate - schist - phyllite - rock.
A rock that forms from other rocks due to heat and pressure beneath the Earth's surface is called a metamorphic rock. Examples include marble, slate, and gneiss.
A fractured surface--rough. A polished or worn surface--smooth.
Height above earths surface is called elevation
The Earth's surface layer is called the crust.
Cobbles and boulders composed of Precambrian gneiss are commonly found on the top of the surface bedrock in the Catskills because they were deposited there by glacial action during the last Ice Age. Glaciers transported these rocks from their original bedrock source areas and left them scattered across the region as they melted. The resistant nature of gneiss allows these rocks to remain on the surface long after the glaciers have retreated.
Gneiss is a part of the earths lower crust. No matter where you drill you will eventually uncover gneiss.
A rock that forms from other rocks due to heat and pressure beneath the Earth's surface is called a metamorphic rock. Examples include marble, slate, and gneiss.
100
70% or 80% of water covers the earths surface
No the crust covers earths surface
to draw the earths surface.
There are almost no extrusive rocks on the earths surface because they are all under the earths surface. They are mainly lower than the earths surface.
The tectonic plates below earths surface shape earths landforms
it is water cycle
mantle
they form above earths surface (THIS ANSWER IS NOT CORRECT) They Form BELOW earths surface(:
They both can change the size of Earths Surface