Consequently due to buoyancy the continental crust rides above the oceanic lithosphere and.
Basaltic igneous rocks are lower in density than granitic rocks.
Rich in quartz and potassium feldspar.
Lava that cools quickly forms rocks.
Light colored igneous rock of lower density than basaltic rock formed from magma rich in silica but poor iron and magnesium.
Lower in density than basaltic rocks d.
High in silica content b.
The density of the continental granitic lithosphere is lower than oceanic basaltic lithosphere.
Sedimentary rocks and granite which are rich in quartz and feldspar tend to be less dense than volcanic rocks.
Continental crust density 2 7 2 8.
They have a higher silica content and a lower iron and magnesium content than the other types of rock.
Intrusive slowly cooled inside the crust.
High in iron content.
Igneous rock with a mineral composition between that of basaltic and granitic rock.
Rock density is very sensitive to the minerals that compose a particular rock type.
This magma is thick and stiff.
Granite and rhyolite are felsic igneous rocks intermediate igneous rocks have a density.
Plutonic rock formed in the earth.
A basalt is about 53 sio2 whereas granite is 73.
Igneous rocks are formed by the crystallisation of a magma.