The specific gravity, on average, of continental crust is 2.7. For oceanic crust, it's 2.9.
It depends on what kind.I like pan the best but my friend likes thin crust.
Density is basically weight. Basaltic oceanic crust is more dense than granitic continental crust because basalt is more dense (heavier) than granite.
oceanic crust
the crust is dense
Dense oceanic crust slides under less dense continental crust
less dense and more felsic
Oceanic crust is thinner and more dense, while continental crust is thicker and less dense.
Because continental crust is less dense and thicker than oceanic crust, it "floats" higher on the underlying mantle rock. Notice how high the continental crust rises above the oceanic crust in this cross section of the North American Plate. Oceanic crust is made of dense basalt; continental crust consists of less dense granite
Because its less dense
Dense oceanic crust slides under less dense continental crust
The crust is the least dense. The inner core is the most dense. So from the middle outwards the layers get less and less dense
Continental crust is thicker but less dense, and oceanic crust is thinner but more dense, making it heavier.
less dense than the material of the Earth's mantle
less dense and more felsic
Oceanic crust is thinner and more dense, while continental crust is thicker and less dense.
The continental crust is less dense
The more dense oceanic crust will submerge below the less dense South American plate. This submergence leads to the melting of the oceanic crust and the production of magma that fuels the Andes Volcanic range.
Continental crust is easier. Continental crust is less dense than oceanic crust, which is made of basalt. (Basalt is very dense.)
subduction
subduction
subduction