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continental oceanic
Eventually the oceanic crust, along with the magnetically aligned minerals contained within, will be subducted into the mantle.
Silicon (Si), Magnessium (Ma), and Iron (Fe).
Basalt rock with a layer of sedimentary rock overlaying that, covered with water saturated sediments.
c plates- bedrock and granite o plates- bastlic
Oceanic crust is mafic in composition and continental crust is felsic in composition. Mafic minerals generally have a higher density than felsic minerals and therefore, the oceanic crust is heavier.
continental oceanic
the oceanic plate
Minerals are not classified as metamorphic. The mid-oceanic ridges are generally considered to be areas where new basaltic crust is formed from uprising magma. The basalt is considered an igneous rock in classification.
Eventually the oceanic crust, along with the magnetically aligned minerals contained within, will be subducted into the mantle.
There are far more than two minerals that form rocks. You have to consider that there are about 3800 known minerals found on Earth. However, two minerals that are extremely abundant in continental and oceanic rock are feldspar and quartz.
Silicon (Si), Magnessium (Ma), and Iron (Fe).
Basalt rock with a layer of sedimentary rock overlaying that, covered with water saturated sediments.
If the plates are moving toward each other, the more dense oceanic plate will subduct underneath the less dense continental plate. Mountain ranges and volcanism may result as the water saturated subducting oceanic crust creates molten rock which attempts to rise to the surface.
c plates- bedrock and granite o plates- bastlic
Ocean water absorbs a lot of minerals because water is such an excellent solvent for so many substances. Combine with that, the abundance of existing dissolved materials that can form soluble salts with many existing minerals and you have an excellent environment for dissolving minerals that start out as oxides.
Oceanic crust is more dense than continental crust and is comprised of mainly mafic minerals (Mg, Fe), as opposed to continental crust, which is mainly felsic (Al and Si rich).