It is denser than continental crust.
yes it can
In technical terms, the oceanic crust is denser than the continental crust so when the continental crust and the oceanic crust meet the continental crust will sink under and the oceanic crust will slide over and a volcano will be formed as well as producing earthquakes in the process.
The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.Continental crust is less dense than oceanic crust and so cannot sink below it.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.
Eventually the oceanic crust, along with the magnetically aligned minerals contained within, will be subducted into the mantle.
oceanic crust.
density
Continental crust is much thicker than oceanic crust. However, continental crust is denser and will therefore sink in subduction zones.
Is there magnetic stripe son the ocean floor are places where oceanic crust sink back to the mantle
In technical terms, the oceanic crust is denser than the continental crust so when the continental crust and the oceanic crust meet the continental crust will sink under and the oceanic crust will slide over and a volcano will be formed as well as producing earthquakes in the process.
The oceanic crust is denser than the continental crust.
The continental crust is less dense than the oceanic crust. That's the reason we find that the oceanic crust sinks (subducts) beneath the continental crust.Continental crust is less dense than oceanic crust and so cannot sink below it.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.
Subduction.
Eventually the oceanic crust, along with the magnetically aligned minerals contained within, will be subducted into the mantle.
Oceanic crust is more dense than continental crust. As a result, over time, continental crust is harder to "recycle". Rocks are recycled when they are subducted and remelted. Since continental crust is harder to subduct (it wants to keep floating), it is not recycled as much as oceanic crust, which is dense and will sink and remelt.
oceanic crust.
Conduction. Heat istransferred from the mantle to the crust, melting it to become part of the mantle.