It is subducted toward the core and eventually melts, forming magma.
In a subduction zone the crust is forced inot the mantle where it is eventually melted and destroyed
Continental crust, on average, is much thicker than oceanic crust. Because of the principles of isostacy and buoyancy, the continental crust will protrude more deeply into the asthenosphere than oceanic crust.
Old oceanic crust is primarily recycled back into the Earth's mantle at subduction zones, where one tectonic plate is forced beneath another. This process leads to the destruction of the oceanic crust, as it melts and contributes to mantle convection. Additionally, some old crust may be uplifted and exposed through tectonic processes, such as orogeny, but the majority is eventually subducted and assimilated into the mantle.
Oceanic crust sinks beneath trenches through a process known as subduction. As oceanic plates collide with continental plates, the denser oceanic plate is forced downward into the mantle due to gravitational pull. This creates a subduction zone where the oceanic crust eventually melts and is recycled back into the mantle.
No, the magnetic stripes on the ocean floor form due to the alignment of magnetic minerals in the crust as it solidifies from the mantle. The oceanic crust is eventually consumed in subduction zones and recycled back into the mantle, but the magnetic stripes themselves do not sink back into the mantle.
When continental plates collide, the denser oceanic crust is usually subducted beneath the less dense continental crust. This process can create subduction zones, where the oceanic crust is forced downward into the mantle. The oceanic crust may melt or be recycled back into the mantle in these subduction zones.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
Oceanic crust sinking under a plate with continental crust
Oceanic crust is mafic.
the oceanic crust is 0.
The youngest parts of the Earth's crust are found in the oceanic crust. This crust is continuously being created at the mid-oceanic ridges.
Oceanic crust is significantly denser.