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It is denser than 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.
The new rocks don't form from nothing. They form either from material from older rocks that were broken down, or magma that originates inside Earth. As magma rises and erupts as lava from volcanoes the crust will sink down slightly, filling in the space left behind. New oceanic crust is formed as lava erupts at mid-ocean ridges, but at the same time old oceanic crust slides down into the mantle at subduction zones.
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Earth's crust is very hard because it is made of rock. If it wasn't hard you would sink down into the Earth's core.
To begin with the Earth was like a ball of hot bubbling liquid of rocks made from different elements and compounds. Some rocks were heavier than others. The heavy rocks started to sink and moved towards the center of the earth. Lighter rocks moved towards its surface. This separation of layers took millions of years. The present day Earth comprises the crust, the mantle and the core.
the plants roots sink into the rock and cracks the rock.
A sinkhole, also known as a sink, shake hole, swallow hole, swallet, doline or cenote is a natural depression or hole in the surface topography caused by karst processes which involves the chemical dissolution of carbonate rocks.
It is denser than continental crust.
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.
The oceanic crust is denser than the continental crust.
density
changes in buoyancy due to changes in density differences between the magma and surrounding rock.
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.
when regions of earth surface sink down