It's generally over 9000
Old crust is removed in subduction zones through a process known as subduction. When two tectonic plates converge, one plate is forced beneath the other into the Earth's mantle. As the descending plate sinks, it carries the old crust with it. The intense heat and pressure of the mantle eventually cause the old crust to melt and recirculate into the mantle, where it can contribute to the formation of new crust.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
Subduction zones.
As new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
subdution zone
The active earth's core continually recycles itself through subduction zones located around certain parts of the planet. The subduction zones are where one tectonic plate is being forced under another, thereby recycling the old crust. New crust is made at rift zones where magma is forced to the surface, cools and then becomes part of our visible (or underwater) earth surface.
At subduction zones along convergent plate boundaries.
Plate tectonic movement and subduction zones.
No. Mid oceanic ridges are the places where new oceanic crust are forming.
Oceanic crust is denser than continental crust due to its higher levels of iron and magnesium, causing it to sink below the continental crust in subduction zones. The cooler, denser oceanic plate is pulled down by gravity into the mantle, initiating the process of subduction. This movement also generates volcanic activity and seismic events along the subduction zone.
It will get pushed under the crust and then it will enter something called the subduction zone the plate that slides over the old crust will create either a volcano or a mountain and the old crust will turn into a trench or anything of that source. Hope it helped
Subduction zones represent convergent boundaries, where two tectonic plates are colliding. In a subduction zone, one plate is forced beneath the other into the Earth's mantle, leading to the formation of deep oceanic trenches, volcanic arcs, and earthquakes. This process can generate powerful geohazards such as tsunamis and volcanic eruptions.