Ocean crust is denser
The ocean crust dives below the continental crust due to a collision. This collision involves the two types of crust and since the oceanic crust is denser, it sinks to the bottom while the less dense continental crust rises to the top.
Because of its higher density, and gravity. One part of plate tectonic theory.
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
A deep ocean trench is formed when ocean crust subducts below continental crust. The descending oceanic plate is forced down into the mantle by the more buoyant continental plate. This process can also lead to the formation of volcanic arcs on the overriding plate.
Ocean crust is typically denser than continental crust because it contains more basalt (rich in iron and magnesium), whereas continental crust is composed of less dense granite (richer in aluminum and silicon).
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The Earth's crust is thinner than the ocean floor because the oceanic crust is formed at mid-ocean ridges where heat from the mantle creates new crust through volcanic activity. This process creates younger, hotter, and thinner crust in the ocean compared to the older and thicker continental crust.
It is not. The oceanic crust is thinner than the continental crust!
Oceanic crust is denser and thinner than continental crust, so when the two converge at a subduction zone, the oceanic crust is forced to sink beneath the less dense continental crust. This process of subduction is driven by the difference in density between the two types of crust, as well as the movement of tectonic plates.
They weld together into new continental crust.
Because the oldest parts reach the continental crust and then the ocean floor sinks beneath the continental crust, into the mantle.
Oceanic crust is typically thinner, denser, and younger than continental crust. It is primarily composed of basaltic rocks and forms the ocean floor, while continental crust is thicker, less dense, and contains a wider variety of rock types, including granitic rocks. Continental crust forms the continents and is older than oceanic crust.