Subduction.
A convergent plate boundary where one plate subducts beneath another destroys crust. This process occurs at subduction zones, where the denser plate is forced beneath the less dense plate, leading to the destruction of crust as it is consumed in the Earth's mantle.
The two types of Crust is the Continental Crust and the Oceanic Crust.
The type of boundary that forms when the crust of one plate is pushed down under another plate and turned into molten rock is referred to as a convergent boundary. Convergent boundaries form when oceanic crust slides beneath continental crust.
It forms a convergent boundary with the South American Plate, divergent.
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
A hot spot is an area where magma from deep within the mantle rises through the crust in the middle of a tectonic plate, creating volcanic activity and forming a chain of volcanic islands or seamounts. The Hawaiian Islands are a well-known example of hot spot activity.
recessive plate boundary
Divergent plate boundary.
Crust is destroyed at the convergent plate boundary. This is usually between the oceanic and continental plates. This is where subduction of the more dense crust occurs.
Convergent plate boundaries.
A convergent plate boundary where one plate subducts beneath another destroys crust. This process occurs at subduction zones, where the denser plate is forced beneath the less dense plate, leading to the destruction of crust as it is consumed in the Earth's mantle.
The Divergent Boundaries.
The two types of Crust is the Continental Crust and the Oceanic Crust.
Subduction boundaries, where one tectonic plate is forced below another, can destroy crust as the subducting plate melts and is absorbed into the mantle. This process can lead to the recycling of crustal material back into the Earth's interior.
This would be called a Spreading center, or a divergent plate boundary.
tides will occur.
The type of boundary that forms when the crust of one plate is pushed down under another plate and turned into molten rock is referred to as a convergent boundary. Convergent boundaries form when oceanic crust slides beneath continental crust.