its destroyed on avi face
Oceanic crust is destroyed at convergent plate boundaries, where two tectonic plates collide. Subduction occurs at these boundaries, where the denser oceanic crust is forced beneath the less dense continental crust into the mantle, resulting in its destruction.
The two types of Crust is the Continental Crust and the Oceanic Crust.
The destructive boundary where the sea floor is destroyed is called a subduction zone. In this type of boundary, one tectonic plate is forced beneath another plate, causing the oceanic crust to be destroyed as it moves into the Earth's mantle. This process can lead to the formation of deep oceanic trenches and volcanic arcs.
Oceanic crust isn't destroyed because it's old; it is, in fact, destroyed due to destructive plate boundaries. This is where a continental plate and an oceanic plate move towards each other. As the oceanic crust is denser, it is pushed under the continental plate. Here it is forced into the mantle of the earth, where it is destroyed due to heat and convection currents.
The sea floor is destroyed in subduction zones, where one tectonic plate is pushed beneath another. This process is responsible for the destruction of oceanic crust and the formation of deep ocean trenches.
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.
Oceanic crust is destroyed at convergent plate boundaries, where two tectonic plates collide. Subduction occurs at these boundaries, where the denser oceanic crust is forced beneath the less dense continental crust into the mantle, resulting in its destruction.
Old crust can be destroyed bysubduction, or the pushing down of an oceanic plate below anoverriding plate at a convergent boundary. The initial phase of adivergent boundary is a rift valley, which progresses to form anoceanic basin with a mid-oceanic ridge.
The type of plate boundary where oceanic crust is destroyed is called a convergent boundary, specifically a subduction zone. At these boundaries, one tectonic plate, typically oceanic, is forced beneath another plate, which can be either oceanic or continental. This process leads to the formation of deep ocean trenches and can result in volcanic activity and earthquakes. An example of this is the boundary between the Nazca Plate and the South American Plate.
The two types of Crust is the Continental Crust and the Oceanic Crust.
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
The destructive boundary where the sea floor is destroyed is called a subduction zone. In this type of boundary, one tectonic plate is forced beneath another plate, causing the oceanic crust to be destroyed as it moves into the Earth's mantle. This process can lead to the formation of deep oceanic trenches and volcanic arcs.
recessive plate boundary
tides will occur.
Crust is destroyed at the convergent plate boundaries in Earth. In between the oceanic and continental plates, the subduction of the denser oceanic crust takes place.
Oceanic crust isn't destroyed because it's old; it is, in fact, destroyed due to destructive plate boundaries. This is where a continental plate and an oceanic plate move towards each other. As the oceanic crust is denser, it is pushed under the continental plate. Here it is forced into the mantle of the earth, where it is destroyed due to heat and convection currents.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.