Trenches. An example would be the deepest point of the ocean in the world, which is a trench in Japan.
oceanic crust and continental crust collide, with the continental crust subducting under the oceanic
Thickness - continental = much thickerDensity - oceanic crust is denser than continental, which is why the oceanic crust subducts under the continental at destructive plates boundaries.
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
the lithosphere is thinner under the oceanic crust
The oceanic crust will slide under the continental crust. And the reason is because the oceanic crust is much denser and the continental crust is least dense.
oceanic crust and continental crust collide, with the continental crust subducting under the oceanic
Thickness - continental = much thickerDensity - oceanic crust is denser than continental, which is why the oceanic crust subducts under the continental at destructive plates boundaries.
Oceanic crust sinking under a plate with continental crust
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
the lithosphere is thinner under the oceanic crust
The ocean is never pulled under the continent. Oceanic crust--the rock and some sediments, however, slide under the edges of continental crust and are pushed downward toward the mantle in areas of oceanic to continental plate collisions.
The oceanic crust will slide under the continental crust. And the reason is because the oceanic crust is much denser and the continental crust is least dense.
The continental crust is the land. The oceanic is under the ocean.
The continental crust is the land. The oceanic is under the ocean.
The mountains on the west coast of North America, such as the Cascade Range and Sierra Nevada, were mainly formed by the movement of tectonic plates. The collision of the Pacific Plate with the North American Plate caused compression and uplift, leading to the formation of the mountain ranges we see today. Additionally, volcanic activity played a significant role in shaping these mountain ranges over millions of years.
denser