oceanic and the continental crust
When two oceanic crusts converge, one plate is typically forced beneath the other in a process known as subduction. This leads to the formation of deep ocean trenches and can result in volcanic activity as the subducted plate melts and generates magma. The interaction can also create earthquakes due to the friction and stress between the colliding plates. Over time, this process contributes to the recycling of oceanic crust back into the mantle.
The lithosphere is composed of the oceanic and continental crusts.
Yes, it is.
The contiental cdrust is forced under the continental crust in a process called subduction.
The rocks that makes up the oceanic crusts, are very dark, relatively thin and highly dense.
Near ocean ridges such as the Atlantic ridge
When two plates carrying oceanic crusts meet at a trench, one plate typically subducts beneath the other due to its higher density. This process can generate volcanic activity, earthquakes, and the formation of deep-sea trenches and volcanic island arcs.
When two oceanic crusts collide, the older plate is forced under the younger one and is pulled under it, forming a subduction zone. This leads to the formation of chains of volcanic islands known as island arcs.
When two oceanic crusts collide, the older plate is forced under the younger one and is pulled under it, forming a subduction zone. This leads to the formation of chains of volcanic islands known as island arcs.
Both oceanic and continental crusts consist primarily of igneous rock although they both contain some sedimentary rock. Oceanic crust is composed mainly of basaltic rock, while continental crust is composed of granitic rock.
When two crustal plates are in the process of collision they deform, the results of which vary:continental-continental, large mountain building (e.g. asia-india building the himalayas)oceanic-oceanic, island arc building with volcanic islands (e.g. the Japanese islands)oceanic-continental, subduction of oceanic plate under continental plate with inland volcanoes (e.g. volcanoes in Washington, Oregon, and northern California)