False! When two continental plates converge a mountain range is formed. This is what formed and is continuing to "build" the Himalayan mountain chain.
Subduction zones form where oceanic crust converges with and is forced under continental crust, or younger more buoyant oceanic crust.
Oceanic-continental convergent boundary: Where oceanic plates subduct beneath continental plates, creating deep ocean trenches and volcanic arcs on the overriding plate. Continental-continental convergent boundary: Where two continental plates collide, causing intense folding and faulting to create mountain ranges. An example is the collision of the Indian Plate with the Eurasian Plate, forming the Himalayas.
When two oceanic plates converge, one plate subducts beneath the other due to differences in density. This can create deep ocean trenches and volcanic arcs as magma rises to the surface. Over time, this process can form new oceanic crust and island chains.
Subduction
Magma is generated along subduction zones when oceanic plates are forced beneath continental plates. The intense heat and pressure cause the oceanic plate to melt, creating magma that rises to the surface and forms volcanoes.
A continental volcanic arc is a chain of volcanoes that forms on a continental plate where two tectonic plates converge. The subduction of an oceanic plate beneath a continental plate results in magma generation and volcanic activity along the continental margin. These volcanic arcs are associated with earthquakes, volcanism, and mountain building.
mountains
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
No. Continental convergent plate boundaries form fold mountain ranges. A rift valley will form at a divergent plate boundary.
These zones are known as subduction zones where tectonic plates collide, forcing one plate to be pushed beneath the other. This process leads to the formation of deep ocean trenches and can result in earthquakes, volcanic activity, and the creation of mountain ranges.
Oceanic-continental convergent boundary: Where oceanic plates subduct beneath continental plates, creating deep ocean trenches and volcanic arcs on the overriding plate. Continental-continental convergent boundary: Where two continental plates collide, causing intense folding and faulting to create mountain ranges. An example is the collision of the Indian Plate with the Eurasian Plate, forming the Himalayas.
When two oceanic plates converge, one plate subducts beneath the other due to differences in density. This can create deep ocean trenches and volcanic arcs as magma rises to the surface. Over time, this process can form new oceanic crust and island chains.
As oceanic crust is thinner, it sinks under the continental crust and forms a subduction zone. This can also form a line of volcanoes.a deep sea trench and an island arc form.
Subduction
Magma is generated along subduction zones when oceanic plates are forced beneath continental plates. The intense heat and pressure cause the oceanic plate to melt, creating magma that rises to the surface and forms volcanoes.
A continental volcanic arc is a chain of volcanoes that forms on a continental plate where two tectonic plates converge. The subduction of an oceanic plate beneath a continental plate results in magma generation and volcanic activity along the continental margin. These volcanic arcs are associated with earthquakes, volcanism, and mountain building.
The type of collision that occurs when two lithospheric plates converge is determined primarily by plate density. If both plates are of similar density, a continental-continental collision may occur, resulting in mountain-building and seismic activity. If one plate is denser than the other, a subduction zone may form where one plate is forced beneath the other, leading to volcanic activity and the formation of oceanic trenches.
mountain or volcanoe