When two convergent plate boundaries have equal density, they push against each other and form a mountain chain. Examples of convergent plate boundaries are the western coast of South America and the Himalayan Mountains.
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.
No, subducting plate and oceanic plate are not the same. An oceanic plate is a type of tectonic plate that lies beneath the ocean, while a subducting plate refers to an oceanic plate that is descending beneath another tectonic plate at a convergent boundary. Subducting plates are a specific category of oceanic plates.
When two oceanic plates converge and one is subducted into the mantle, the subducted plate melts due to the high temperatures and pressure, forming magma. This magma can then rise to the surface, leading to volcanic activity. Additionally, the subducted plate can cause earthquakes as it descends into the mantle.
Oceanic-continental convergent boundaries form mountains with a volcanic origin, such as the Andes in South America. Oceanic-oceanic convergent boundaries create volcanic island arcs, like the Japanese archipelago.
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.
subduction zones
subduction zones
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.
When an oceanic to oceanic happens, two oceanic plates converge and one of the plates subducts into a trench. The subducted plate sinks down into the mantle and begins to melt. Molten rock from the plate rises toward the surface and forms a chain of volcanic islands, also called a volcanic island arc, behind the trench in the ocean.
Divergent Boundaries happen when two plates (oceanic or contental) begin to diverge, or move apart. Convergent Boundaries occur when two plates (again, oceanic or contential) begin to converge or move apart
When two oceanic plates or two plates both containing oceanic crust collide or converge, the convergent boundary will form a trench. The plate which has the higher density will plunge beneath the other plate forming a trench.
an earth quake happens when two plates meet
When two tectonic plates converge, a subduction zone can form where one plate is pushed beneath the other, creating deep oceanic trenches and volcanic arcs. Another possibility is a collision boundary, where the two plates collide and form mountain ranges due to intense pressure and folding of the Earth's crust.
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
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.
they over lap and cause mountains and hills Folded mountains are produced
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.