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When two continental plates converge, they can create mountain ranges due to the intense pressure and collision between the plates. This process, known as continental collision, leads to the folding and uplift of the Earth's crust. Examples of mountain ranges formed by this process include the Himalayas, which were created by the collision of the Indian and Eurasian plates. Additionally, seismic activity is common in these regions due to the stress and strain on the crust.
What else can I help you with?
Name the two types of lithospheric plates?
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
What type of geologic feature will form two continental plates collide ( Explain)?
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
What layer of the earth makes up the continental plates?
The continental lithosphere.
What are the tectonic plates large pieces of?
lithosphere
Which types of lithosphere are colliding with continent collisions?
In continent-continent collisions, the primary types of lithosphere involved are continental crusts. These collisions occur when two continental plates converge, leading to the formation of mountain ranges, such as the Himalayas, as neither plate is subducted due to their relatively similar densities. Additionally, oceanic lithosphere may also play a role in these tectonic interactions when it subducts beneath continental crust before the collision occurs, but the direct collision involves primarily continental lithosphere.
Name the two types of lithospheric plates?
There are two types of lithosphere: the oceanic lithosphere and the continental lithosphere. The oceanic lithosphere exists in the ocean basins while the continental lithosphere exists in the continental crust.
Is the lithosphere located in the plates why not?
Yes, the tectonic plates-both continental and oceanic- are part of the lithosphere.
What type of geologic feature will form two continental plates collide ( Explain)?
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
What layer of the earth makes up the continental plates?
The continental lithosphere.
How non-volcanic mountains are created by plate tectonics?
Non-volcanic mountains are caused when continental plates converge.
What are the two lithosphere plates called?
Continental and oceanic
If two continental plates converge a subduction zone forms?
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.
How do the mountains that form along an oceanic-oceanic convergent boundary differ from those associated with an oceanic continental convergent boundary?
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.
What are the tectonic plates large pieces of?
lithosphere
Which types of lithosphere are colliding with continent collisions?
In continent-continent collisions, the primary types of lithosphere involved are continental crusts. These collisions occur when two continental plates converge, leading to the formation of mountain ranges, such as the Himalayas, as neither plate is subducted due to their relatively similar densities. Additionally, oceanic lithosphere may also play a role in these tectonic interactions when it subducts beneath continental crust before the collision occurs, but the direct collision involves primarily continental lithosphere.
How is continental lithosphere different from oceanic lithosphere?
Continental plates are thicker and less dense. Continental plates are mainly granitic in composition. Oceanic plates are mainly basaltic in composition. The rock of continental plates is on average, much older than the rock of the oceanic plates. The oceanic plate underlies the oceans, and the continental plate makes up the land masses. Continental plates do not subduct at convergent plate boundaries.
Why does oceanic lithosphere sink beneath convergent lithosphere at convergent boundaries?
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
