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What is the edge between two tectonic plates?

What is the edge between two tectonic plates?

When two plates come together, it is known as a convergent boundary. The impact of the colliding plates can cause the edges of one or both plates to buckle up into a mountain ranges or one of the plates may bend down into a deep seafloor trench.

Is that plate border divergent convergent or transform?

Divergent boundaries — where new crust is generated as the plates pull away from each other. Convergent boundaries — where crust is destroyed as one plate dives under another. Transform boundaries — where crust is neither produced nor destroyed as the plates slide horizontally past each other.

What plate boundary is formed by the collision of two plates?

Convergent boundaries
Convergent boundaries: where two plates are colliding. Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust. The denser plate is subducted underneath the less dense plate. The plate being forced under is eventually melted and destroyed.

Which plate boundaries are convergent?

Convergent boundaries are areas where plates move toward each other and collide….Orogenic belts

  • The European Alps.
  • The Carpathians.
  • The Pyrenees.
  • The Apennines.
  • The Dinarides.
  • The North African mountain belts such as the Atlas Mountains.
  • The Karst Plateau of the Balkan Peninsula.
  • The Caucasus.

When two of Earth’s plates pull apart it is called?

Divergent or constructive plate boundaries. The plates diverge and this causes the construction of new rock. It happens when two tectonic plates pull apart and rock from the mantle rises up through the opening to form new surface rock when it cools.

What happens when two tectonic plates collide with each other?

If two tectonic plates collide, they form a convergent plate boundary. Usually, one of the converging plates will move beneath the other, a process known as subduction. The new magma (molten rock) rises and may erupt violently to form volcanoes, often building arcs of islands along the convergent boundary.

How does it look like of convergent?

Usually the plate with the greatest density slips on top of the plate with the lower density. Often the convergence of plates results in the formation of volcanos or other natural landforms such as mountains due to cracks in the the crust and land being pushed upwards.

Which is the best example of a convergent plate boundary?

Answer: The Washington-Oregon coastline of the United States is an example of this type of convergent plate boundary. Here the Juan de Fuca oceanic plate is subducting beneath the westward-moving North American continental plate. The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate.

How are divergent and convergent plate boundaries different?

*If both plates are continental crust, the plates will crumple up as they collide, forming a high mountain range,like the Himalayas. *Divergent Plate Boundaries is when two plates move away from each other and magma comes up to the surface to fill the open void, creating the new crust. Convergent Plates are exactly the opposite of Divergent Plates.

What happens when two plates push into each other?

This happens at a convergent boundary. A convergent boundary is a boundary where two separate plates are pushing into each other. There are two kinds of surface features that are associated with a convergent boundary. The first is a deep ocean trench that forms a line of the two colliding plates.

Which is the boundary where two separate plates meet?

Introduction to Plate Boundaries. The boundary where two separate plates meet is where all the action occurs and is called a fault. A fault is a crack in the earth’s crust resulting from the movement of the two plates.

When does a convergent boundary cause an earthquake?

Convergent boundaries form strong earthquakes, as well as volcanic mountains or islands, when the sinking oceanic plate melts. The third type is transform boundaries, or boundaries where plates slide past each other, forming strong earthquakes.