Which plate collisions would most likely result in a subduction zone?

Which plate collisions will produce subduction?

Subduction occurs when two plates collide at a convergent boundary, and one plate is driven beneath the other, back into the Earth’s interior.

What two types of collisions cause a subduction zone?

When an oceanic and a continental plate collide, eventually the oceanic plate is subducted under the continental plate due to the high density of the oceanic plate.

At which plate boundary type are you most likely to find a subduction zone?

Convergent Plate Boundaries—Subduction Zones.

Which of the following are results of a subduction zone?

These plates collide, slide past, and move apart from each other. Where they collide and one plate is thrust beneath another (a subduction zone), the most powerful earthquakes, tsunamis, volcanic eruptions, and landslides occur.

What happens at a subduction zone?

Where two tectonic plates meet at a subduction zone, one bends and slides underneath the other, curving down into the mantle. (The mantle is the hotter layer under the crust.) Tectonic plates can transport both continental crust and oceanic crust, or they may be made of only one kind of crust.

What happens when two plates collide at a subduction zone?

i) When 2 tectonic plates collide along a subduction zone, the heavier oceanic plate slides underneath the continental plate and forms a trench. ii) Subduction leads to volcanic activity because as one plate is subducted under another over a hotspot, the plate melts into magma.

What 2 things happen as a subducting plate sinks back into the earth?

What 2 things happen as a subducting plate sinks back into the earth? Earthquakes are common along the subduction zone, and fluids released by the subducting plate trigger volcanism in the overriding plate.

Which results from the collision of two continental plates?

With collision of the two continental plates, subduction ceases because neither of the continental plates will subduct beneath each other. The result is a collision between two continental blocks. During this collision, the continental crust is folded, stacked and thickened , and generally shortened.

How do subduction zones cause volcanoes?

At a subduction zone an oceanic crust is pushed under the continental crust. As the oceanic crust is pushed under the continental crust it is subjected to heat and pressure. The heat and pressure causes the crust to melt and become magma. … When the magma reaches the surface it creates a volcano.

What type of volcanoes are created in a subduction zone?

The volcanoes produced by subduction zone volcanism are typically stratovolcanoes. Incipient island arcs tend to be more basaltic in composition, whereas mature continental volcanic arcs tend to be more andesitic in composition.

How do subduction zones cause earthquakes?

At subduction zones, the oceanic plate is pushed down, or subducted, below the continental lithosphere. As the oceanic slab descends, earthquakes are generated within the slab and at the interface between the plates.

What type of volcanoes form at subduction zones?

Stratovolcanoes tend to form at subduction zones, or convergent plate margins, where an oceanic plate slides beneath a continental plate and contributes to the rise of magma to the surface.

What are examples of subduction zones?

An oceanic plate can descend beneath another oceanic plate – Japan, Indonesia, and the Aleutian Islands are examples of this type of subduction. Alternately, an oceanic plate can descend beneath a continental plate – South America, Central America, and the Cascade Volcanoes are an example of this type of subduction.

Where can you find collision zones?

These are often seen in old, eroding mountain ranges such as the Appalachians. Folded slate in the Green Mountains, Vermont. Actively colliding boundaries are the site of frequent earthquakes.

What type of plate is the collision zone?

Collision zones form when two continental plates move towards each other and collide. The land between the plates is forced upwards to form fold mountains, eg The Alps and Himalayas.

Which plate is represented by collision zones?

A collision zone occurs when tectonic plates meet at a convergent boundary both bearing continental lithosphere.

Which plate boundaries are represented by collision zones?

Convergent boundaries: where two plates are colliding.

Subduction zones occur when one or both of the tectonic plates are composed of oceanic crust.

What is the difference between a subduction zone and a collision zone?

In the collision zone the shallow thrust zone is not provided with fluid, and the zone is completely coupled. In the subduction zone the thrust zone is provided with fluid, and the lower plate moves with respect to the upper plate beneath the barriers. The upper plate is dragged through asperities by the lower plate.

How does a collision zone differ from a destructive plate boundary?

How does a collision zone differ from a destructive plate boundary? Collision zones differ from destructive plate boundaries due to the types of crust found in each. Collision zones have two continental plates, whereas destructive boundaries have one continental and one oceanic.

What happens at destructive plate boundaries?

At a destructive plate boundary (also called convergent boundaries) two plates move towards another. One plate is then pushed underneath the other. (It is the heavier plate that is forced beneath the lighter plate). The point at which one plate is forced beneath the other is called the subduction zone.

What do destructive plate boundaries cause?

Destructive plate margins

The plates move towards one another and this movement can cause earthquakes. As the plates collide, the oceanic plate is forced beneath the continental plate. This is known as subduction . This happens because the oceanic plate is denser (heavier) than the continental plate.

What features are found at destructive plate boundaries?

Large scale landforms at a destructive plate boundary include super volcanoes, such as the Campi Flegrei volcano in Italy – where the Eurasian plate and the African Atlantic plate are moving towards each other along the Mediterranean sea.