Subduction Zones and Oceanic Crust

Subduction Zones and Oceanic Crust

Assessment

Interactive Video

Science, Geography, Other

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

Subduction zones are convergent plate boundaries where oceanic crust, which is denser and composed of basalt, collides with continental crust, which is lighter and composed of granite. The denser oceanic plate subducts beneath the continental plate, driven by mantle convection currents. This process leads to the formation of mountains, active volcanoes, and earthquakes, as well as deep-sea trenches. Subduction zones are characterized by significant volcanic and seismic activity, making them some of the most dynamic regions on Earth.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a subduction zone?

A type of static plate boundary

A type of convergent plate boundary

A type of transform plate boundary

A type of divergent plate boundary

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of rock primarily composes oceanic crust?

Granite

Limestone

Basalt

Sandstone

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which crust is denser, oceanic or continental?

Continental crust

Both are equally dense

Oceanic crust

Neither, they are both light

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of rock is continental crust primarily composed of?

Marble

Granite

Shale

Basalt

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens when oceanic and continental crusts collide?

Both crusts remain stationary

The oceanic crust subducts beneath the continental crust

The continental crust subducts beneath the oceanic crust

The oceanic crust rises above the continental crust

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What geological features are formed due to subduction?

Flat plains

Jagged mountains and volcanoes

Deserts

Coral reefs

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a common feature found where two plates meet in a subduction zone?

Rift valleys

Plateaus

Deep sea trenches

Mountain ranges

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