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Magma and Plate Tectonics Concepts

Magma and Plate Tectonics Concepts

Assessment

Interactive Video

Science

9th - 10th Grade

Practice Problem

Hard

Created by

Patricia Brown

FREE Resource

Dr. Christopher White explains the formation of igneous rocks, focusing on magma generation at divergent plate boundaries. He describes the process of decompression melting and the structure of oceanic lithosphere, including mantle peridotites, gabbros, sheeted dike complexes, and pillow basalts. The video also covers continental divergent boundaries, where mafic magma interacts with continental crust, leading to the formation of felsic and intermediate magmas.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What percentage of all magma is generated at divergent plate boundaries?

30%

60%

90%

100%

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary role of the asthenosphere in oceanic divergent plate boundaries?

To cool down the crust

To rise and fill the space created by thinning crust

To create earthquakes

To form mountains

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to mantle peridotite when it is brought to a lower pressure region?

It cools down

It solidifies

It remains unchanged

It melts through decompression

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which layer in the oceanic lithosphere is formed by vertical sheets of basalt?

Mantle rocks

Sheeted dike complex

Pillowed basalts

Gabbros

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the result of magma reaching the sea floor in oceanic divergent plate boundaries?

Cooling of the ocean

Formation of pillowed basalts

Creation of earthquakes

Formation of mountains

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the typical temperature of mafic magma?

500°C

800°C

1200°C

1500°C

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens when mafic magma interacts with continental crust?

It forms mountains

It cools down and solidifies

It melts the continental crust

It causes earthquakes

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