Pillow Lava, Dikes, Gabbro, and Peridotite

Pillow Lava, Dikes, Gabbro, and Peridotite

Assessment

Interactive Video

Engineering, Geography, Science, Chemistry

11th Grade - University

Hard

Created by

Quizizz Content

FREE Resource

The video tutorial explores the structure and formation of oceanic crust, starting with sediment layers and moving to the formation of pillow lava at mid-ocean ridges. It explains the role of sheeted dykes as magma conduits and the formation of gabbro. The tutorial also covers layered peridotite and the process of magma differentiation. Finally, it discusses ophiolites, their formation, and geological significance, using the Somali Ophiolite as a reference point for seismic studies.

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7 questions

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1.

OPEN ENDED QUESTION

3 mins • 1 pt

What is the process by which pillow lavas are formed?

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2.

OPEN ENDED QUESTION

3 mins • 1 pt

Describe the characteristics of basaltic rocks.

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3.

OPEN ENDED QUESTION

3 mins • 1 pt

What are sheeted dikes and how are they formed?

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4.

OPEN ENDED QUESTION

3 mins • 1 pt

Explain the significance of the gabbro layer in oceanic crust.

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5.

OPEN ENDED QUESTION

3 mins • 1 pt

How does the process of differentiation affect magma composition?

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6.

OPEN ENDED QUESTION

3 mins • 1 pt

What is the role of olivine in the composition of oceanic crust?

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7.

OPEN ENDED QUESTION

3 mins • 1 pt

What is an ophiolite and where can it be found?

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