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Volcanic Formation Concepts

Volcanic Formation Concepts

Assessment

Interactive Video

Science, Geography, Other

9th - 12th Grade

Practice Problem

Hard

Created by

Patricia Brown

FREE Resource

The video explores volcanic processes, focusing on magma intrusions and extrusions. It explains different types of intrusions like sills, dikes, and batholiths, and how they form and become exposed through erosion. The video also covers volcanic landforms, such as cones and lava plateaus, and distinguishes between intrusive and extrusive rocks. Examples of extrusive rocks, like lava flows and domes, are provided. The session concludes with a preview of the next topic on igneous rocks.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are plutons in the context of volcanic formations?

Large magma chambers that solidify underground

Small volcanic cones

Eroded volcanic necks

Lava flows on the surface

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which type of magma intrusion is characterized by horizontal layers?

Lava domes

Batholiths

Sills

Dikes

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following is NOT a type of magma intrusion?

Sill

Dike

Lava flow

Batholith

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary difference between intrusive and extrusive rocks?

Intrusive rocks are always visible, extrusive rocks are not

Intrusive rocks form on the surface, extrusive rocks form underground

Intrusive rocks are made of lava, extrusive rocks are made of magma

Intrusive rocks solidify underground, extrusive rocks solidify on the surface

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What geological process can expose intrusive rocks?

Erosion and uplift

Earthquakes

Lava flows

Volcanic eruptions

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following is an example of a magma extrusion?

Batholiths

Lava plateaus

Dikes

Sills

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do lava domes typically form?

By the erosion of volcanic cones

By the accumulation of pyroclastic material

Through the uplift of batholiths

Through the solidification of magma in a caldera

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