Geoscience Processes Review Game

Geoscience Processes Review Game

Assessment

Interactive Video

Science, Geography, History

6th - 8th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explores the concept of Pangaea, a supercontinent that existed over 240 million years ago. It discusses the theory of continental drift proposed by Alfred Wegener, which explains how continents moved to their current positions. The video introduces plate tectonics, describing how the Earth's crust is divided into tectonic plates that move and interact at boundaries. It explains three types of plate boundaries: convergent, divergent, and transform, and how these interactions shape the Earth's surface. The formation of the Himalayan Mountains through convergent boundaries is also highlighted.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What was the name of the supercontinent that existed over 240 million years ago?

Laurasia

Pangaea

Gondwana

Atlantis

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Who proposed the theory of continental drift?

Galileo Galilei

Charles Darwin

Alfred Wegener

Isaac Newton

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What evidence did Wegener use to support his theory of continental drift?

Same species of birds found worldwide

Similar climates across continents

Matching fossils and rock formations across continents

Identical languages spoken across continents

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the process called where the Earth's crust is broken into moving pieces?

Seafloor spreading

Erosion

Volcanic activity

Plate tectonics

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which layer of the Earth is directly below the crust?

Lithosphere

Mantle

Core

Asthenosphere

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of boundary occurs when two tectonic plates move towards each other?

Static

Transform

Convergent

Divergent

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which type of boundary is responsible for the creation of the Mid-Atlantic Ridge?

Transform

Convergent

Divergent

Subduction

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