Geological Processes and Earth's History

Geological Processes and Earth's History

Assessment

Interactive Video

Science, Geography, History

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explores the changes in Earth since its origin, estimated to be over 4.5 billion years old. It discusses the DUS Cloud hypothesis for Earth's formation and the processes that led to its differentiation into layers. The video also covers the formation and drift of continents, highlighting the supercontinents Gondwana and Laurasia, and the eventual breakup of Pangia. It explains how natural forces like volcanic activity and erosion have continuously reshaped Earth's surface, providing evidence of these changes through fossils and geological formations.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the estimated age of the Earth according to geologists?

6.5 billion years

5.5 billion years

4.5 billion years

3.5 billion years

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which hypothesis is widely accepted for the formation of the solar system?

Big Bang Theory

Dus Cloud Hypothesis

Steady State Theory

String Theory

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary cause of Earth's internal heat?

Solar radiation

Heat from the sun

Friction from tectonic plates

Radioactive decay

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What process describes the reorganization of Earth's materials into layers?

Sedimentation

Differentiation

Erosion

Metamorphism

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What were the names of the supercontinents in the Southern and Northern Hemispheres?

Atlantis and Lemuria

Gondwana and Laurasia

Avalonia and Baltica

Pangaea and Eurasia

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What term describes the movement of continents over time?

Seafloor Spreading

Plate Tectonics

Subduction

Continental Drift

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do scientists deduce the movement of continents?

By analyzing fossil records

By measuring magnetic fields

By studying ocean currents

By observing weather patterns

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