Earth's Magnetic Field and Reversals

Earth's Magnetic Field and Reversals

Assessment

Interactive Video

Science, Physics

9th - 12th Grade

Medium

Created by

Liam Anderson

Used 2+ times

FREE Resource

The video explores Earth's magnetic field, its reversals, and the potential link to plate tectonics. It explains the dynamo theory and how volcanic rocks help study past magnetic fields. The video also discusses the randomness of reversals and the role of heat flow between Earth's core and mantle. Finally, it touches on the sponsorship by Fabulous, an app for habit building.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary source of Earth's magnetic field?

The movement of iron in the outer core

The Earth's mantle

The Earth's crust

The Earth's atmosphere

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What theory explains the generation of Earth's magnetic field?

Plate tectonics theory

Dynamo theory

Quantum theory

Continental drift theory

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do scientists study ancient magnetic fields?

By studying ocean currents

By observing the moon

By examining volcanic rocks

By analyzing ancient trees

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What pattern do scientists observe in Earth's crust related to magnetic fields?

It is striped like a zebra

It is striped like a tiger

It is dotted like a leopard

It is plain with no patterns

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How often do magnetic field reversals occur on average?

Every few million years

Every few hundred thousand years

Every few thousand years

Every few billion years

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is one hypothesis for why magnetic field reversals occur?

Movements of tectonic plates

Shifts in ocean currents

Changes in the Earth's atmosphere

Variations in solar activity

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the challenge in linking plate tectonics to magnetic field reversals?

The lack of technology to measure magnetic fields

The absence of historical data

The unpredictability of volcanic eruptions

The unknown time it takes for a plate to descend through the mantle

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