Continental Drift and Marie Tharp's Contributions

Continental Drift and Marie Tharp's Contributions

Assessment

Interactive Video

Science, Geography, History

9th - 12th Grade

Hard

Created by

Emma Peterson

FREE Resource

In 1912, Alfred Wegener proposed the theory of continental drift, suggesting that continents were once a single landmass called Pangea. Initially dismissed, the theory gained support through the work of Marie Tharp, who mapped the ocean floor and discovered rift-valleys, providing evidence for the theory. Despite skepticism, her findings were validated by Jacques Cousteau's expedition, leading to a paradigm shift in earth sciences and the development of plate tectonics.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Who proposed the theory of continental drift in 1912?

Alfred Wegener

Bruce Heezen

Jacques Cousteau

Marie Tharp

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What was the name of the single landmass proposed by Wegener?

Pangea

Laurasia

Atlantis

Gondwana

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What method did Bruce Heezen's team use to collect depth data?

Sonar mapping

Seismic reflection

Echo sounding

Satellite imaging

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why was Marie Tharp not allowed to join the early ocean expeditions?

Health concerns

Insufficient qualifications

Fear of bad luck at sea

Lack of funding

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What did Tharp's maps reveal about the ocean floor?

It was covered in coral reefs

It had a complex geography of crevices and valleys

It was flat and featureless

It was mostly sandy plains

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What did Tharp's discovery of rift valleys support?

The presence of deep-sea trenches

Wegener's continental drift theory

The existence of underwater volcanoes

The theory of plate tectonics

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What did Howard Foster's earthquake data reveal?

Earthquakes were decreasing in frequency

Earthquakes occurred along mid-oceanic ridges

Earthquakes were random

Earthquakes were unrelated to oceanic features

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