Natural Disasters and Plate Boundaries

Natural Disasters and Plate Boundaries

Assessment

Interactive Video

Science, Geography, Physics

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explores different types of tectonic plate boundaries: constructive, destructive, collision, and conservative. Constructive boundaries, where plates move apart, often result in volcanic activity and mild earthquakes. Destructive boundaries involve subduction, leading to powerful earthquakes and volcanic eruptions. Collision boundaries form mountains like the Himalayas, with earthquakes but no volcanic activity. Conservative boundaries, where plates slide past each other, cause earthquakes but no volcanoes. The video concludes with a call to action for viewers to engage with the content.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is another name for plate boundaries?

Plate edges

Plate cores

Plate margins

Plate centers

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where are constructive plate boundaries most commonly found?

On land

At the bottom of the sea

In mountain ranges

In deserts

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of natural disaster is common at constructive boundaries?

Tsunamis

Hurricanes

Tornadoes

Volcanic eruptions

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens during subduction at destructive boundaries?

Continental plates rise

Plates slide past each other

Oceanic plates sink beneath continental plates

Plates move apart

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What causes powerful earthquakes at destructive boundaries?

Volcanic eruptions

Plates getting stuck and then jolting upwards

Plates sliding past each other

Plates moving apart

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is formed at collision boundaries?

Volcanoes

Oceans

Valleys

Mountains

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why don't volcanic eruptions occur at collision boundaries?

The plates are moving apart

The plates are too dense

The plates are sliding past each other

There is no magma rising from beneath

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