Mountain Formation Around the World

Mountain Formation Around the World

Assessment

Interactive Video

Science, Geography, Other

6th - 7th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explains the different types of mountains: folded, volcanic, and fault block. Folded mountains form at convergent boundaries where rock layers are pushed together, with examples like the Himalayas and the Appalachian Mountains. Volcanic mountains are created by eruptions, often found in the Ring of Fire, with examples like Mount Griggs and Mount Fuji. Fault block mountains form when the lithosphere breaks into normal faults, with examples like the Teton Mountains and the Sierra Nevadas. The video concludes with a call to subscribe for more educational content.

Read more

6 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are the primary processes through which mountains can form?

Sedimentation, folding, and weathering

Glaciation, erosion, and deposition

Erosion, sedimentation, and weathering

Folding, volcanism, and faulting

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where do many folded mountains typically form?

In the middle of tectonic plates

At convergent boundaries

At transform boundaries

At divergent boundaries

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which mountain range is an example of folded mountains?

The Pyrenees

The Himalayas

The Rockies

The Andes

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a characteristic feature of volcanic mountains?

They are created by the eruption of melted rock onto the Earth's surface

They are formed by the collision of tectonic plates

They are created by the folding of rock layers

They are formed by the erosion of sedimentary layers

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which area is known for having a high concentration of active volcanoes?

The Atlantic Ocean

The Arctic Circle

The Sahara Desert

The Ring of Fire

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do fault-block mountains form?

Through the collision of oceanic and continental plates

By the eruption of magma through the Earth's crust

When tension causes the lithosphere to break into normal faults

By the folding of sedimentary rock layers