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Continental- Continental Convergent

Authored by K Kirby

Geography

11th - 12th Grade

Used 1+ times

Continental- Continental Convergent
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6 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Name an example of a continental- continental plate boundary

North American and Caribbean Plate

North American and Eurasian Plate

Pacific and South American Plate

Eurasian and Indian Plate

2.

REORDER QUESTION

1 min • 1 pt

Reorder the following to show how the Himalayas formed

The sediments were crumpled and buckled up to form the Himalayas

The Himalayas are still rising by more than 1 cm per year as India continues to move northwards into Asia

The Tethys Ocean became narrower and was subducted under the Eurasian Plate

The Eurasian and Indian Plate moved towards each other

The sediments from the Tethys ocean were scaped off onto the Eurasian plate

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why is there very little or no subduction when two continental plates collide?

Because there is no friction

Because both plates are equally buoyant

Because one plate is more dense than the other

Because it s blocked by teh accretionary wedge

4.

OPEN ENDED QUESTION

3 mins • 1 pt

What type of earthquakes are found where two continental plates collide?

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5.

DROPDOWN QUESTION

1 min • 1 pt

The continental crust ​ (a)   thick in the Himalayas

75km
55km
7.5km
25km

6.

CATEGORIZE QUESTION

3 mins • 1 pt

Organize these options into the right categories

Groups:

(a) Continental -Continental

,

(b) Oceanic-Oceanic

,

(c) Continental-Oceanic

Shallow focus earthquakes

Media Image

No subduction

North American and Caribbean Plates

Fold mountains and ocean trenches

Earthquakes along fault lines

Indian and Eurasian Plates

Island Arcs

Mariana Trench

Media Image

Continental crust thickness variations

Pacific and South American Plates

Media Image

Fold mountains such as the Himalayas

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