
Continental- Continental Convergent
Authored by K Kirby
Geography
11th - 12th Grade
Used 1+ times

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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
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
No subduction
North American and Caribbean Plates
Fold mountains and ocean trenches
Earthquakes along fault lines
Indian and Eurasian Plates
Island Arcs
Mariana Trench
Continental crust thickness variations
Pacific and South American Plates
Fold mountains such as the Himalayas
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