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Oceanic Oceanic Convergent Boundary

Authored by K Kirby

Geography

12th Grade

Used 1+ times

Oceanic Oceanic Convergent Boundary
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8 questions

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1.

OPEN ENDED QUESTION

3 mins • 1 pt

Name 2 oceanic plates that are moving towards each other

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2.

FILL IN THE BLANK QUESTION

1 min • 1 pt

The South American Plate is moving westwards due to sea floor spreading at the Mid Atlantic Ridge. Where it meets the Caribbean Plate, it descends (________) beneath it.

3.

DRAG AND DROP QUESTION

1 min • 1 pt

subduction causes low density ocean floor sediment to be ​ (a)   off the surface of the South American Plate and thrust onto the Caribbean Islands as ​ (b)   wedges, in a process called ​ (c)   . The line of subduction is marked by the deep sea Puerto Rico ​ (d)  

scraped
accretionary
obduction
Trench

4.

DROPDOWN QUESTION

1 min • 1 pt

As the ​ (a)   descends, it drags against the overlying plate, causing both to fracture and deform. This results in frequent ​ (b)   focus earthquakes that get deeper as the ocean plate descends further, defining a zone of earthquake foci known as a ​ (c)   zone.

shallow
superficial
surface
minor
Benioff
Obduction
Milankovitch
South American Plate
Caribbean
less dense

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the name of the magma produced at an oceanic-oceanic convergent boundary?

basalmic

andesitic

rhyolitic

basaltic

6.

OPEN ENDED QUESTION

3 mins • 1 pt

What happens to the melting point of the plate as it descends into the mantle?

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7.

DRAG AND DROP QUESTION

1 min • 1 pt

Andesitic magma is less dense than the surrounding material, and can have a temperature of ​ (a)   . It is ​ (b)   , trapping gases as it rises. The water and gases in andesitic magma account for the ​ (c)   activity of andesitic volcanoes, which typically lie ​ (d)   for many hundreds or thousands of years. These volcanoes typically produce ash and ​ (e)   flows, as well as small amounts of andesitic lava.

1000oC
viscous
dormant
pyroclastic
explosive

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