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Plate Tectonics
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Plate Tectonics
The place where some parts of the Crustal Plates are destroyed is known as:
obstructive plate boundary
constructive plate boundary
subductive plate boundary
destructive plate boundary
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Plate Tectonics
The sliding past of two Crustal Plates in opposite direction is known as:
Convergent Plate Movement
Divergent Plate Movement
Transform Plate Movement
Boundary Plate Movement
Author:
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Plate Tectonics
The magma cools to form
sea beds only
crustal rocks only
crustal rocks and sea floors
rocks to support land and water
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Plate Tectonics
When the collision of Oceanic and Continental Plates takes place, the Continental Plate is pushed towards the:
mantle
core
crust
ocean
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Plate Tectonics
Unlike convergent and divergent plate boundaries, there is no construction or destruction in:
constructive plate boundary
destructive plate boundary
active plate boundary
passive plate boundary
Author:
rikazzz
Comment
Plate Tectonics
The word ‘Tectonics’ comes from a Greek word:
tekton
tecutan
tecuashian
tectiron
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Plate Tectonics
The number of types of crustal plates is:
one
two
three
four
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Plate Tectonics
The Transform Plate Movement is seen in a state of America known as:
Mississippi
Alabama
Texas
California
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Plate Tectonics
The process of collision of two plates with different densities is known as:
Abduction
Subduction
Prediction
Production
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Plate Tectonics
The plates and the upper part of the mantle combine to form a layer known as:
atmosphere
troposphere
exosphere
lithosphere
Author:
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