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Plate Tectonics
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Plate Tectonics
The divergence is cause because of the:
convection current in the crust
convection current in the core
convection current in the mantle
blasts in the core
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Plate Tectonics
The Continental Plates are:
thinner than Oceanic Plates
thicker than Oceanic Plates
equal in thickness to Oceanic Plates
None of these
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rikazzz
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Plate Tectonics
The average temperature of mantle is:
1200°C
1500°C
2000°C
2400°C
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Plate Tectonics
The place where two crustal plates meet is called the:
tectonic
plate
convergent boundary
divergent boundary
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Plate Tectonics
The mantle is mainly:
solid
semi-solid
molten
gaseous
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rikazzz
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