
The Mantle convection theory
Authored by Iam Olam
Arts
2nd Grade
Used 2+ times

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10 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
The innermost layer of the Earth.
Mantle
Core
Crust
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
The thick middle layer of the Earth.
Mantle
Core
Crust
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
It is a large sections of the Earth's crust that move over the mantle.
Vocanoes
Plates
Earthquake
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Openings in Earth's crust that allow magma.
Mountain
Volcanoe
Volcanoes
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What role does density play at subduction zones in mantle convection?
The mantle behaves like a viscous fluid over long timescales, and the process of convection transfers heat efficiently from the deep Earth to the surface.
At subduction zones, dense, cold oceanic plates sink back into the mantle because they are heavier than the surrounding hotter, less dense mantle material.
Mantle convection is a driving force behind the movement of tectonic plates. The currents in the mantle cause plates to move, collide, and separate, resulting in earthquakes, volcanic activity, and mountain formation.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does the difference in density drive mantle convection?
In mantle convection, hot mantle material becomes less dense as it heats up, causing it to rise towards the Earth's surface. As it cools near the surface, it becomes denser and sinks back down.
The Earth's mantle is heated from below by the core, which causes the lower mantle material to become hot and less dense.
Mantle convection is a driving force behind the movement of tectonic plates. The currents in the mantle cause plates to move, collide, and separate, resulting in earthquakes, volcanic activity, and mountain formation.
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is mantle convection?
Mantle convection is a driving force behind plate tectonics. The convection currents in the mantle move tectonic plates, causing them to converge, diverge, and slide past each other at plate boundaries.
The primary sources of heat driving mantle convection are radioactive decay of elements like uranium, thorium, and potassium, as well as primordial heat left over from the formation of the Earth.
Mantle convection refers to the slow, circular movement of the Earth's mantle due to heat transfer. Hot material from deep within the Earth rises towards the surface, cools, and then sinks back down, creating convection currents that drive the movement of tectonic plates.
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