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Convection in the Mantle

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Presentation on theme: "Convection in the Mantle"— Presentation transcript:

1 Convection in the Mantle
Khan Academy Convection in the Mantle Video

2 Remember the three types of heat transfer?
Radiation Conduction Convection

3 Remember density? Amount of mass in a given volume Decreases as a substance is heated because molecules move faster, bounce around more and take up more space.... Increases as a substance cools....

4 Changes in fluid density
CONVECTION Flow that transfers heat within a fluid caused by Heating & Cooling of a fluid Changes in fluid density gravity

5 CONVECTION CURRENT When a fluid is heated its density decreases
...heat goes higher ...Hot air, hot water, hot rock rise When a fluid cools, its density increases ....Cold creeps lower ....Cold air, cold water, cool rock sink

6 Mantle rocks near Earth’s hot core are heated and become less dense than cooler, upper mantle rocks. These hotter rocks rise & the cooler rocks sink, creating slow convection currents, or convection cells.

7 Convection cells in the mantle – in the asthenosphere - cause the lithosphere to move.

8 Ridge-push Hypothesis
Spooner, Alecia, Geology for Dummies, Wiley Publishing, 2011

9 Slab-Pull hypothesis Spooner, Alecia, Geology for Dummies, Wiley Publishing, 2011

10 Magma Plumes hypothesis
Spooner, Alecia, Geoplogy for Dummies, Wiley Publishing, 2011


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