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Convection and the Mantle
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Convection and the Mantle
There are 3 main types of heat transfer: radiation, conduction, convection
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Heat Transfer - Radiation
Radiation – transfer of energy through empty space, has no direct contact between the heat source and an object (Ex: sunlight warming Earth’s surface)
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Heat Transfer - Conduction
Conduction – heat transfer by direct contact of particles of matter (Ex: metal spoon heating up in a pot of hot soup)
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Heat Transfer - Convection
Convection – transfer of heat by the movement of a heated fluid (includes liquids and gases); Heat transfer is caused by differences in temperature and density within a fluid (Ex: Water on a stove – water heats at the bottom of the pan, becomes less dense and rises; away from the heat source the water cools, becomes more dense and sinks; the process begins again) This is a Convection Current, or flow that transfers heat. Density – measure of how much mass there is in a volume of a substance
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Convection and Density
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Convection Convection Currents
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COMPLETE AND PUT THE NEXT GRAPHIC ORGANIZER IN YOUR NOTEBOOK!
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Convection Currents in the Mantle
The heat source is the Earth’s core and from the mantle itself. These currents have been acting like a conveyor belt moving the lithosphere above for the past four billion years
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Convection Currents, A to D
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Convection Currents
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