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Convection Currents and the Mantle
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The Heat of the Earth Earth’s outer core is nearly as hot as the surface of the sun
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Heat Transfer The movement of energy from a warmer object to a cooler object
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Three Types of Heat Transfer Radiation Conduction Convection
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Radiation The transfer of energy through empty space
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Radiation Heat transfer by radiation takes place with no direct contact between a heat source and an object
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Conduction Heat transfer by direct contact of particles of matter
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convection Heat transfer by the movement of a heated fluid
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How Convection Works During convection heated particles of fluid begin to flow, transferring heat energy from one part of the fluid to another
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What Causes Convection Heat transfer by convection is caused by differences of temperature and density within the fluid
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Density A measure of how much mass there is in a volume of a substance
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Convection Current the flow that transfers heart within a fluid
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The heating and cooling of the fluid, changes in the fluid’s density, and the force of gravity combine to set convection currents in motion
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Convection in Earth’s Mantle The core creates convection currents that flow through the asthenosphere
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Convection in the Mantle At the top of the asthensophere the hot material spreads out and pushes the cooler material out of the way
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Convection in the Mantle The cooler material sinks back into the asthenosphere
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