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This type of heat transfer sees magma rise to the top of the mantle, cool, then sink, reheat, and rise again causing changes in Earth's surface.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This layer is solid, but capable of flow like hot asphalt or fudge.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This layer is located about 1,800 miles beneath the crust and is about 1,400 miles thick.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This layer is the very center of the Earth, is very hot and, and due to intense pressure, is solid.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This layer of the Earth is made up of large amounts of silicon and aluminum.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This is the thickest layer of the Earth making up 70% of the Earth’s mass.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
This increases as the depth of the Earth increases.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
The lithosphere moves in big chunks of land called ___________.
mantle
convection currents
temperature
outer core
crust
tectonic plates
mantle
inner core
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