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This increases as the depth of the Earth increases.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This layer is the very center of the Earth, is very hot and, and due to intense pressure, is solid.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This layer is solid, but capable of flow like hot asphalt or fudge.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This is comprised of the crust and upper layer of the mantle.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
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.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This layer is located about 1,800 miles beneath the crust and is about 1,400 miles thick.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This layer of the Earth is made up of large amounts of silicon and aluminum.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
This is the thinnest layer of the Earth that ranges from only 2 miles in some areas of the ocean floor to 75 miles deep under mountains.
crust
temperature
lithosphere
outer core
mantle
inner core
convection currents
crust
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