sink ago into EarthWhen temperature differences exist, warm liquids rise and cold liquids sink. This create convection currents. Convection currents transfer warmth through the fluidity of water, air, or even hot magma. Convection currents build when boil fluids expand. This fluids become less dense. The decrease in density reasons the liquid to increase away from the original warm source. Together the liquid rises, cooler fluid is pulled toward the heat resource and replace instead instead the warm fluid. This liquid is then heated. The rises, and the process begins again. Convection currents develop a circular present that just ceases once the warmth is evenly transferred throughout the fluid.

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