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Structural Features of Earth Movement by rotsacreijav666666 is a document available to read on EtoBox.
Convection currents in the asthenosphere are the driving force behind plate tectonics, pushing the plates along at rates of about 1 to 4 inches per year. Tectonic plates can interact in three ways - converging toward each other, diverging away from each other, or transforming by sliding past one another. The type of geological activity that occurs at plate boundaries depends on how the plates are interacting and the composition of the margins.
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- rotsacreijav666666
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- EN