Why Do Tectonic Plates Move Relative With One Another at Ryder Rhodes blog

Why Do Tectonic Plates Move Relative With One Another. Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different rates, from two to 15 centimeters (one to six inches) per year. Active margins are places where the oceanic and continental lithospheric tectonic plates meet and move relative to each other, such as the western coasts of north and south america. Plate tectonics involves the movements of earth’s lithospheric plates relative to one another over the planet’s weak asthenosphere. Due to the convection in the lithosphere and asthenosphere, the plates move relative to one other at different rates, between one to six inches per year. Convergent, where plates move into one another; Divergent, where plates move apart; The movement of the plates creates three types of tectonic boundaries:

Plate Tectonics ,Plate Boundaries and Hotspot Explanation
from geologyscience.com

Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different rates, from two to 15 centimeters (one to six inches) per year. Plate tectonics involves the movements of earth’s lithospheric plates relative to one another over the planet’s weak asthenosphere. Convergent, where plates move into one another; The movement of the plates creates three types of tectonic boundaries: Divergent, where plates move apart; Due to the convection in the lithosphere and asthenosphere, the plates move relative to one other at different rates, between one to six inches per year. Active margins are places where the oceanic and continental lithospheric tectonic plates meet and move relative to each other, such as the western coasts of north and south america.

Plate Tectonics ,Plate Boundaries and Hotspot Explanation

Why Do Tectonic Plates Move Relative With One Another Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different rates, from two to 15 centimeters (one to six inches) per year. Due to the convection in the lithosphere and asthenosphere, the plates move relative to one other at different rates, between one to six inches per year. Active margins are places where the oceanic and continental lithospheric tectonic plates meet and move relative to each other, such as the western coasts of north and south america. Convergent, where plates move into one another; Due to the convection of the asthenosphere and lithosphere, the plates move relative to each other at different rates, from two to 15 centimeters (one to six inches) per year. The movement of the plates creates three types of tectonic boundaries: Divergent, where plates move apart; Plate tectonics involves the movements of earth’s lithospheric plates relative to one another over the planet’s weak asthenosphere.

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