Ridge Push Explained at Paul Harlan blog

Ridge Push Explained. As the lithosphere formed at divergent plate margins is hot, and less dense than the surrounding area it rises to form oceanic ridges. As it cools it becomes denser. In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of. The magma cools to form new plate material. In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of an ocean ridge where magma is rising.

Plate Tectonics by Timmy shea
from www.haikudeck.com

In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of an ocean ridge where magma is rising. As the lithosphere formed at divergent plate margins is hot, and less dense than the surrounding area it rises to form oceanic ridges. The magma cools to form new plate material. In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of. As it cools it becomes denser.

Plate Tectonics by Timmy shea

Ridge Push Explained In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of. As it cools it becomes denser. In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of an ocean ridge where magma is rising. As the lithosphere formed at divergent plate margins is hot, and less dense than the surrounding area it rises to form oceanic ridges. The magma cools to form new plate material. In this model, plates move through a combination of pull from the weight of the subducting edge of the plates, and through the outward pushing of.

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