Plate Tectonics

Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός “relating to manufacturing”) is a science hypothesis that portrays the hefty-scale movements of World’s lithosphere. The model extends the ideas of mainland float, advanced around the first decades of the 20th century. It was embraced by the geoscientific group following the ideas of seafloor spreading were improved in the late 1950s and early 1960s.

CI Plate Tectonics

CI Plate Tectonics

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