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Plate Tectonics

By Michael Alan Prestwood

Sat 3 Jul 2021
Published 5 years ago.
Updated 3 months ago.
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By dating rocks and fossils scientists can document the movement of the continents over time. (Public domain image, United States Geological Survey.)

Plate Tectonics

Circa 260 Million BCE

By dating rocks and fossils scientists can document the movement of the continents over time. 

To confirm and refine this science, geologists study rocks, paleontologists study fossils, and anthropologists study human societies, cultures, and relics. The location and dating of rocks, fossils, and relics allow us to understand the distant past.

  • Cynognathus, circa 242 million BCE
  • Lystrosaurus, circa 250 million BCE
  • Glossopteris, circa 275 million BCE
  • Mesosaurus, circa 285 million BCE

— map / TST —

Michael Alan Prestwood
Author & Natural Philosopher
Prestwood writes on science-first philosophy, with particular attention to the convergence of disciplines. Drawing on his TST Framework, his work emphasizes rational inquiry grounded in empirical observation while engaging questions at the edges of established knowledge. With TouchstoneTruth positioned as a living touchstone, this work aims to contribute reliable, evolving analysis in an emerging AI era where the credibility of information is increasingly contested.
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