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Topic: Plate tectonics

Plate tectonics is the theory that explains the large-scale motion of the Earth's surface, where the Earth's outermost rigid layer is divided into pieces called tectonic plates that move and interact with each other, driving processes like earthquakes, volcanoes, and continental drift.

More on: Plate tectonics

The podcast episodes cover various aspects of plate tectonics and its impacts on our understanding of the Earth's geology and the processes that shape the planet.

For example, the discovery of the Mid-Atlantic Ridge by Marie Tharp, as discussed in "The deepest spot in the ocean", provided evidence for the theory of plate tectonics and continental drift, which revolutionized our understanding of Earth's geology.

Similarly, the role of plate tectonics in influencing the interior dynamics, heat transfer, and magnetic field generation of planets, as discussed in "264 | Sabine Stanley on What's Inside Planets", is another key aspect of the episodes.

The "SYMHC Classics: Orphan Tsunami" episode also highlights how the Cascadia subduction zone, a fault line resulting from plate tectonics, was the source of the catastrophic 1700 earthquake studied.

Finally, the "The tallest mountains on Earth are ... underground?" episode explores how the theory of plate tectonics may help explain the discovery of massive underground structures in Antarctica, potentially shedding light on critical processes that sustain life on our planet.

All Episodes