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🌍 Plate Boundaries — Tectonics Lab

🌍 Plate Boundaries — Tectonics Lab

Four boundary types, four very different landscapes: spreading ridges, subduction volcanoes, Himalaya-scale collisions and stick-slip transform faults — with earthquakes and mantle convection driving it all.

earthquakes: 0
📖 Key facts

Earth's lithosphere is broken into ~15 major plates riding on the slowly flowing mantle (a few cm/yr — fingernail speed).GPS confirms the motions. Three boundary types do almost all the work: divergent (plates apart — new crust, shallow quakes, ridges & rifts), convergent (one plate sinks or two crumple — trenches, volcanic arcs, the deepest earthquakes, the tallest mountains), and transform (plates sliding past — shallow, violent strike-slip quakes like San Francisco 1906).

The magnetic stripes in the divergent view are real: as lava cools through the Curie point it freezes the Earth's magnetic field direction — flipped many times in history — giving stripe pairs that proved seafloor spreading in the 1960s. Ring of Fire = subduction zones around the Pacific.

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