🌍 Plate Boundaries β€” Tectonics Lab

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

earthquakes: 0
πŸ“– Key facts

Earth's lithosphere is broken into ~15 major plates riding on the slowly flowing mantle (a few cm/yr β€” fingernail speed).GPS confirms the motions. Three boundary types do almost all the work: divergent (plates apart β€” new crust, shallow quakes, ridges & rifts), convergent (one plate sinks or two crumple β€” trenches, volcanic arcs, the deepest earthquakes, the tallest mountains), and transform (plates sliding past β€” 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 β€” flipped many times in history β€” giving stripe pairs that proved seafloor spreading in the 1960s. Ring of Fire = subduction zones around the Pacific.