Earth's outer shell is broken into huge plates that move a few centimetres a year, about as fast as fingernails grow. Where they part, new ocean floor forms; where they collide, old floor sinks back into the mantle and mountains rise. This slow movement, plate tectonics, also drives most earthquakes and volcanoes.
The idea that continents move goes back to Alfred Wegener in 1912, but geologists accepted it only in the 1960s, when surveys of the ocean floor showed new crust forming along mid-ocean ridges and spreading away on both sides. Old ocean floor sinks back into the mantle at subduction zones, where one plate dives beneath another. That is why the oldest large areas of ocean floor are only about 180 to 200 million years old, while some continental rocks are about 4 billion years old. Turkey shows the process at work: most of the country sits on the small Anatolian plate, whose edges include the North and East Anatolian Faults. The 1999 İzmit earthquake struck on the first, and the 2023 Turkey–Syria earthquakes on the second.


