Answer: C
Correct answer: Plate tectonics
Plate tectonics holds that the lithosphere - the crust together with the rigid uppermost mantle - is broken into about fifteen major plates that move a few centimetres a year over the ductile asthenosphere beneath. Almost all earthquakes, volcanoes and mountain ranges occur at their boundaries, of which there are three kinds: divergent, where plates separate and new crust forms, as at the Mid-Atlantic Ridge; convergent, where one plate is driven beneath another, producing trenches and volcanic arcs; and transform, where plates slide past each other, as along the San Andreas Fault. The theory grew out of Alfred Wegener’s continental drift, which he proposed in 1912 but could not explain a mechanism for. It was accepted only in the 1960s, once seafloor spreading and the magnetic striping of the ocean floor supplied one. Isostasy is the buoyant balance of crust on mantle; uniformitarianism is the principle that present processes explain past ones; and orogeny is mountain building, one consequence of tectonics rather than the theory itself.