Reading Comprehension — Passage 1
Questions 11–15 are based on the passage below.
The theory of plate tectonics, which holds that the Earth's outer shell is divided into moving plates, became accepted only in the 1960s, half a century after Alfred Wegener first proposed that continents drift. Wegener had assembled impressive evidence: the coastlines of South America and Africa fit together like puzzle pieces, and identical fossils and rock formations appear on continents now separated by oceans. His critics, however, pointed out that solid continents could not plough through the solid ocean floor.
The breakthrough came from the ocean floor itself. Mapping in the 1950s revealed enormous underwater mountain ranges, and magnetic surveys showed symmetrical stripes of rock on either side of them, recording reversals of the Earth's magnetic field. These stripes indicated that new crust was forming at the ridges and spreading outward. The continents, it turned out, did not plough through the ocean floor; they rode along with it.