In 1915, Alfred Wegener proposed his continental drift theory. He said that thecontinents floated atop the mantle, a heavier, denser layer of rocks deep within theearth. Wegener predicted that heat rising within the hot mantle created currents ofpartially melted rocks that could move the continents around the earth’s surface. Likemany revolutionary theories, Wegener’s was not initially accepted by scientists. All BUTONE of the research scenarios below supports Wegener's continental drift theory andalso supports the 1965 theory of plate tectonics.
In the 1950's and 1960's, marine geologists used data from echo sounders tomap ocean ridges in the North Atlantic and the Pacific. They noticed that theseridges stretched on for thousands of kilometers in long, continuous mountainchains that wound around the Earth’s surface, almost like the stitches on abaseball. The scientists also observed that the crest of the ridges had atopography that closely resembled volcanic rift zones on land. This evidence ledearly marine geologists to deduce that the mid-ocean ridges were formed byseafloor volcanoes.
Henry Hess discovered that as the ocean crust spreads and cools over millions ofyears, it becomes denser and eventually sinks down into oceanic trenches, orsubduction zones, a long way from where it forms at the mid-ocean ridge crest.As ocean crust descends toward the hot mantle, it melts and becomes recycledinto the mantle.
In the late 1960's, data revealed an alternating striped pattern of seafloor rocks.Rocks that formed when Earth’s magnetic field was in one position alternatedwith rocks that formed when the field was reversed. The stripes ran parallel tothe mid-ocean ridges and extended out hundreds of miles on either side of them.The seafloor’s permanent magnetic signatures showed that new ocean crust wascreated at the ridge crests and then spread outward in both directions.
In the 1960's, Nicholas Steno studied the relative positions of sedimentary rocksand found that solid particles settle from a fluid according to their relativeweight or size. The largest, or heaviest, settle first, and the smallest, or lightest,settle last. Slight changes in particle size or composition result in the formationof layers in the rock. He theorized that in any sequence of layered rocks, a givenbed must be older than any bed on top of it.