Plate Tectonics : Subduction Zones. When two oceanic plates collide, the younger of the two plates, because it is less dense,* will ride over the edge of the older plate. *[Oceanic plates grow more dense as they cool and move further away from the Mid-Ocean Ridge]. (Image: Keith-Wiess Geological Laboratories; Rice University) The older, heavier plate bends and plunges steeply through the athenosphere, and descending into the earth, it forms a trench that can be as much as 70 miles wide, more than a thousand miles long, and several miles deep. The Marianas Trench, where the enormous Pacific Plate is descending under the leading edge of the Eurasian Plate, is the deepest sea floor in the world.
It curves northward from near the island of Guam and its bottom lies close to 36,000 feet below the surface of the Pacific Ocean. Trench Flipping If the descending oceanic plate is carrying a continent, the less dense continental material cannot sink, so it dives into the trench behind the leading oceanic crust until it gets stuck. Can Catastrophic Plate Tectonics Explain Flood Geology. What Is Plate Tectonics? The earth’s thin rocky outer layer (3–45 mi [5–70 km] thick) is called “the crust.” On the continents it consists of sedimentary rock layers—some containing fossils and some folded and contorted—together with an underlying crystalline rocky basement of granites and metamorphosed sedimentary rocks.
In places, the crystalline rocks are exposed at the earth’s surface, usually as a result of erosion. Beneath the crust is what geologists call the mantle, which consists of dense, warm-to-hot (but solid) rock that extends to a depth of 1,800 mi (2,900 km). Below the mantle lies the earth’s core, composed mostly of iron. All but the innermost part of the core is molten (see Figure 1). Investigations of the earth’s surface have revealed that it has been divided globally by past geologic processes into what today is a mosaic of rigid blocks called “plates.” Figure 1. Compressional deformation occurs where two plates move toward one another. History of Plate Tectonics. Pangaea & Plate Tectonics. HamerTech - Plate Tectonics. Geography Site: Plate Tectonics. Continental Drift and Plate Tectonics Continental Drift As far back as 1620, Francis Bacon spotted that the west coast of Africa and the east coast of South America looked as if they would fit together, like pieces of a jigsaw puzzle.
Between then and 1912 other people identified further similarities between other continental coastlines, but it was only in 1912 that Alfred Wegener (left) published a theory to explain why the Earth looked like a huge jigsaw puzzle. He suggested that a very long time ago all the land that covered the Earth had been joined together into one huge continent. He named this landmass, Pangaea, and suggested that millions of years ago this supercontinent had somehow broken up. The different parts had then drifted into the present day positions.His evidence for this was drawn for several sources, covering geology, biology, geography and other sciences. Other discoveries added to his list of evidence. The origins of Plate Tectonics Plate Tectonics 1. 2. 3. 4. 5. 6. 7.