Plate Tectonics

Have you ever looked at a map of the earth and thought that the continents could be fit together like a jigsaw puzzle? German scientist Alfred Wegner thought this in 1912 and from this simple observation developed the basis of the theory of Plate Tectonics. During the 1950's and 1960's scientists applied the theory and eventually by 1968 most of the earth's geologic activity was incorporated into the New Global Tectonics theory or more commonly Plate Tectonics.

The rigid lithosphere is suspended on a fluid layer of mostly molten rock known as the asthenosphere.  On this fluid layer, the continually expanding plates drift across the earth's surface at a rate of 3 inches (75 mm) per year and over millions of years changing the face of the earth.

Ocean crust continually produced in places called mid-ocean ridges. These submarine mountain ranges of volcanic origin are formed at the plate boundary. The excess plate material instead of changing the size of the earth's surface is consumed elsewhere. The oceanic plate material submerges under the crust of the continental plate in a process known as subducion.

At the point of subduction there is a tremendous amount of friction. The two plates are pushing against each other, and the subducted plate forces its way through the upper mantel. When the subducted material reaches a point approximately 60 miles (97 km) under the earth's crust it is melted by the asthenosphere, forming magma. The magma, which is made up of less dense rocks, rises to the surface through cracks and crevasses forming reservoirs near the crust. Eventually the magma reaches a Hot Spot where it is pushed above the crust in the form of a volcano. The process of Subduction has created volcanoes including the Galapagos Islands, the Philippine Islands and Mount St. Helen's.