PLATE TECTONICS - GS146
Tuesday, Thursday 11:30 am - 1:00 pm
Room 3540 CC Little Building
Plate tectonic theory, which developed from the hypothesis that continents on opposite sides of the Atlantic Ocean had drifted apart, is one of the most revolutionary concepts developed in all of science during the last century. As with any great theory, it has developed geologists understand considerably more than its original intent, which was to explain the obvious puzzle-like fit between continents on opposite sides of the Atlantic Ocean. Development of the theory has progressed to the extent that it allows geologists to better understand earthquakes, volcanic activity, the origin of rocks and mineral deposits, mountain building, the distribution of fossil remains, the origin of features on the ocean floor, and much more.
There are only few aspects of the broad spectrum of geological phenomena that are not linked or explained in some way by this theory.