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The Continental Drift Hypothesis and Plate Tectonic Theory - The initial ideas of the continental drift hypothesis led to the development of plate tectonic theory. English Language Learners Definition of continental drift technical.

Continental Drift Theory Definition Live Science

The very slow movement of the continents on the surface of the Earth See the full definition for continental drift in the English.

Continental drift theory definition. Set forth in 1912 by Alfred Wegener a geophysicist and meteorologist continental drift also explained why look-alike animal and plant fossils and similar rock formations are found on different continents. He called this movement continental drift. Continental drift During the 20th Century scientists developed the theory of Plate Tectonics.

Continental drift was a theory that explained how continents shift position on Earths surface. Continental drift is the theory that the continents slowly and gradually moved to take on their current form. Continental drift was a theory that explained how continents shift position on Earths surface.

Continental drift large-scale horizontal movements of continents relative to one another and to the ocean basins during one or more episodes of geologic time. Wegener said that continents move around on Earths surface and that they were once joined together as a single supercontinent. The gradual movement and formation of continents as described by plate tectonics.

Alfred Wegener first supported continental drift. Set forth in 1912 by Alfred Wegener a geophysicist and meteorologist continental drift also explained why look-alike animal and plant fossils and similar rock formations are found on different continents. Over a vast period of time the continents drifted apart to their current locations.

Pangaea existed about 300 million years ago. Continental drift - the gradual movement and formation of continents as described by plate tectonics geological phenomenon - a natural phenomenon involving the structure or composition of the earth. The theory of continental drift is most associated with the scientist Alfred Wegener.

The continental drift theory is the theory that once all the continents were joined in a super-continent which scientists call Pangaea. CONTINENTAL DRIFT THEORY Continental drift is the hypothesis that all the continents had once been joined together in a single landmass. Continetal drift theory Essays - Continental Drift the theory that continents move slowly about the earths surface changing their positions relative to one another and to the poles of the earth.

Continental drift is a translation of the German. Continental drift can also be used in a jokey way to describe things that move really slowly. In the early 20th century Wegener published a paper explaining his theory that the continental landmasses were drifting across the Earth sometimes plowing through oceans and into each other.

Alfred Wegener named this supercontinent Pangaea. This concept was an important precursor to the development of the theory of. This was the time when reptiles and winged insects first appeared.

Theory of Continental Drift The continental drift hypothesis was developed in the early part of the 20th century mostly by Alfred Wegener. Continental drift was a revolutionary scientific theory developed in the years 1908-1912 by Alfred Wegener 1880-1930 a German meteorologist climatologist and geophysicist that put forth the hypothesis that the continents had all originally been a part of one enormous landmass or supercontinent about 240 million years ago before breaking apart and drifting to their current locations. Continental drift plate tectonics The theory of continental drift was proposed at the beginning of the last century by German scientist Alfred Wegener.

The theory suggested that the crust of the Earth is split up into seven large plates see map below and a few smaller ones all of which can slowly move around on the Earths surface.