Did you mean Plate Tectonics Theory? - Plate Tectonics Theory is the combination of Continental Drift and Ocean/Sea Floor Spreading. BTW. The scientist who started it is Howard Baker continued by Alfred Wegener.
Alfred Wegener proposed the theory of continental drift at the beginning of the 20th century. His idea was that the Earth's continents were once joined together, but gradually moved apart over millions of years. The idea was rejected at first as he was a Meteorologist and not regarded as a proper scientist.
they though he was crazy and became his critics
No, not until later was this theory proven and supplemented by the theory of plate tectonics.
what year did Alfred Wegener graduate college in
Alfred wegener's theory of continental drift was not accepted by most of the scientific community in his world.
Did you mean Plate Tectonics Theory? - Plate Tectonics Theory is the combination of Continental Drift and Ocean/Sea Floor Spreading. BTW. The scientist who started it is Howard Baker continued by Alfred Wegener.
Alfred Wegener
because they didn't have the proper technology to prove it.
Alfred Wegener's continental drift theory has subsequently been honed by scientific discoveries to the more all-inclusive plate tectonic theory which is generally accepted by earth scientists.
they finally accepted his theory because scientist tested his theory and found the same conclusion which alfred wegner had already said before he died.
Alfred Wegener was a meteorologist who introduced the theory of continental drift.
Alfred Wegener
Alfred wegener call the supercontinent Pangaea (i guess)
Alfred Wegener's full name is "Alfred Lothar Wegener", and he is a German scientist who came up with the theory of Continental Drift.
Because Alfred Wegener couldn't specify the mechanism responsible for the movement of the continents, the continental drift hypothesis was rejected. This theory is now accepted science.
Alfred Wegener was the proponent of the Continental Drift Theory. The scientific community accepted this theory due to the phenomena of paleomagnetism, sea floor spreading and plate tectonics.