Alfred Wegener Hypothesis of Continental Drift

Alfred Wegener included all of the following lines of evidence as supporting his continental drift hypothesis except one. Which was NOT part of Wegeners evidence.

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Plate tectonics implies that Earth must be expanding.

. Alfred Wegeners fossil evidence for continental drift is shown on the cut-outs. 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. The first truly detailed and comprehensive theory of continental drift was proposed in 1912 by Alfred Wegener a German meteorologistBringing together a large mass of geologic and paleontological data Wegener postulated that throughout most of geologic time there was only one continent which he called PangeaLate in the Triassic Period which lasted from.

Try to logically piece the continents together so that they form a giant supercontinent. In convection warm material rises because it is more dense. When you are satisfied with the fit of the continents glue the land masses down on a piece of paper.

Stripes of reverse magnetism on either side of oceanic rides. Use Wegeners fossil evidence to place them in the correct positions.

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