Alfred Wegener's theory of continental drift is supported by the fitting together of the Coastlines of South America and Africa, which appear to align like pieces of a jigsaw puzzle. Additionally, geological similarities, such as matching rock formations and fossil evidence of identical species found on both continents, further bolster his argument. These findings suggest that the continents were once part of a larger landmass, which eventually split and drifted apart over time.
Fossil evidence: the discovery of identical fossils on continents separated by vast oceans supports the idea that these landmasses were once joined together. Matching geological features: the alignment of mountain ranges and rock formations on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, provide evidence of past connections.
One main evidence is the fit of the continents' coastlines, particularly the fit of South America and Africa. Fossil evidence of similar species found on different continents also supports the idea of continental drift. Additionally, the matching geological features and rock formations across continents provide further evidence for the theory of continental drift.
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An example of evidence from land features that supported Wegener's idea of continental drift might include the piecing together of map layouts which show the way that the continents fit together. Wegener is famous for sharing this example.
Evidence to prove the existence of the supercontinent Pangaea includes fossil evidence of similar plant and animal species across continents, the matching shapes of coastlines and mountain ranges on different continents, and the distribution of ancient rock formations that line up when continents are fitted together. Additionally, geological evidence such as rock layers and paleoclimatic data also supports the theory of Pangaea's existence.
The continents of Africa and South America are often used as evidence for the continental puzzle due to their matching coastlines and geological features, suggesting they were once connected. This supports the theory of continental drift and plate tectonics.
South America and Africa have coastlines that fit together like puzzle pieces, providing evidence of the continental drift theory. Another example is North America and Europe, particularly the eastern coast of North America and the western coast of Europe, which also show signs of fitting together.
South America and Africa fit together like puzzle pieces.
The geographic distribution of the swimming reptile Mesosaurus provides evidence that supports continental drift. Fossils belonging to the Mesosaurus were found far away from each other, in both South Africa and South America.
Evidence Supporting PangeaCoastlines fit togetherFossil DistributionRock StrataCoal DistributionAfrica and South America appear to fit together very well, this however is not enough evidence alone to support the idea of continental drift. There are however matching fossils of animals have been found in both Africa and South America. Plant fossils have also been found on parallel lines indicating that the climate at one point had to be the same but now, the climates are extremely different and wouldn't allow for mutual fern species to grow.Rock strata, and mineral deposits also line up to indicate that at one point, the continents formed one, large super continent called "Pangea."
Cynognathus is a good candidate for providing evidence for the continental drift theory because its fossil has been found in both South America and Africa, which were once connected in the supercontinent Gondwana. This distribution pattern supports the idea of continental drift, as it suggests that these continents were once joined together and later drifted apart.
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