i dont even kno ok you people shouldf know
the continents fit together like a puzzle
Climate fossil and fossil climate
The 3 pieces of evidence is: 1. fossils 2. climate 3. glaciers Wegner found out that the same fossils were found on a different continent. There was this tropical plant (i forgot whats it called) was found at a icy cold region so then the plant couldn't grow there only by continental drift. The glaciers have scratches on them which was one of the evidence. I hope this really helped :D
the age of the rocks in the sea floor is all the same
he used fossils, glacial indentations, and different types of rock.
Alfred Weneger was trying to prove his theory of Continental Drift. Many other scientists before him had the same theory, but they never could prove it. He had five pieces of evidence.
the continents fit together like a puzzle
Climate fossil and fossil climate
The 3 pieces of evidence is: 1. fossils 2. climate 3. glaciers Wegner found out that the same fossils were found on a different continent. There was this tropical plant (i forgot whats it called) was found at a icy cold region so then the plant couldn't grow there only by continental drift. The glaciers have scratches on them which was one of the evidence. I hope this really helped :D
the age of the rocks in the sea floor is all the same
he used fossils, glacial indentations, and different types of rock.
The pieces of evidence Alfred Wegener used to support his theory about continental drift were; Puzzle Fit, Fossil evidence from animals that were once on the same continent, geologic evidence like mountain chains that were connected and now split apart, and ice sheets. Thank you for reading this article and I hoped it answered your question!
Climate, and landforms
Alfred Wegener's theory was known as the theory of continental drift.
The 100% correct answer is A similar fossil was found in Africa, South America, Australia, India, and Antarctica.
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Alfred Wegener used various pieces of evidence to support his theory of continental drift, including the fit of the continents, rock and fossil similarities across continents, glacial evidence, and similar geological features on different continents.