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A German scientist Alfred Wegener first proposed the idea of Continental Drift.
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!
I do, looking at the map it does look like a puzzle and all the continents look like they connect or used to connect.
Faults and folds just support the idea that there lithospheric plates are in motion because folds appear when the plates move towards each other. The faults appear when the plates drift apart and cause an empty space.
The hypothesis that continents 'drift' was first put forward by Abraham Ortelius in 1596 and was fully developed by Alfred Wegener in 1912. During Wegener's lifetime, his theory of continental drift was severely attacked by leading geologists, who viewed him as an outsider meddling in their field.[12] His hypothesis received support from South African geologist Alexander Du Toit as well as from Arthur Holmes, but was not generally supported due to the lack of a known driving force and the absence of evidence beyond the coastline shapes and fossil records. The possibility of continental drift gradually became accepted by the late 1950s. By the 1960s, geological research conducted by Robert S. Dietz, Bruce Heezen, and Harry Hess, along with a revision of the theory including a mechanism by J. Tuzo Wilson, led to widespread acceptance of the theory among geologists.
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The name of the floral fossils Wegner used for the idea of continental drift was glossopteris. Alfred Wegner used the continental drift as a way to explain the continental shapes.
the theory would be called Continental drift.
Alfred Wegener
the mechanism for continental drift was not well understood at the time, and there was no evidence to support the idea of continents moving. It wasn't until the theory of plate tectonics was developed that the idea of continental drift became widely accepted.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
the breaking down of pangea
The idea known as "Continental Drift."
Alfred Wegener was the scientist who proposed the idea of continental drift in the early 20th century. He suggested that the Earth's continents were once joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.
Evidence of ancient climates, such as glacial deposits in regions that are now near the equator, support continental drift theory because they suggest that these regions were once located at higher latitudes where glaciers were common. This is consistent with the idea that continents were once joined together in different configurations and have since drifted to their current positions. Additionally, similarities in fossil distributions and rock formations across continents also support the theory of continental drift.