because Alfred Wegener stated that the continents seperated there for the parts have seperated.
The continents in the eastern hemisphere are ...Completely:AsiaAustraliaPartly:EuropeAfricaAntarcticaNorth America
Well I know 4 Rock evidence mountain belt evidence fossil evidence puzzle piece evidence Hope it helped.......
The world continents are North America, South America, Africa, Europe, Asia, Australia.
Canada actually has no continents. You need to phrase your questions properly. "How continents does Canada have?" actually makes no sense at all. You should have said "What continent does Canada belong to?" Because we don't own any continents. To answer your question: North America.
The theory of plate tectonics provides evidence that continents have moved over time. This evidence includes matching geological features between continents that were once part of the same landmass, like the coastlines of Africa and South America. Additionally, the distribution of fossils and the alignment of mountain ranges suggest that continents were once connected and have since drifted apart.
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.
Alfred Wegener used several lines of evidence to establish the theory of continental drift, including the fit of the continents, matching geological features across continents, and the distribution of fossils. One key piece of evidence Wegener used was the matching geological formations and rock types found on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe. These similarities in geological features across continents supported Wegener's hypothesis that the continents were once connected and had drifted apart over time.
Evidence supporting the theory of continental drift includes the matching shapes of continents like South America and Africa, similar rock formations and mountain chains across continents, matching fossils found on continents that are now separated by oceans, and the alignment of magnetic minerals in rocks on either side of mid-ocean ridges. These pieces of evidence suggest that continents were once connected and have since moved apart.
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.
Evidence to support the theory of Pangaea includes the fit of continents like South America and Africa, the distribution of similar fossils and rock formations across continents, and matching mountain ranges and geological structures on different landmasses. Furthermore, the study of plate tectonics has provided additional evidence by explaining how continents have moved over time.
North America and Europe had matching rocks and minerals found, indicating that these continents were once joined together as part of the supercontinent Pangaea.
Africa and South America were used as evidence for the continental puzzle due to the matching shapes of their coastlines and geological similarities such as rock formations and fossils found on both continents. This helped support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
Fossil evidence: Identical fossils of plants and animals have been found on continents that are now widely separated, suggesting they were once connected. Geological evidence: Matching rock formations and mountain ranges on different continents provide evidence of their past connection. Climate evidence: Similar coal deposits and glacial striations found across continents support the idea of a single supercontinent with a consistent climate.
The matching coastlines and geologic similarities between continents, specifically between South America and Africa, led some to suspect that the continents were once connected. This evidence, known as continental drift, was proposed by Alfred Wegener in the early 20th century.
Alfred Wegener's evidence for the theory of continental drift included matching coastlines on different continents, similar rock formations and mountain ranges across continents, and the presence of identical fossils on separate continents. He also noted the jigsaw-like fit of South America and Africa and the distribution of climatic zones in ways that made more sense if the continents were once connected.
Fit of the continents – The coastlines of South America and Africa appeared to fit together like puzzle pieces. Fossil evidence – Similar fossils of plants and animals were found on continents that are now separated by oceans. Rock formations – Matching rock formations and mountain ranges were observed on different continents. Climate evidence – Evidence of past glaciation patterns suggested that continents were once connected in ways that are not currently seen.