the same rock types on the edges of different continents
and the reverse magnetic polarity show seafloor spreading which shows that the continents are moving.
the Coastlines of South Africa and south ameria seem to match and fit together like a jigsaw and so do many other countries which gives the impression that all the continents were onced joined together as a massive continent called Pangaea
The theory of continental drift is primarily supported by evidence such as the fit of continental coastlines, fossil correlations across continents, and geological similarities. However, it is not supported by the idea that continents are fixed in place, as this contradicts the core concept of continental drift, which posits that continents move over geological time. Additionally, the lack of a mechanism for how continents could drift was a significant challenge to the theory before the development of plate tectonics.
In the 1960s, scientific evidence from studies of paleomagnetism, seismic activity, and ocean floor mapping supported the occurrence of continental drift. This evidence provided crucial support for the theory of plate tectonics, which explains how the Earth's continents move and interact on the surface.
Several evidences were given as proof to the theory of continental drift, they include; 1. Climatic evidence (Paleoclimatic Reconstruction). 2. Fossil evidence (Paleontological proof). 3. Continental fit. (Continental margin shapes). 4. Lithological and Stratigrapical similarities of adjacent continental masses. 5. Seafloor spreading. 6. Glacial till. 7. Plate tectonics.
Yes, fossils are evidence of continental drift because similar fossils have been found on different continents that are now far apart. This suggests that these continents were once connected, supporting the theory of continental drift.
The presence of glossopteris fossils in regions that are now widely separated provided evidence for continental drift. This plant species was found in South America, Africa, India, Antarctica, and Australia, suggesting that these landmasses were once part of a single supercontinent. The distribution of glossopteris fossils supported the theory of continental drift proposed by Alfred Wegener.
Tropical fossils in Antarctica.
Is there a list? Continental drift is real, so religious fanatics don't provide evidence for continental drift.
no
The same fossils found on different sides of the ocean.
South America and Africa fit together like puzzle pieces.
It is good evidence of continental drift as fossils of previous duck billed platypuses were found in America and Alaska, which Australia was once connected to. This means the platypuses once lived there hence evidence of continental drift.
Plate Tectonics.
In the 1960s, scientific evidence from studies of paleomagnetism, seismic activity, and ocean floor mapping supported the occurrence of continental drift. This evidence provided crucial support for the theory of plate tectonics, which explains how the Earth's continents move and interact on the surface.
Continental drift is a concept relating to the movement of the Earth's continents. The proving of the continental drift theory came from evidence found around the world. Foremost, scientists had discovered that similar plants and animal fossils were found in or around different continents, suggesting that they were once joined. The theory of plate tectonics also supported continental drift. If one were to look at a global map, the complementary arrangements between South America and Africa can be easily seen.
Several evidences were given as proof to the theory of continental drift, they include; 1. Climatic evidence (Paleoclimatic Reconstruction). 2. Fossil evidence (Paleontological proof). 3. Continental fit. (Continental margin shapes). 4. Lithological and Stratigrapical similarities of adjacent continental masses. 5. Seafloor spreading. 6. Glacial till. 7. Plate tectonics.
their roots
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.