because when continental drift happened it split fossils and when people found the fossils in one continent.It matched with other continents fossils.making a hypothesis that they were once joined together...................................your welcome
if you write this that would be bad and you will go to jail....good luck dick sucker
Evidence for the continents being joined together in a supercontinent, called Pangaea, includes similar fossil and rock formations found on different continents, the alignment of mountain ranges and geological structures when continents are pieced together like a jigsaw puzzle, and matching Coastlines and continental shelves that fit together like a puzzle. Additionally, evidence from paleoclimatology, the study of past climates, supports the theory of continental drift.
The main evidence that supports the theory of one supercontinent is the presence of similar geological features, rock formations, and fossils on different continents that align perfectly when the continents are pieced together, such as the coastlines of South America and Africa. Additionally, studies on paleoclimatology and the distribution of ancient species provide further evidence of the continents once being connected in a single landmass.
If I were Wegener, I would look for matching geological features on different continents, such as similar rock types, mountain ranges, and fossils. I would also investigate any evidence of past climate change that could support the idea of continents moving. Additionally, I would search for remnants of ancient land bridges or plate boundaries to further support my hypothesis of continental drift.
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.
Fossils of the same species found on separate continents suggest that those continents were once connected. Mountain belts show evidence of ancient tectonic activity, helping to illustrate how continents may have moved. These clues were key in developing the theory of plate tectonics and determining how continents have shifted over geological time.
Paper cutouts of the continents can be pieced together to form a single whole is because the continents were at one point all connected, which was the super continent Pangaea.
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
Evidence supporting the theory of the supercontinent Pangaea includes the jigsaw-like fit of continents, similarities in rock formations and mountain ranges across continents that align when continents are brought together, distribution of fossils of identical species across distant continents, and similarities in ancient climates and geological records found on separate continents. These pieces of evidence work together to suggest that the current continents were once part of a single landmass.
Maybe the depth of oceans
Evidence for continental drift includes the matching coastlines of continents, similar rock formations and mountain ranges across continents, identical fossils found on different continents, and the alignment of magnetic minerals in rocks that show continental movement. These pieces of evidence support the theory that continents were once joined together in a supercontinent called Pangaea and have since drifted apart.
The main evidence that supports the theory of one supercontinent is the presence of similar geological features, rock formations, and fossils on different continents that align perfectly when the continents are pieced together, such as the coastlines of South America and Africa. Additionally, studies on paleoclimatology and the distribution of ancient species provide further evidence of the continents once being connected in a single landmass.
If I were Wegener, I would look for matching geological features on different continents, such as similar rock types, mountain ranges, and fossils. I would also investigate any evidence of past climate change that could support the idea of continents moving. Additionally, I would search for remnants of ancient land bridges or plate boundaries to further support my hypothesis of continental drift.
One example is the fit of the continents' coastlines, such as the matching shapes between the continents of Africa and South America. This suggests that they were once connected and have since drifted apart.
Scientists use various pieces of evidence to support the theory of past continents, such as matching geological formations, rock types, and fossils found on different continents, and the fit of continental coastlines like pieces of a puzzle. Additionally, studies of plate tectonics show how continents have moved and shifted over millions of years, providing further evidence for the existence of ancient landmasses.
The shapes of continents appearing on the map clearly show similar shapes and how the continents might fit together.
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.
It can help show that continental drift happened, if you find the same fossils on different continents. This would mean that the continents had to be close together if the fossils are found on land.
Fossils found in different regions can provide evidence of past geographic connections by showing similar species distributed across separate continents. By studying fossils, scientists can piece together the history of land formations and the movement of continents, helping to support the theory of supercontinents like Pangaea.