Evidence for the theory of continental drift includes the fit of the continents like puzzle pieces, similarities in rock formations and geological structures across continents, matching fossil evidence of similar plants and animals found on different continents, and similarities in ancient climate evidence like glaciation patterns. The most notable evidence now comes from the study of plate tectonics, which explains how and why the continents have moved over time.
Evidence of continental drift includes the matching shapes of continents, similar fossils found on different continents, and geological features that align across separate continents. These clues suggest that the continents were once joined together in a single landmass called Pangea.
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.
Continents fit together like puzzle pieces - the coastlines of continents such as South America and Africa seem to fit together like pieces of a puzzle. Fossil evidence - similar fossils of plants and animals found on continents that are now far apart suggest they were once connected. Rock formations and mountain ranges - similar geological features and rock formations found on continents that are now separated indicate they were once part of the same landmass.
Evidence for continental drift includes the fit of continents like South America and Africa, similar rock formations and mountain ranges on different continents, and the distribution of fossils that were once found on now widely separated landmasses. These pieces of evidence suggest that the continents were once connected in a single landmass called Pangaea.
There are two basic evidences to support this theory: 1. Animals or plants of the same species can be found on separated continents (for example, Africa and Australia or North America and Europe) naturally, and have not been placed by man. This must mean all the continents were previously connected, allowing the animals and plants to disperse. 2. The continents all seem to fit together like a jigsaw puzzle. This must mean all the continents were previously connected, but have since broken off and their coastlines have eroded since then, which explains why they do not perfectly fit together.
One piece of evidence that indicates the continents were once connected is the shape of the continents. Many of the continents look as if they fit together like a puzzle.
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.
Evidence of continental drift includes the matching shapes of continents, similar fossils found on different continents, and geological features that align across separate continents. These clues suggest that the continents were once joined together in a single landmass called Pangea.
The shapes of those continents, too many looked like they fitted together.
smiliar fossils and plants, matching of the continents as a jig-saw puzzle, remaining of tropical plants
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.
Continents fit together like puzzle pieces - the coastlines of continents such as South America and Africa seem to fit together like pieces of a puzzle. Fossil evidence - similar fossils of plants and animals found on continents that are now far apart suggest they were once connected. Rock formations and mountain ranges - similar geological features and rock formations found on continents that are now separated indicate they were once part of the same landmass.
It seems to prove that these continents were once close enough to each other that animals and plants could easily move between them through land.
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.
Yes, the theory of continental drift suggests that the Earth's continents were once joined together in a single landmass called Pangaea. This theory is supported by evidence such as the matching shapes of continents, distribution of fossils, and geological similarities across continents.
Wegner developed this theory not only because many continents appear to fit together like a jigsaw, but also because he had fossil and climate evidence to support the fact that the continents once fit together.
Evidence for continental drift includes the fit of continents like South America and Africa, similar rock formations and mountain ranges on different continents, and the distribution of fossils that were once found on now widely separated landmasses. These pieces of evidence suggest that the continents were once connected in a single landmass called Pangaea.