Alfred Wegener noticed that the continents looked like they could fit together like a puzzle, particularly along their Coastlines. This observation led him to propose the theory of continental drift, suggesting that the continents were once joined together in a supercontinent called Pangaea.
The evidence for moving continents, known as continental drift, includes the fit of the coastlines of continents like South America and Africa, the similarity of rock formations and fossils on different continents, and the presence of ancient glaciation patterns on continents that are now located in warmer climates. These pieces of evidence formed the basis for the theory of plate tectonics.
Yes, the presence of the same organisms on multiple continents suggests that at some point in the past, those continents were connected. This supports the theory of continental drift, which explains how landmasses have moved over time. The distribution of these similar organisms across different continents provides additional evidence for this theory.
Wagner proposed the theory of continental drift, suggesting that the continents were once joined together in a single supercontinent called Pangaea. He observed that identical rock sequences and geological structures appeared on different continents, supporting the idea of continental movement over time.
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 welcomeif you write this that would be bad and you will go to jail....good luck dick sucker
Alfred Wegener used geological and paleontological evidence to propose the theory of continental drift. He observed similarities in rock formations, fossils, and mountain ranges on different continents that suggested they were once connected. Additionally, Wegener developed a hypothesis known as Pangaea, suggesting a supercontinent that gradually broke apart over millions of years to form the continents we see today.
Fossils found on different continents that were once connected support the idea of continental drift. The similarities in fossilized plants and animals found on separate continents suggest these landmasses were once part of the same supercontinent. This evidence helps corroborate the hypothesis of continental drift proposed by Alfred Wegener.
These observations were used in the process of making observations and forming a hypothesis about continental drift. By noticing the fit of continents, matching fossils, and similar structures across different continents, scientists were able to propose the theory that continents were once connected and have since drifted apart. This hypothesis was then tested and supported through further research and evidence gathering.
Continental drift is the hypothesis that states that the continents once formed a single land
Alfred Wegener used fossil evidence (matching plant and animal species across continents), geological evidence (similar rock formations and mountain ranges on different continents), climate evidence (glacial deposits and ancient climate patterns that suggested continents were once connected), and fit of continents (the way the continents seem to fit together like a puzzle) to support his hypothesis of continental drift.
Yes, fossils and rocks support the hypothesis of continental drift. Matching plant and animal fossils found on different continents suggest they were once part of the same landmass. Rocks with similar ages and compositions found across continents also provide evidence for the movement of these landmasses over time.
matching geological features, such as similar rock formations and mountain ranges, on different continents. This suggests that the continents were once connected and have since drifted apart.
Fossil evidence showing similar plant and animal species in regions that are now widely separated provides support for Wegner's hypothesis of continental drift. This suggests that the continents were once connected in a single landmass.
Fossils of the reptile Mesosaurus have been found in South America and Africa. It probably couldn't swim between the continents. Scientists theorized that this reptile lived on both continents when they were joined. All continents were once part of a large landmass, called Pangea, that broke apart 250-million years ago.
The evidence for moving continents, known as continental drift, includes the fit of the coastlines of continents like South America and Africa, the similarity of rock formations and fossils on different continents, and the presence of ancient glaciation patterns on continents that are now located in warmer climates. These pieces of evidence formed the basis for the theory of plate tectonics.
Wegner's hypothesis of continental drift was supported by evidence such as the jigsaw-like fit of continents, similarities in rock formations and geological structures across continents, and matching fossil evidence found on different continents. Additionally, the discovery of mid-ocean ridges and magnetic striping on the ocean floor provided further evidence for the movement of continents.
Yes, the presence of the same organisms on multiple continents suggests that at some point in the past, those continents were connected. This supports the theory of continental drift, which explains how landmasses have moved over time. The distribution of these similar organisms across different continents provides additional evidence for this theory.
Alfred's hypothesis was that all the continents was a big land mass which he called Pangaea because if you see a world map it is like a jigsaw puzzle and other evidence is that some animal fossils were on other continents and also the same rock range was found on different continents. This hypothesis is known as continental drift.