Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
Climate clues such as glacial deposits and ancient sea level changes can help support the theory of continental drift by showing how certain landmasses were once connected and located in different positions on Earth. By looking at these climate indicators, scientists can reconstruct past climates and the movement of continents over millions of years. This evidence helps explain how continents have shifted and drifted to their current positions.
he used climate clues and fossil clues and rock clues to figure out for example he found that it was warm in the south and the north and he founddinosaurs fossils on different continents and he found out that there was the same rocks on different continents there so that answers your question.
Climate clues are evidence or indicators that help scientists understand historical changes in the Earth's climate. These clues can include ice cores, tree rings, sediment layers, and temperature records which provide information about past climate conditions and trends. By studying these clues, scientists can reconstruct past climates and predict future climate patterns.
Rock clues such as similar rock formations and fossils found on different continents supported the hypothesis of continental drift by indicating that the continents were once connected. Matching patterns of mountain ranges and geological structures between continents further supported the idea of continental drift and the existence of a supercontinent in the past. Also, the presence of glacial deposits in regions that are now separated by oceans provided evidence of past climatic conditions and continental movement.
Clues useful in reconstructing Pangaea include the matching shapes of continents' coastlines, similarities in rock formations and fossils across continents, and the alignment of mountain ranges and geological structures. Additionally, paleoclimatic evidence such as glacial deposits and ancient climate patterns can provide further support for the theory of Pangaea.
well it wasn't so much climate as the fossils that have been found
glacial deposits
I don't know. :p
fossils of once living things provide clues that support contenental drift
Climate clues such as glacial deposits and ancient sea level changes can help support the theory of continental drift by showing how certain landmasses were once connected and located in different positions on Earth. By looking at these climate indicators, scientists can reconstruct past climates and the movement of continents over millions of years. This evidence helps explain how continents have shifted and drifted to their current positions.
Rock clues support Wegners theory of continental drift and Pangaea because when India hit Eurasia the Himalayas formed and that is where Mt Everest is today! Climate clues include glacial evidence in tropical places it shows glacial evidence that there was once glaciers there. Fossil clues in clue many tropical plants and animal fossils were found in places like Antarctica where these plants and animals could not grow. Also dinosaur bones were found scattered around there earth. Dinosaurs can't swim, so they must have walked around this way!
parts of the Appalachian Mountain of the eastern US are similar to those found in Greenland and western Europe. Rock clues like these support the idea that the continents were connected in the past.
he used climate clues and fossil clues and rock clues to figure out for example he found that it was warm in the south and the north and he founddinosaurs fossils on different continents and he found out that there was the same rocks on different continents there so that answers your question.
Climate clues are evidence or indicators that help scientists understand historical changes in the Earth's climate. These clues can include ice cores, tree rings, sediment layers, and temperature records which provide information about past climate conditions and trends. By studying these clues, scientists can reconstruct past climates and predict future climate patterns.
Well it wasn't so much climate as the fossils that have been found. Fossils have been found in Antarctica of plants that only occur in tropical climates so at one point it must have had a tropical climate. That is the most dramatic example but there are more subtle ones that led him to believe that the continents, at one point, must have been in different locations on the Earth and then moved to where they currently are.
The evidence scientists have are fossil clues, plant clues, climate clues and rock clues. Fossil clues supported the idea because a certain fossil the Mesosaurus was found in two continents on opposite sides of the Earth and the only reason for that is if the lands came together at one time. Plant clues support the idea the same way fossil clues do, like the plant called a Glossopteris was found in different areas around the world. Climate clues support the idea because some of the fossils and plants from warmer climates were found in the Arctic. That explains why there are glaciers in tropical areas. Lastly rock clues support the idea because if the continents were once connected at one time, then the rocks that made up the continents should be in the same locations where they were joined.
Rock clues such as similar rock formations and fossils found on different continents supported the hypothesis of continental drift by indicating that the continents were once connected. Matching patterns of mountain ranges and geological structures between continents further supported the idea of continental drift and the existence of a supercontinent in the past. Also, the presence of glacial deposits in regions that are now separated by oceans provided evidence of past climatic conditions and continental movement.