fossils continents look like puzzle pieces (which means Coastlines match up) rock samples that's bout it...
Evidence of Pangaea includes the fit of the modern continents, similarities in rock formations across continents, distribution of fossils found on continents that were once part of Pangaea, and geological structures found in different continents that line up when Pangaea is reconstructed. Additionally, the mapping of ancient climate belts and glacial deposits provide further evidence of the supercontinent.
Geology, paleontology, and paleoclimatology were used to gather evidence for the existence of Pangaea. These sciences helped researchers study the geological formations, fossil records, and ancient climate patterns across different continents to reconstruct the supercontinent Pangaea.
Scientific evidence supporting the theory of Pangaea includes the fit of the continents' coastlines, similarities in rock formations and geological structures across continents, and matching fossil evidence of ancient plants and animals. Additionally, the distribution of certain species among continents and the discovery of mid-ocean ridges and plate tectonics further support the concept of Pangaea.
Evidence supporting the existence of Pangaea includes the jigsaw-like fit of the continents, similarities in rock types and mountain ranges across continents, fossil evidence of similar species found on different continents, and glacial striations that align when continents are pieced back together. Additionally, scientists have used paleomagnetic data and plate tectonics theory to further support the theory of Pangaea's existence.
Alfred Wegener proposed the theory of Pangaea in 1912 based on his research on the fit of the continents, fossil evidence, and rock formations.
Evidence supporting the existence of Pangaea includes: Fossil evidence of similar species found on different modern continents. Rock formations and mountain ranges that match up when continents are rearranged. Paleoclimatic evidence, such as glacial deposits in regions that are now warmer. Similarities in geologic structures and ages of rocks across continents.
Plate tectonics led to the theory of Pangaea.
Egghead Egghead
Geology, paleontology, and paleoclimatology were used to gather evidence for the existence of Pangaea. These sciences helped researchers study the geological formations, fossil records, and ancient climate patterns across different continents to reconstruct the supercontinent Pangaea.
Pangaea
Evidence to prove the existence of the supercontinent Pangaea includes fossil evidence of similar plant and animal species across continents, the matching shapes of coastlines and mountain ranges on different continents, and the distribution of ancient rock formations that line up when continents are fitted together. Additionally, geological evidence such as rock layers and paleoclimatic data also supports the theory of Pangaea's existence.
Scientific evidence supporting the theory of Pangaea includes the fit of the continents' coastlines, similarities in rock formations and geological structures across continents, and matching fossil evidence of ancient plants and animals. Additionally, the distribution of certain species among continents and the discovery of mid-ocean ridges and plate tectonics further support the concept of Pangaea.
Evidence supporting the existence of Pangaea includes the jigsaw-like fit of the continents, similarities in rock types and mountain ranges across continents, fossil evidence of similar species found on different continents, and glacial striations that align when continents are pieced back together. Additionally, scientists have used paleomagnetic data and plate tectonics theory to further support the theory of Pangaea's existence.
Alfred Wegener proposed the theory of Pangaea in 1912 based on his research on the fit of the continents, fossil evidence, and rock formations.
Evidence supporting the existence of Pangaea includes: Fossil evidence of similar species found on different modern continents. Rock formations and mountain ranges that match up when continents are rearranged. Paleoclimatic evidence, such as glacial deposits in regions that are now warmer. Similarities in geologic structures and ages of rocks across continents.
Evidence such as the distribution of fossils, rock formations, and magnetic fields on different continents support the theory of continental drift and the breakup of Pangaea. The matching geological features, such as mountain ranges and coastlines, on opposite sides of the Atlantic Ocean provide further evidence that the continents were once connected. Additionally, the movement of tectonic plates and the ongoing process of plate tectonics help explain the separation of the continents from Pangaea.
Many scientists were skeptical of the Pangaea theory when it was first proposed by Alfred Wegener in the early 20th century because he did not have a satisfactory mechanism to explain how the continents moved. It wasn't until the development of the theory of plate tectonics that provided a mechanism for continental drift that the scientific community widely accepted the concept of Pangaea.
The existence of Pangaea, the supercontinent that existed over 290 million years ago, is supported by various lines of evidence such as the matching shapes of continents and similarities in rock formations and fossils found across continents. Climate data, including evidence from ancient glaciations and sedimentary rocks, also supports the theory of Pangaea. These pieces of evidence help scientists reconstruct the past positions of continents and understand Earth's geological history.