The continents of Africa and South America are often used as evidence for the continental puzzle due to their matching Coastlines and geological features, suggesting they were once connected. This supports the theory of continental drift and plate tectonics.
Africa and South America were used as evidence for the continental puzzle due to the matching shapes of their coastlines and geological similarities such as rock formations and fossils found on both continents. This helped support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
Alfred Wegener proposed the idea of continental drift, suggesting that the continents of South America and Africa fit together like a puzzle. He used geological and fossil evidence to support his theory of the supercontinent Pangaea.
Fossil evidence of the same species found on multiple continents. Matching geological formations across continents, such as mountain ranges. Similar rock formations and ages of rocks on different continents. Paleoclimatic evidence, like glacial deposits in areas that are now far from the poles. Fit of continental shelf margins, where coastlines align when continents are pieced together.
Africa and SouthAmerica because they used to be part of a huge land 200 million years ago called Pangaea the land mass started separating. The pieces slowly drifted apart.Today they are now seven continents
A modern day map would do the trick. Alfred Wegener's theory of continental drift is also a factor, which explains that the continents are constantly shifting and that their positions have differed throughout time.
Africa and South America were used as evidence for the continental puzzle due to the matching shapes of their coastlines and geological similarities such as rock formations and fossils found on both continents. This helped support the theory of continental drift proposed by Alfred Wegener in the early 20th century.
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.
Alfred Wegener used evidence such as the fit of continents like puzzle pieces, matching rock formations and fossils across continents, and similarities in geological features to support his theory of continental drift. These pieces of evidence suggested that the continents were once joined together in a single supercontinent, which later drifted apart to their current positions.
Alfred Wegner had 4 theory`s,Climate evidence,Fossil evidence,the continents fitting together like a puzzle,and horizontal movement. The fossils were different types of ancient ferns and Dinosaurs.
Alfred Wegener proposed the idea of continental drift, suggesting that the continents of South America and Africa fit together like a puzzle. He used geological and fossil evidence to support his theory of the supercontinent Pangaea.
Two forms of evidence used to support the continental drift theory are the fit of the continents (jigsaw-like arrangement of continents' coastlines) and matching geological formations (similar rock types, structures, and mountain ranges on different continents). Additionally, paleontological evidence, such as similar fossil records found across separate continents, also supports the theory.
Alfred Wegener used several lines of evidence to support his theory of continental drift, including the fit of the continents like pieces of a jigsaw puzzle, similarities in rock formations and fossils across continents, as well as evidence of past glaciation patterns and ancient climate belts that only made sense if the continents were once connected.
Wegner used evidence from fossil distributions, rock formations, and the fit of continents like puzzle pieces to support his theory of continental drift. He also noted similarities in plant and animal species found on different continents, suggesting they were once connected.
Alfred Wegener used several lines of evidence to support his theory of continental drift. This included the fit of the continents like a jigsaw puzzle, similarities in rock formations and mountain ranges across different continents, matching fossils on separate continents, and paleoclimatic evidence such as glacial striations in tropical regions. These pieces of evidence led Wegener to propose the theory of continental drift in the early 20th century.
Evidence supporting continental drift includes the fit of the continents like pieces of a giant jigsaw puzzle, matching geological features across different continents, similarities in rock formations and mountain chains, distribution of fossils across continents, and the pattern of magnetic stripes on the ocean floor that support seafloor spreading. These pieces of evidence collectively support the theory of continental drift proposed by Alfred Wegener.
Two forms of evidence used to support continental drift are fossil evidence, where similar plant and animal fossils are found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges across separate continents. These pieces of evidence provide support for the idea that continents were once joined together and have since drifted apart.
Alfred Wegener used fossil evidence, geological evidence, paleoclimatic evidence, and the fit of continental coastlines to support his theory of continental drift. By comparing fossils, rock formations, climate patterns, and the alignment of continents like puzzle pieces, Wegener proposed that the continents were once connected in a single supercontinent called Pangaea that drifted apart over time.