Alfred Wegener observed that the continents seemed to fit together like pieces of a puzzle, that identical fossils and rock formations were found on separate continents, and that similar climates and geological features occurred on continents that were now far apart. These observations led him to propose the theory of continental drift.
he used fossils, glacial indentations, and different types of rock.
Alfred Wegener used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Alfred Wegener's theory of continental drift was supported by several pieces of evidence, including the fit of the continents like a jigsaw puzzle, similarities in rock formations and fossils across continents, and matching geological features such as mountain ranges and coastlines. Additionally, Wegener found evidence of past glaciation in regions that are now separated by oceans, suggesting they were once connected.
Most scientists rejected Alfred Wegener's theory of continental drift in the early 20th century because he did not provide a convincing mechanism to explain how continents could move. Additionally, Wegener's idea went against prevailing scientific beliefs at the time, and there was limited geological evidence to support his theory. It wasn't until the development of plate tectonics in the 1960s that Wegener's ideas were widely accepted.
Wegener used evidence from the fit of the continents, the distribution of fossils, and similarities in rock formations and mountain ranges across different continents to support his theory of drifting continents.
Yes, Alfred Wegener had two daughters with his wife Elsa, named Lotte and Inge.
November 2 or 3, 1930
he used fossils, glacial indentations, and different types of rock.
He did get Married he married, In 1850 he married Emily Sarah Sellwood.......
Alfred Wegener Noticed: 1. Landforms like coal saturations or mountain ranges on either side of the ocean. 2. Fossil record. Fossils of identical plants and animals found in africa and south america. 3. Aincient striations (grooves and scratches made by ice ages) identical on either side of the ocean.
Unsure but Alfred Wegener invented them/studies them so try looking him up.
nutin
Alfred Wegener used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Alfred Wegener's theory of continental drift was supported by several pieces of evidence, including the fit of the continents like a jigsaw puzzle, similarities in rock formations and fossils across continents, and matching geological features such as mountain ranges and coastlines. Additionally, Wegener found evidence of past glaciation in regions that are now separated by oceans, suggesting they were once connected.
Alfred Wegener proposed his theory of continental drift based on three main pieces of evidence: first, the jigsaw-like fit of continental coastlines, particularly South America and Africa; second, the presence of similar fossils, such as Mesosaurus and Glossopteris, found on widely separated continents; and third, geological similarities, including matching rock formations and mountain ranges across continents. These observations suggested that continents were once connected and have since drifted apart over time.
Gondwana and laurasia......tehehehhe i feel sooo special helping you:)<3
Alfred Wegener proposed his theory of continental drift by citing three main pieces of evidence: first, the jigsaw-like fit of the continents, particularly South America and Africa; second, the distribution of similar fossils across widely separated continents, such as the Mesosaurus found in both South America and Africa; and third, geological similarities, including matching rock formations and mountain ranges found on different continents. These observations suggested that the continents were once joined together in a supercontinent before drifting apart.