Alfred Wegener used climate to support his hypothesis of continental drift by noting that matching plant and animal fossils, as well as rock formations, across continents with similar past climates suggested that these landmasses were once connected. He argued that the distribution of certain geological features and fossils could only be explained by the movement of the continents over time.
Wegener used similarities in fossil evidence and rock formations across different continents, along with past climatic evidence such as glacial deposits in regions where glaciers no longer exist, to support his hypothesis of continental drift. He argued that these geological and climatic similarities could only be explained by the continents once being connected in a single landmass.
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
A continent close to the equator has a warm and mild climate. A continent far from the equator has a colder climate. Wegener found that continents now in a colder climates have evidence that they used to be in warmer climates, or vice versa. E.g. Wegener found that Spitsbergen, an island now in the Arctic Ocean, has fossils of tropical plants, plants that lived in warm places. Spitsbergen couldn't possibly be warm when it was in the Arctic Ocean, so according to Wegener, Spitsbergen must have been located near the equator about 300 million years ago.
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.
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.
well it wasn't so much climate as the fossils that have been found
hypothesis
Wegener used similarities in fossil evidence and rock formations across different continents, along with past climatic evidence such as glacial deposits in regions where glaciers no longer exist, to support his hypothesis of continental drift. He argued that these geological and climatic similarities could only be explained by the continents once being connected in a single landmass.
Alfred Wegener used several pieces of evidence to support his theory of continental drift, including the fit of continents like South America and Africa, similar rock formations and mountain ranges across continents, and the distribution of plants and animals. He also looked at evidence from fossils and ancient climate data to support his hypothesis.
A continent close to the equator has a warm and mild climate. A continent far from the equator has a colder climate. Wegener found that continents now in a colder climates have evidence that they used to be in warmer climates, or vice versa. E.g. Wegener found that Spitsbergen, an island now in the Arctic Ocean, has fossils of tropical plants, plants that lived in warm places. Spitsbergen couldn't possibly be warm when it was in the Arctic Ocean, so according to Wegener, Spitsbergen must have been located near the equator about 300 million years ago.
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.
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.
science stuff and about soccer
Wegener used the presence of the same fossil species on continents that are now widely separated as evidence for his hypothesis of continental drift. He argued that these fossils could only have come from animals that were able to move, ruling out the possibility of passive transport by ocean currents. This supported his idea that the continents were once connected and later drifted apart.
Alfred Wegener used deductive reasoning in developing his continental drift theory. He collected evidence from different fields such as geology, paleontology, and climatology to support his hypothesis that the continents were once connected in a single supercontinent called Pangaea.
He uses everything
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.