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.
There are four things that are used for evidence for the continental drift. The four continental drift was Shape of continents, fossil evidence, glacial evidence and similar rocks found in different continents.
Fossil similarities across continents. Matching geological formations across continents. Alignment of mountain ranges across continents. Distribution of ancient climates and glacial deposits.
Alfred Wegener used four main lines of evidence to support his theory of continental drift: the geometric fit of the continents, matching geological formations across continents, matching fossil distributions across continents, and evidence of past climates from glacial deposits. These pieces of evidence suggested to Wegener that the continents were once joined together in a supercontinent called Pangaea and had since drifted apart.
The evidence of the theory of continental drift can be found on the edges of the tectonic plates. For example, the boundary of the African Plate and the Eurasian plate is in the Mediterranean Sea, just south of the island of Crete. At this boundary, scientists have observed that the Eurasian Plate is sliding under the African Plate at a rate of three to four centimeters per year as the African Plate drifts north.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.
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.
There are four things that are used for evidence for the continental drift. The four continental drift was Shape of continents, fossil evidence, glacial evidence and similar rocks found in different continents.
Fossil similarities across continents. Matching geological formations across continents. Alignment of mountain ranges across continents. Distribution of ancient climates and glacial deposits.
Alfred Wegener used four main lines of evidence to support his theory of continental drift: the geometric fit of the continents, matching geological formations across continents, matching fossil distributions across continents, and evidence of past climates from glacial deposits. These pieces of evidence suggested to Wegener that the continents were once joined together in a supercontinent called Pangaea and had since drifted apart.
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.
The evidence of the theory of continental drift can be found on the edges of the tectonic plates. For example, the boundary of the African Plate and the Eurasian plate is in the Mediterranean Sea, just south of the island of Crete. At this boundary, scientists have observed that the Eurasian Plate is sliding under the African Plate at a rate of three to four centimeters per year as the African Plate drifts north.
Wegener showed evidence of similar rock formations and mountain ranges on different continents, evidence of matching plant and animal fossils on different continents, evidence of matching glacial deposits on different continents, and evidence of matching ancient climates on different continents to support his theory of continental drift.
Alfred Wegener went on four expeditions to Greenland between 1906 and 1930. His expeditions involved studying glaciers, geology, and meteorology to gather evidence to support his theory of continental drift.
To provide a concise answer, could you please specify the context or topic for which you need four pieces of evidence? This will help me tailor the response accurately.
Matching geological formations across continents. Fossil evidence of similar species on different continents. Similar ancient climates and rock formations across continents. Fit of the continents like puzzle pieces on the Earth's surface.
Fit of continents: Fitting the shapes of continents together, especially the east coast of South America and the west coast of Africa. Fossil evidence: Similar fossils and rock formations found on continents separated by vast oceans. Climatic evidence: Tropical plant fossils found in regions that are currently cold, suggesting a different climate in the past. Geological evidence: Similar rock formations and mountain ranges found on different continents, indicating a common geological history. These pieces of evidence were crucial for Wegener's theory because they provided tangible support for the idea that continents were once connected and had drifted apart over time.