Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
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.
The continental Coastlines fit together like puzzle pieces, fossils, and glacier Grover in warm places
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.
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.
Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
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.
Thomson had two pieces of evidence: 1- No matter what metal he used for the disk, the particles produced were indentical. 2- The particles had about 1/2000 the mass of a hydrogen, the lightest atom. These experiments provided the first evidence that atoms are made of even smaller particles.
Thomson had two pieces of evidence: 1- No matter what metal he used for the disk, the particles produced were indentical. 2- The particles had about 1/2000 the mass of a hydrogen, the lightest atom. These experiments provided the first evidence that atoms are made of even smaller particles.
The continental Coastlines fit together like puzzle pieces, fossils, and glacier Grover in warm places
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 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.
Support for Wagner's hypothesis of continental drift includes evidence of fossil records, matching coastlines and geologic formations across continents, and the distribution of certain species that suggest connected landmasses in the past. These pieces of evidence helped bolster the idea that continents were once joined together and have since drifted apart.
There were four peices of evidence: 1. He noticed that the some of the continents fit together like a puzzle. 2. He found the same fossils in both continents, this is only possible if they were once touching each other. 3. There were the same kind of mountains in canada and Europe, the only way this is possible is if the two plates once collided. 4. 250 million years ago there were ice sheets in southern Africa, India, and Australia and this is only possible if they once touched Antartica.
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.
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.
Thomson had two pieces of evidence: 1- No matter what metal he used for the disk, the particles produced were indentical. 2- The particles had about 1/2000 the mass of a hydrogen, the lightest atom. These experiments provided the first evidence that atoms are made of even smaller particles.