The shapes of the continents provide evidence of past tectonic activity, such as the splitting of continents through plate tectonics. For example, the fit of the continents' Coastlines, like the matching shapes of South America and Africa, suggests they were once joined. This helps us understand the movement of Earth's plates over millions of years.
The shapes of the continents suggest that they were once connected as a single landmass known as Pangaea, which later drifted apart due to the movement of tectonic plates. The matching coastlines and geological evidence support the theory of continental drift and plate tectonics.
The shapes of the continents tell us that they were once connected as a single landmass called Pangaea over 200 million years ago. The movement of tectonic plates caused the continents to drift apart to their current positions, creating the geography we see today. This process is known as plate tectonics.
The current shape and position of continents provide evidence for the theory of plate tectonics, which suggests that continents were once part of a supercontinent called Pangaea that has since drifted apart. This movement helps explain the similarities between the geology and fossils of now widely separated continents, as well as the presence of matching coastlines and mountain ranges.
Fossil symbols helped in determining the past connections between continents by showing similarities in species that were now separated by large distances. Mountain belts provided geological evidence of past tectonic activity, such as where two continents may have collided. By studying these clues, scientists were able to infer the movement of continents and reconstruct past supercontinents.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
The shapes of the continents suggest that they were once connected as a single landmass known as Pangaea, which later drifted apart due to the movement of tectonic plates. The matching coastlines and geological evidence support the theory of continental drift and plate tectonics.
The shapes of the continents tell us that they were once connected as a single landmass called Pangaea over 200 million years ago. The movement of tectonic plates caused the continents to drift apart to their current positions, creating the geography we see today. This process is known as plate tectonics.
The current shape and position of continents provide evidence for the theory of plate tectonics, which suggests that continents were once part of a supercontinent called Pangaea that has since drifted apart. This movement helps explain the similarities between the geology and fossils of now widely separated continents, as well as the presence of matching coastlines and mountain ranges.
The shapes of continents do not fit together exactly because they have been moving and shifting over millions of years due to plate tectonics. This movement has caused the continents to break apart and drift apart from each other, resulting in their current shapes. Additionally, erosion and other geological processes have also altered the original shapes of the continents.
shows that all three continents were once connected (joined) together. because the 'exact' same fossil types were found in all three different continents, which are now split from each other.
Fossil symbols helped in determining the past connections between continents by showing similarities in species that were now separated by large distances. Mountain belts provided geological evidence of past tectonic activity, such as where two continents may have collided. By studying these clues, scientists were able to infer the movement of continents and reconstruct past supercontinents.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
Matching geological features like mountain ranges and rock formations on continents that are now separated by oceans. Fossil evidence of the same species found on multiple continents that are now far apart. The alignment of magnetic minerals in rock formations, providing a record of past changes in the Earth's magnetic field and the movement of continents.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!
If "happens now" means present tense, no. Told is the past tense of tell.
Fossil symbols were helpful in deciding where to move the continents because they provided evidence of past connections between landmasses. Similar fossils found on continents that are now far apart suggest that they were once joined together. By using fossil evidence, scientists could determine the past positions of continents and reconstruct ancient supercontinents like Pangaea.
As the continents moved further apart, natural erosion of the Coastlines removed and added to the basic shape over billions of years. Much of the evidence relates to the similarities of plants and animals found on now separate continents. Geological evidence points to Antarctica was once further north and had a tropical climate!