Distinctive rock strata provide evidence for continental drift by showing similar geological formations, ages, and fossil types across continents that are now widely separated. For instance, identical sedimentary layers and mountain ranges found on different continents suggest they were once connected. This correlation in rock strata supports the idea that continents have moved apart over time, consistent with the theory of plate tectonics. Additionally, matching fossil records in these strata reinforce the notion of a shared geological history.
Distinctive rock strata provide crucial evidence for the theory of continental drift by showing similarities in geological formations across distant continents. For instance, identical sequences of rock layers and fossilized remains found in South America and Africa suggest that these landmasses were once connected. Additionally, similar age and composition of rocks across continents support the idea that they were part of a single supercontinent, Pangaea, before drifting apart. This geological continuity underscores the concept that continents have moved over geological time, aligning with the principles of continental drift.
Distinctive rock strata found on different continents provide compelling evidence for the theory of continental drift by demonstrating that these landmasses were once connected. Similar rock formations, fossil records, and geological structures, such as mountain ranges, can be found on continents that are now separated by vast oceans. This alignment suggests that these continents have drifted apart over time, supporting the idea of a dynamic Earth where landmasses shift due to tectonic activity. Additionally, the age and composition of these rock strata often correlate, reinforcing the concept of a unified geological history.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
I think that continetal drift replaced his theory
It supports the theory because it can be found on all of the continents.
Since you can find the same distinctive rock strata in both the east coast of South America and the west coast of Africa, it suggests that those two coasts were once connected.
Distinctive rock strata provide crucial evidence for the theory of continental drift by showing similarities in geological formations across distant continents. For instance, identical sequences of rock layers and fossilized remains found in South America and Africa suggest that these landmasses were once connected. Additionally, similar age and composition of rocks across continents support the idea that they were part of a single supercontinent, Pangaea, before drifting apart. This geological continuity underscores the concept that continents have moved over geological time, aligning with the principles of continental drift.
Rock strata that match on different continents suggest that these continents were once connected and have since drifted apart. Fossils and geological formations found in these rock layers further support the theory of continental drift by indicating past connections between continents that are now separated. Matching rock strata across continents provide evidence of a shared history and movement of land masses over time.
Distinctive rock strata found on different continents provide compelling evidence for the theory of continental drift by demonstrating that these landmasses were once connected. Similar rock formations, fossil records, and geological structures, such as mountain ranges, can be found on continents that are now separated by vast oceans. This alignment suggests that these continents have drifted apart over time, supporting the idea of a dynamic Earth where landmasses shift due to tectonic activity. Additionally, the age and composition of these rock strata often correlate, reinforcing the concept of a unified geological history.
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
Alfred Wegener's support of continental drift was known as the theory of "continental drift," which proposed that the continents were once joined together as a single supercontinent called Pangaea and have since drifted apart.
they couldn't agree on how it separated or what made it separate.
Glossopteris
composition of meteorites
Digestive rocks strata contain evidence of the Earth's past magnetic field orientation. By studying these magnetic patterns, scientists can determine the original location of the rock from when it was formed. This data supports the theory of continental drift by showing that continents were once joined together and have since moved apart.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
yes it does.