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.
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.
No
The shapes of continents appearing on the map clearly show similar shapes and how the continents might fit together.
It supports the theory because it can be found on all of the continents.
In every way.
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 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.
It should be Alfred Wegener
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.
A German scientist Alfred Wegener first proposed the idea of Continental Drift.
It's an ism! Terry
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.
character.
It is generally thought to support the Theory of Evolution.
Nicolas Steno is that sedimentary strata had been deposited in former seas, and that fossils are organic in origin..((((((:<3
Red shift does not support the steady state theory.
No