They are lined up if you put them together.
An example of rock and mountain correlation in the theory of continental drift is the Appalachian Mountains in the eastern United States and the Caledonian Mountains in Scotland and Scandinavia. Both mountain ranges share similar rock formations and structures, providing evidence that these regions were once connected before the continents drifted apart.
The Caledonian and Appalachian mountains are similar in that they both were formed during the same geological period, specifically during the Paleozoic Era, through the process of continental collision and plate tectonics. They share a similar geological composition, consisting primarily of ancient rocks and sediments that have been heavily eroded over time. Additionally, both mountain ranges exhibit similar structural features and are remnants of ancient mountain chains that have undergone significant geological transformation.
The appalachian Mountain range
Appalachian Mountain Range
Appalachian and Rocky Mountains
The Appalachian mountain range, which parallels the eastern seaboard of the continental US.
Rock types can provide evidence of continental drift by matching on opposite sides of current oceans, showing that the continents were once connected. For example, the Appalachian Mountains in North America align with the Caledonian Mountains in Scotland, indicating they were once part of the same mountain range before continental drift occurred. Additionally, similar fossils and rock formations found on different continents support the theory of continental drift.
It is the Appalachian Mountians. Which consist of: Taconic Orogeny (Ordovician);Acadian Orogeny (Devonian);Caledonian Orogeny (Silurian); Allegheny Orogeny (Pennsylvanian & Permian).
Appalachian, the oldest mountain range in the US
The correct spelling is "Appalachian" mountain.
Appalachian
The Appalachian Mountains are the major mountain range in the Eastern US.