Final answer:
The Appalachian Mountains and the Caledonian Mountains provide evidence for plate tectonics through similar rock formations and the movement of the plates.
Step-by-step explanation:
The Appalachian Mountains in North America and the Caledonian Mountains in Greenland and Northern Europe provide evidence that supports the theory of plate tectonics. These mountain ranges, though separated by oceans and seas over many miles, contain many of the same distinctive rock formations, landforms, and glacial sequences. Additionally, both mountain ranges formed as magma from Earth's mantle flowed to the surface at the same mid-ocean ridge. This supports the idea that the plates beneath these mountain ranges were once connected and have since moved apart.
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