The Pyrenees mountain range, which stretches between France and Spain, is geologically active and experiences movement due to tectonic processes. On average, the range is uplifted by about 1 to 2 millimeters per year as a result of the collision between the Iberian and Eurasian tectonic plates. This movement can vary in different areas of the range and may be influenced by factors such as erosion and seismic activity.
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