Noctis Labyrinthus on Mars is a region between Valles Marineris and the Tharsis upland. It is one of the most tectonically active regions on the planet, with evidence of faulting, folding, and volcanic activity. The canyons are up to 7 kilometers deep and 200 kilometers wide, with some reaching lengths of over 1,000 kilometers. The canyon network is thought to have formed over billions of years, through a combination of tectonic activity, erosion, and volcanic eruptions.
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