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The Paleozoic sediments present a gentle dip of approximately 4° towards the west. The flat-topped plateau characterizing much of Devon Island's surface is an old erosional surface (peneplain) exposing sediments of increasing age towards the east. Devon Island is home to one of the highest-latitude impact structures known on Earth, Haughton Crater. At 20 kilometers in diameter the crater formed 23 million years ago, at the beginning of the Miocene, when an asteroid or a comet collided with our planet.
Little imagination is required to believe oneself on Mars when exploring Devon Island. Many features and sites there are strikingly reminiscent of the Martian landscape, from barren rocky blockfields to intricate valley networks, from precipitous winding canyons to recent gully systems on their slopes...
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