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Crawford Notch

geological formation, New Hampshire, United States

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Crawford Notch is a geological formation in New Hampshire, United States, characterized as a defile or pass within the White Mountains. This scenic area was shaped by glacial action during the last ice age. The pass is traversed by the Saco River and is one of several mountain notches in New Hampshire, including Dixville, Franconia, and Pinkham, all of which are results of glacial activity. The region's landscape, including its mountains and lakes, was significantly formed by the movement of the Wisconsin ice sheet.12

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