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Pinkham Notch (elevation 2032 ft. / 619 m) is a mountain pass in the White Mountains of north-central New Hampshire, United States. The notch is a result of extensive erosion by the Laurentide Ice Sheet during the Wisconsinian ice age .
The Presidential Range is notorious for having some of the worst weather on Earth, mainly because of the unpredictability of high wind speeds and whiteout conditions on the higher summits. Because of the poor weather conditions, the Presidential Range is often used for mountaineering training for those who go on to climb some of the world's ...
The most common hiking trail approach to the summit is via the 4.1-mile (6.6 km) Tuckerman Ravine Trail. It starts at the Pinkham Notch camp area and gains 4,280 feet (1,300 m), leading straight up the bowl of Tuckerman Ravine [48] via a series of steep rock steps that afford views of the ravine and across the notch to Wildcat Mountain.
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The ravine is named after botanist Edward Tuckerman who studied alpine plants and lichens in the area in the 1830s and 1840s. According to the New England Ski Museum, the first recorded use of skis on Mount Washington was by a Dr. Wiskott of Breslau, Germany, who skied on the mountain in 1899, while the first skier in Tuckerman Ravine was John S. Apperson of Schenectady, New York, in April 1914.
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Kinsman Notch (elev. 1,870 feet (570 m) [1]) is a mountain pass located in the White Mountains of New Hampshire, United States. [ 2 ] [ 3 ] It is the westernmost of the major notches through the White Mountains (the others being Franconia Notch , Crawford Notch , and Pinkham Notch ).
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