Pinkham Notch
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. Pinkham Notch was eroded into a glacial U-shaped valley whose walls are formed by the Presidential, Wildcat, and Carter-Moriah ranges. Due to the volatility of the area's climate and rugged character of the terrain, a number of rare or endemic ecosystems have developed throughout the notch.
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Pinkham Notch
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. Pinkham Notch was eroded into a glacial U-shaped valley whose walls are formed by the Presidential, Wildcat, and Carter-Moriah ranges. Due to the volatility of the area's climate and rugged character of the terrain, a number of rare or endemic ecosystems have developed throughout the notch.
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Pinkham Notch (elevation 2032 ...... t a hub for hiking and skiing.
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Pinkham Notch
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Wikipage page ID
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720,106,691
elevation ft
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The steep, glaciated walls of Pinkham Notch can be seen in this topographic map.
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USGS Stairs Mountain, Jackson, Carter Dome, Mount Washington
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44.2576 -71.2537
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Pinkham Notch (elevation 2032 ...... eveloped throughout the notch.
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Pinkham Notch
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4.42576e+1
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-7.12537e+1