New Hampshire | Capital, Population, Map, History, & Facts

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Presidential Range of the White Mountains3 of 3
Presidential Range of the White MountainsPresidential Range of the White Mountains in autumn, northern New Hampshire.(more)

The basic physical features of New Hampshire are the result of the most recent glacial age (approximately 70,000 to 10,000 years ago), during which the Wisconsin ice sheet moved like a huge bulldozer across New England from the northwest to the southeast. Loose sand, silt, clay, and gravel were deposited as masses of glacial till that, near the town of Greenland, are 395 feet (120 meters) in depth. The mountain notches of New Hampshire—Crawford, Dixville, Franconia, and Pinkham—are the result of the glacial action, as are the potholes and cirques (deep, steep-walled basins on mountains) found in the state. The great glacier left many deltas and hillocks of stratified deposits. The many lakes that dot the New Hampshire countryside are also the results of glacial action; the largest of these is Lake Winnipesaukee in the east-central part of the state.

New Hampshire: Mount Washington
New Hampshire: Mount WashingtonMount Washington in the White Mountains, north-central New Hampshire.(more)

The mountains are the most striking feature of New Hampshire’s landscape. There are about 1,500 classified elevations, including several peaks in the White Mountains, rising above 5,000 feet (1,500 meters) in elevation. The best-known is Mount Washington, at 6,288 feet (1,917 meters) the third highest peak in the country east of the Mississippi River. The mean elevation of the state is about 1,000 feet (300 meters) above sea level.

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