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Map of the White Mountains, Franklin Leavitt, 1871. Some of the earliest maps of the White Mountains were produced as tourist maps and not topographical maps. One of the first two tourist maps of the mountains was that produced by Franklin Leavitt, a self-taught artist born near Lancaster, New Hampshire in 1824. [4]
In this 2018 map by the N.H. Department of Transportation, the White Mountains region is located in the north-central portion of New Hampshire, colored orange in this map. The White Mountains Region is a tourism region designated by the New Hampshire Division of Travel and Tourism. [1]
Covered bridge near the Flume A hiking trail through Franconia Notch The Basin. Franconia Notch State Park is a public recreation area and nature preserve that straddles eight miles (13 km) of Interstate 93 as it passes through Franconia Notch, a mountain pass between the Kinsman Range and Franconia Range in the White Mountains of northern New Hampshire, United States.
Located along the Ellis River in the White Mountain National Forest, this 64-foot-tall waterfall is located at the end of a short 0.4 mile walk along the wooded trail, with a few steps to navigate ...
Polar Caves Park is a set of glacially-formed talus caves located in New Hampshire's White Mountains region, in the United States. [1] The caves were formed during the last ice age from granite boulders and are so named because the deepest cave is cold enough to allow snow to linger long into the summer. [2] The caves are a popular tourist ...
Franconia Notch (elev. 1,950 feet/590 m) is a major mountain pass through the White Mountains of New Hampshire. Dominated by Cannon Mountain to the west and Mount Lafayette to the east, it lies principally within Franconia Notch State Park and is traversed by the Franconia Notch Parkway (Interstate 93 and U.S. Route 3).
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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.
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