Taconic Mountains
The Taconic Mountains (/təˈkɒnɪk/) are a 150-mile-long sub-range of the Appalachian Mountains lying on the eastern border of New York State and adjacent New England. The range, which played a role in the history of geological science, is separated from the Berkshires and Green Mountains to the east by a series of valleys, principally those of the Housatonic River, Battenkill River and Otter Creek. The Taconics' highest point is Mount Equinox in Vermont at 3,840 feet (1,170 m); among many other summits are Dorset Mountain, Mount Greylock and Mount Everett.
Taconic Mountains | |
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Mount Equinox (3,840 ft) in Vermont is the high point of the Taconic range | |
Highest point | |
Peak | Equinox Mountain, Bennington County, Vermont |
Elevation | 3,850 ft (1,170 m) |
Geography | |
Orogenies of the northeast United States
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Country | United States |
State | New York, Connecticut, Massachusetts, Vermont |
Region | western New England, eastern New York |
Range coordinates | 42°41.5′N 73°17.1′W |
Parent range | Appalachian Mountains |
Biome | Northern hardwood forest, |
Geology | |
Orogeny | Taconic Orogeny |
Age of rock | 440 million years |
Type of rock | Thrust fault |
Forests are predominately maple-beech-birch with some spruce-fir at higher elevations, "and oak and hickory common to the south and at lower elevations." The area is part of the New England-Acadian forests ecoregion. Although mostly private property, the Taconics contain a half-dozen sizable state forests and parks, as well as many preserves of lesser acreage protected by land trusts. Several hundred miles of trails are within these mountains, including parts of the Appalachian Trail.