Jump to content

Bare Mountain (Massachusetts)

Coordinates: 42°18′11″N 72°31′48″W / 42.30306°N 72.53000°W / 42.30306; -72.53000
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Backspace (talk | contribs) at 04:05, 31 December 2009 (To provide a category). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Alternate spelling: should not be confused with Bear Mountain.
Bare Mountain
Map

Bare Mountain, 1,014 feet (309 m) above sea level, is a prominent peak of the Holyoke Range of traprock mountains located in the Connecticut River Valley of Massachusetts, and part of the greater Metacomet Ridge that stretches from Long Island Sound to nearly the Vermont border. The peak rises steeply from the river valley 1,000 feet (300 m) below; its bald summit offers sweeping views. Bare Mountain is located within the towns of Amherst and South Hadley, Massachusetts and is traversed by the 110-mile (180 km) Metacomet-Monadnock Trail.

Description and history

A hiking destination popular among local college students, Bare Mountain offers a 270° vista over the surrounding valleys to the north and south, and a bird's eye view across Mount Norwottuck and the eastern peaks of the Holyoke Range. Also visible from the top are the Round Mountain quarry and the campus of the University of Massachusetts, Amherst. A prime example of a basalt talus slope is located on the east side of the mountain, along the Metacomet-Monadnock Trail.

The Five Colleges Library Depository is located on the north side of the mountain, within a subterranean bunker formerly occupied by the United States Air Force Strategic Air Command. (See The Notch.)

Geology and ecology

Talus slope on Bare Mountain

Bare Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The mountain formed near the end of the Triassic Period when North America was rifting apart from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the dramatic cliffs and ridges of Bare Mountain. Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Massachusetts. (See Metacomet Ridge for more information on the geology and ecosystem of Bare Mountain.

See also

< West East >
Seven Sisters
(no image)
Mount Norwottuck

References