Bare Mountain (Massachusetts)
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- Alternate spelling: should not be confused with Bear Mountain.
| Bare Mountain (Massachusetts) | |
|---|---|
 View from the summit of Bare Mountain |
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| Elevation | 1,014 feet (309 m) |
| Location | Amherst and South Hadley, Massachusetts. |
| Range | Holyoke Range / Metacomet Ridge |
| Coordinates | Coordinates: |
| Type | Fault-block; igneous |
| Age of rock | 200 million yrs. |
| Easiest route | Metacomet-Monadnock Trail |
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 (305 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 mi (177 km) Metacomet-Monadnock Trail.
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[edit] Description and history
A hiking destination popular among local college students, Bare Mountain offers a 270-degree 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.
[edit] Geology and ecology
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]].
[edit] See also
- Bare Mountain is also the name of several other mountains in the United States.
- Should not be confused with Bear Mountain, the name of more than 70 peaks in the United States alone, including two in Massachusetts.
- Metacomet Ridge
- Robert Frost Trail (Massachusetts)
- Metacomet-Monadnock Trail
- Adjacent summits:
| < West | East > | |
|---|---|---|
| Seven Sisters (no image) |
[edit] References
- Farnsworth, Elizabeth J. "Metacomet-Mattabesett Trail Natural Resource Assessment." 2004. PDF file. Cited Nov. 20, 2007.
- "Amherst College Library Chronology". Cited from web Dec. 2, 2007.
- The Metacomet-Monadnock Trail Guide. 9th Edition. The Appalachian Mountain Club. Amherst, Massachusetts, 1999.
- Mt. Holyoke Range Historical Timeline. Cited from web Dec. 2, 2007.
- Raymo, Chet and Maureen E. Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut, 1989.
[edit] External links
- J.A. Skinner State Park Map
- Mount Holyoke Range State Park map
- Hampshire College mountain biking map of the Holyoke Range
- Bershire Chapter of the Appalachian Mountain Club
- The Kestrel Trust
- The Valley Land Fund
- Friends of the Mount Holyoke Range
- Natural resource assessment of the Metacomet Ridge
- Geology of the northern Metacomet Ridge region
- State website for Skinner State Park
