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Rattlesnake Mountain (Connecticut)

Rattlesnake Mountain
Ct rattle west.jpg
View from Rattlesnake Mountain
Highest point
Elevation 750 ft (230 m) 
Parent peak 41° 41' 59"N, 72° 49' 58"W
Coordinates 41°41′59″N 72°49′58″W / 41.69972°N 72.83278°W / 41.69972; -72.83278Coordinates: 41°41′59″N 72°49′58″W / 41.69972°N 72.83278°W / 41.69972; -72.83278
Geography
Location Farmington, Connecticut
Parent range Metacomet Ridge
Geology
Age of rock 200 Ma
Mountain type Fault-block; igneous
Climbing
Easiest route Metacomet Trail

Rattlesnake Mountain is a traprock mountain, 750 feet (230 m) above sea level, located 9 miles (14 km) southwest of Hartford, Connecticut in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Rattlesnake Mountain, a popular outdoor recreation resource of the metropolitan Hartford area, is known for its cliff-top scenic vistas, unique microclimate ecosystems, and rare plant communities. Will Warren's Den, a boulder cave located on the mountain, is a local historic site. Rattlesnake Mountain is traversed by the 51-mile (82 km) Metacomet Trail.

Roughly 1 mile (1.6 km) in diameter, Rattlesnake Mountain rises steeply 500 feet (150 m) above the Farmington River valley to the west. The mountain consists of an upper summit cone that descends into a series of tiered ridges which become contiguous with the Metacomet Ridge on Pinnacle Rock to the south and Farmington Mountain to the north.

A small traprock quarry, 0.4 miles (600 m) wide, occupies the northeast side of the mountain, and a suburban development the southwest side. Two broadcasting towers (WTIC-TV and WVIT) stand on the summit.

The east side of Rattlesnake Mountain drains into Trout Brook, then to the Park River, thence into the Connecticut River and Long Island Sound; the west side into the Pequabuck River, then to the Farmington River, thence to the Connecticut River. The south side of the mountain supports the headwaters of the Quinnipiac River, which flows directly into Long Island Sound.


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Wikipedia

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