Hanging Hills | |
---|---|
Metacomet Ridge | |
Highest point | |
Peak | West Peak |
Elevation | 1,024 ft (312 m) |
Dimensions | |
Length | 3 mi (4.8 km) east-west |
Geography | |
Country | United States |
State | Connecticut |
Range coordinates | 41°33.45′N 72°49.4′W / 41.55750°N 72.8233°W |
Geology | |
Rock age(s) | Triassic and Jurassic |
Rock type(s) | fault-block, igneous and sedimentary |
The Hanging Hills of south central Connecticut, United States, are a range of mountainous trap rock ridges overlooking the city of Meriden and the Quinnipiac River Valley 900 feet (274 m) below. They are a subrange 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. The range is also a subrange of the Appalachian Mountains. A popular outdoor recreation resource, the range is known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that rise abruptly over 700 feet (213 m) above the surrounding landscape.[1] The Hanging Hills encompass the 1,800-acre (7.3 km2) Hubbard Park, designed with the help of landscape architect Frederick Law Olmsted.[2] The 51 mile (80k) Metacomet Trail traverses the range.