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The Metacomet Ridge, Metacomet Ridge Mountains, or Metacomet Range of southern New England is a narrow and steep fault-block mountain ridge known for its extensive cliff faces, scenic vistas, microclimate ecosystems, and rare or endangered plants. The ridge is an important recreation resource located within 10 miles (16 km) of more than 1.5 ...
The following is a list of the more notable summits and sub–ranges that make up the crest of the Metacomet Ridge, a fault-block landform located in Connecticut and Massachusetts, known for its microclimate ecosystems, rare plant communities, scenic vistas, proximity to major urban centers, and recreational opportunities.
Pinnacle Rock, 600 feet (180 m), is a traprock mountain peak located 10 miles (16 km) southwest of Hartford, Connecticut, in the towns of Farmington and Plainville.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.
The Mount Tom Range is a traprock mountain range located in the Connecticut River Valley of Massachusetts.It is a subrange of the Appalachians and part of the Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to nearly the Vermont border.
Long 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 with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick.
Beacon Hill, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The hill formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick.
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