Ragged Mountain is a 761-foot traprock ridge in central Connecticut, west of New Britain in Southington and Berlin, and part of the Metacomet Ridge. Rising steeply above the Quinnipiac River valley, it is known for broad views, cliffs, ledges, reservoirs, and varied microclimates created by its basalt geology. Formed near the end of the Triassic Period as faulting tilted ancient lava flows, the ridge supports uncommon plant and animal communities and serves as a raptor migration path. It is also one of Connecticut’s best-known recreation areas, especially for hiking and climbing, with much of the mountain protected through watershed, preserve, and conservation efforts.