Bradley Mountain

Bradley Mountain is a summit in Connecticut that rises approximately 700 feet above sea level and features steep basalt rock cliffs along its slopes. The ridgeline contains multiple peaks offering views across the Quinnipiac River valley and connecting to surrounding hiking areas.

The mountain formed during the Triassic Period through volcanic activity and continental rifting that shaped the traprock ridges of the Metacomet Range. These geological events created the distinctive rock formations visible today along the summit and slopes.

The mountain was historically used by indigenous peoples as a travel route and seasonal settlement site before European colonization arrived in Connecticut. Visitors walking the trails today move along paths that echo these ancient patterns of movement through the landscape.

The Metacomet Trail crosses the mountain and provides hikers access to panoramic views and connections to other areas within the regional trail network. The path is most comfortable to walk during drier months when the ground is more stable.

The volcanic composition creates specialized microclimates that support rare plant species found nowhere else in the surrounding region. These conditions also provide critical habitats for migratory birds of prey during their seasonal movements through the area.

Location: Connecticut

Made from material: igneous rock

Part of: Metacomet Ridge

GPS coordinates: 41.65760,-72.83760

Latest update: December 13, 2025 17:04