Pistapaug Mountain

Pistapaug Mountain is a summit composed of dark basalt rock that rises 210 meters above the Quinnipiac River valley. The steep slopes display exposed rock formations that give the mountain its dramatic profile.

The basalt rock formed during the Triassic Period when North America separated from Africa and Eurasia through continental rifting. This geologic activity shaped the formation visible today.

The name comes from the Algonquin language and refers to the area's geography. Today, hikers and locals use the mountain for outdoor recreation and seasonal nature study.

Trails are accessible from a parking area on Route 17 located a few kilometers east of town. The paths are best hiked during dry weather and offer varying levels of difficulty.

Different temperatures between the hot upper slopes and cool ravines create specialized plant communities adapted to these conditions. The varying microclimates also attract migrating raptors that use the mountain as a resting point.

Location: Connecticut

Elevation above the sea: 210 m

Made from material: igneous rock

Part of: Metacomet Ridge

GPS coordinates: 41.43176,-72.73704

Latest update: December 14, 2025 14:25