Chauncey Peak

Chauncey Peak rises 688 feet above sea level, featuring vertical cliff faces that overlook Bradley Hubbard Reservoir and create distinct microclimates along its slopes.

The mountain formation dates back 200 million years when North America's rifting caused basalt lava flows, resulting in the current traprock mountain structure.

Local hiking communities gather at Giuffrida Park to explore the Mattabesett Trail, which spans 50 miles and connects multiple natural landmarks across the region.

The western slope offers marked trails for hiking and snowshoeing, while the eastern section requires caution due to active quarrying operations.

The mountain's geography creates two separate drainage systems, with the western half flowing to Long Island Sound and the eastern half to the Connecticut River.

Location: Connecticut

Made from material: igneous rock

Part of: Metacomet Ridge

GPS coordinates: 41.55843,-72.75954

Latest update: March 17, 2025 20:06