Chauncey Peak

Chauncey Peak is a mountain summit in Connecticut featuring steep rocky cliffs that rise above Bradley Hubbard Reservoir. The varying elevations along its slopes create different environments with distinct plant life and weather conditions.

The mountain formed approximately 200 million years ago during the rifting of North America when basalt lava flows shaped what is now the traprock mountain structure. This volcanic activity established the geological features visible throughout the area today.

Local hiking groups use Giuffrida Park as a starting point to explore trails that connect several natural areas in the region. The location has become an important gathering spot for people interested in outdoor activities and nature.

The western side offers marked hiking trails and snowshoeing paths, while the eastern side requires caution due to active quarry operations. It is important to stay on marked trails and avoid quarry work areas.

The mountain divides water into two separate directions, with the western half flowing toward Long Island Sound and the eastern half flowing toward the Connecticut River. This natural watershed demonstrates the geological diversity of the peak in a subtle way.