Fowler Mountain

Fowler Mountain is a summit in Connecticut with steep slopes formed from basalt, rising to an elevation of 230 meters above sea level. The Mattabesett Trail crosses through the ridge, guiding hikers across exposed rock formations and forested sections.

This summit formed during the Triassic Period when continental rifting separated North America from Africa and Eurasia. The resulting geological upheaval created the basalt formations that define the mountain's character today.

The mountain serves as a gathering place for outdoor enthusiasts who hike its trails throughout the year. These paths connect the surrounding communities and remain central to how locals experience the region's natural spaces.

Access to the mountain is provided through Trimountain State Park with marked hiking trails available year-round. Weather conditions can change quickly due to the elevation and exposed ridge sections, so visitors should come prepared for variable conditions.

The mountain's elevation changes create distinct microclimates across its slopes, from dry upper sections to cool ravines below. These varying conditions support specialized plant communities adapted to their particular pockets of the landscape.

Location: Connecticut

Elevation above the sea: 230 m

Made from material: igneous rock

Part of: Metacomet Ridge

GPS coordinates: 41.44288,-72.74093

Latest update: December 14, 2025 15:02