The park's namesake, Buttermilk Falls, is a result of the creek falling over layers of soft shale and harder siltstone.
The park contains a natural swimming pool at the base of the falls which is monitored by lifeguards during the summer season.
The Gorge Trail features over 500 stone stairs carved into the landscape to navigate the steep elevation gain.
The park is part of a series of 'gorge parks' in the Ithaca area formed by post-glacial stream erosion.
The upper portion of the park, known as Lake Treman, was created by an earthen dam built in the early 20th century.
Buttermilk Falls State Park is defined by a 500-foot cascading drop formed by Buttermilk Creek as it descends into the Cayuga Lake valley. The park features a steep gorge trail that connects the lower falls with an upper park area containing a series of smaller cascades and natural swimming pools. The terrain rises rapidly, resulting in a dramatic change in elevation over a short horizontal distance. The park includes ten distinct waterfalls along its primary watercourse. Facilities include a swimming area at the base, picnic grounds, and multiple hiking trails that connect to the Finger Lakes Trail system. The geological composition consists of Devonian-era shale and sandstone, which creates the stair-step effect of the falls.
The viewing platform at the base of the main waterfall looking upward.
Wear footwear with significant grip, as the stone steps and gorge trails are frequently wet and slippery.
Check official New York State Parks updates before arriving, as high water levels or storm damage can trigger trail closures.
Visit the upper park area for a flatter, more wooded hiking experience away from the main waterfall crowd.
Attempting to swim in the gorge pools outside of the designated, lifeguard-monitored area at the base.
Swimming is limited to the summer season only; upper trails may close during winter due to icy conditions.
Stay on marked trails to protect the fragile shale gorge walls and follow 'Leave No Trace' principles.
