The waterfall is 215 feet tall, making it one of the highest free-falling waterfalls in the Northeastern United States.
The name 'Taughannock' is derived from the Delaware word for 'great fall in the woods'.
The bedrock exposed in the gorge walls dates back to the Middle and Upper Devonian period, approximately 380 million years ago.
The park contains a 19th-century hotel site that was once a destination for Victorian-era tourists.
The gorge is a deep, narrow canyon formed by the post-glacial erosion of Taughannock Creek into the plateau.
The park is situated within the Finger Lakes region, a series of long, narrow lakes formed by glacial scouring.
Taughannock Falls State Park centers on a 215-foot plunge waterfall that is three stories taller than Niagara Falls. The gorge is carved through layers of Devonian-era shale, siltstone, and sandstone. The primary Gorge Trail is a flat, 0.75-mile path leading to the base of the waterfall. An additional North Rim and South Rim trail network provides views from the top of the gorge cliffs. The park grounds extend to the shores of Cayuga Lake, featuring a marina and a swimming beach. The waterfall originates from Taughannock Creek, which flows into the Finger Lakes watershed. Geologically, the waterfall formed as the creek cut through the plateau after the retreat of glacial ice. Public facilities include picnic areas, a playground, and a seasonal snack bar near the lakefront.
The observation platform located at the end of the Gorge Trail provides an direct, head-on view of the waterfall base.
Use the upper viewing area near the visitor center for a panoramic view of the falls without the hike.
The Gorge Trail is flat and gravel-surfaced, making it accessible for most strollers and wheelchairs.
Visit the lakefront area to escape the crowds often found at the main waterfall trail.
Attempting to climb the shale gorge walls, which is hazardous due to loose rock and strictly prohibited.
Trails may be subject to seasonal closures during winter months due to ice and hazardous conditions; check local status for flooding or trail maintenance.
Stay on marked trails to prevent erosion of the fragile gorge walls and strictly adhere to no-swimming rules in the gorge basin.
