Barberville Falls is a spectacular sight. Above Barberville, the Poesten Kill drains about 35 square miles of the Rensselaer Plateau—an area from Dyken Pond on the north to Taberton on the south. This drainage basin generates a substantial flow of water throughout the year, although the flow is most dramatic in the spring when the snowpack is melting. When it reached the Hudson River at Troy, this same flow of water provided water power for much of that city's early industrial development.
Below the falls, the stream flows through a gorge as deep as 100 feet and 500-1,000 feet wide. The waterfall itself is about 90 feet high and 50-60 feet wide. The main rock at the falls is Rensselear greywacke; above the falls are beds of Nassau slate and limestone.
Before you visit, download a trail map.
In August 2019, The Nature Conservancy transferred the Barberville Falls Preserve to the Rensselaer Plateau Alliance. For more information, visit rensselaerplateau.org/barbervillefalls.