Draft:Van Cleef Lake
Submission declined on 22 November 2025 by Hurricane Wind and Fire (talk).
Where to get help
How to improve a draft
You can also browse Wikipedia:Featured articles and Wikipedia:Good articles to find examples of Wikipedia's best writing on topics similar to your proposed article. Improving your odds of a speedy review To improve your odds of a faster review, tag your draft with relevant WikiProject tags using the button below. This will let reviewers know a new draft has been submitted in their area of interest. For instance, if you wrote about a female astronomer, you would want to add the Biography, Astronomy, and Women scientists tags. Editor resources
|
Comment: Hello. Most of the sources are affiliated with the subject in some way, not counting towards the notability guideline. Before resubmission, find more reliable sources that are independent of the subject to establish notability. 🌀Hurricane Wind and Fire (talk) (contribs)🔥 04:54, 22 November 2025 (UTC)

Van Cleef Lake
Van Cleef Lake is a man-made lake located in the Town of Seneca Falls in Seneca County, New York, United States. The lake was created in 1915 as part of a hydroelectric and flood-control project on the Seneca River and the Cayuga–Seneca Canal, following the construction of a concrete dam that impounded the former river channel.[1]
The lake lies within the central business district of Seneca Falls and is crossed by several bridges and canal structures. It forms a segment of the New York State Canal System and is used for recreational boating, sightseeing, and community events.[2]
Van Cleef Lake also helps regulate water flow between Cayuga Lake and the Erie Canal, ensuring reliable navigation levels throughout the canal season.[3]
Dimensions
Van Cleef Lake measures approximately 0.5 miles (0.80 km) from east to west and between 300 and 900 feet (91–274 m) wide depending on the section. Its surface area is roughly 40 acres, though the exact size varies with seasonal canal levels.[4]
Depths range from 12 ft in the shallower western end to approximately 50 ft near the dam, which contains the deepest portion of the lake where the original river channel descended sharply toward bedrock.[5]
Pre-Impoundment Geography and Former River Features
Before the construction of the Seneca Falls dam in 1915, the Seneca River flowed through a series of natural rapids and small waterfalls along the channel that is now submerged beneath Van Cleef Lake. These rapids gave the village its name and provided waterpower for early mills and factories.[6]
The low-lying area along the riverbank, later submerged, was a working-class neighborhood known as “The Flats.” It contained industrial buildings, boarding houses, warehouses, and canal-related structures. When the hydroelectric dam and realigned Cayuga–Seneca Canal were built, much of The Flats and the former river channel were inundated. Buildings were removed or demolished, and the remaining terrain became part of the lake floor.
The pre-1915 river channel was narrower, faster, and steeper than the present impoundment. The transformation fundamentally altered the hydrology of the area, converting the Seneca River from a shallow, fast-flowing stretch with multiple cascades into a deep, slow-moving lake suitable for navigation and hydroelectric power.
Depth and Submerged Structures
Historical engineering records indicate that Van Cleef Lake varies in depth from 12 ft to 50 ft, with the deepest point near the dam.[7]
Structures submerged after the lake’s creation include:
Sections of original Cayuga–Seneca Canal locks[8]
Mill and pump factory foundations (Goulds, Silsby, Rumsey)[9]
Streets, rail spurs, and part of the pre-1915 riverbank grid
During low-water periods, portions of one historic stone lock have been exposed.[10]
Access and Boat Launches
The main public boat launch for trailered vessels is located on the Cayuga–Seneca Canal at approximately 42.9097° N, 76.8026° W, maintained by the New York State DEC.[11]
Additional hand-launch sites for kayaks and paddleboards are located at the Seneca Falls Recreation Center at 35 Water Street, providing direct access to the canal and lake.[12]
Boaters may also enter the lake via the Seneca Falls Harbor on the canal.[13]
Cultural Significance
The Trinity Episcopal Church, situated on the lake’s northern shore, is widely regarded as one of the most photographed historic churches in New York State. Its lakeside setting and Gothic Revival architecture have made it a signature landmark of the village and a popular subject in tourism materials and canalway photography.[14]
References
[edit]- ^ Seneca Falls Power Plant and Dam Assessment (Report). Town of Seneca Falls. 2019.
- ^ "Cayuga–Seneca Canal Navigation Charts". New York State Canal Corporation. Retrieved 2025-01-01.
- ^ New York State Canal System Historic Structure Inventory (Report). U.S. Army Corps of Engineers. 2018.
- ^ Seneca Falls Power Plant and Dam Assessment (Report). Town of Seneca Falls. 2019.
- ^ Seneca Falls Power Plant and Dam Assessment (Report). Town of Seneca Falls. 2019.
- ^ Administrative History of Women's Rights National Historical Park (Report). National Park Service. 2012.
- ^ Seneca Falls Power Plant and Dam Assessment (Report). Town of Seneca Falls. 2019.
- ^ Erie Canalway National Heritage Corridor: NRHP Documentation (Report). National Park Service. 2014.
- ^ Administrative History of Women's Rights National Historical Park (Report). National Park Service. 2012.
- ^ "Seneca Falls Village Historic District". National Register of Historic Places. Retrieved 2025-01-01.
- ^ "Seneca County Boat Launch Sites". New York State Department of Environmental Conservation. Retrieved 2025-01-01.
- ^ "Seneca Falls Waterfront Access". Seneca Falls Development Corporation. Retrieved 2025-01-01.
- ^ "Seneca Falls Harbor". Marinas.com. Retrieved 2025-01-01.
- ^ "History – Trinity Church Seneca Falls". Trinity Episcopal Church (Seneca Falls). 29 August 2012. Retrieved 2025-11-14.

- in-depth (not just passing mentions about the subject)
- reliable
- secondary
- independent of the subject
Make sure you add references that meet these criteria before resubmitting. Learn about mistakes to avoid when addressing this issue. If no additional references exist, the subject is not suitable for Wikipedia.