Nepaug Phelps Dam, also known as Nepaug Reservoir, is a historic masonry dam located in Burlington, Connecticut, along the Farmington River.
Wind
Humidity
Built in 1916, this dam serves a primary purpose of water supply, with a storage capacity of 40,540 acre-feet and a normal storage of 29,300 acre-feet. Covering an area of 850 acres and draining a watershed of 31.9 square miles, this dam plays a crucial role in water resource management in the region.
With a height of 67 feet and a length of 1250 feet, Nepaug Phelps Dam stands as a significant structure in the state, regulated by the Department of Energy and Environmental Protection (DEEP). It has a fair condition assessment and a high hazard potential, making regular inspections and maintenance crucial. The dam features a valve outlet gate and is associated with two other structures, contributing to the overall water management system in the area.
For water resource and climate enthusiasts, Nepaug Phelps Dam presents a fascinating example of early 20th-century engineering designed to meet the water supply needs of the community. Its location in the picturesque Hartford County adds to its allure, while its historical significance and ongoing regulatory oversight highlight the importance of sustainable dam operations in the face of changing environmental conditions. As a key component of the local water infrastructure, Nepaug Phelps Dam continues to play a vital role in ensuring a reliable water supply for Unionville and beyond.
Year Completed |
1916 |
Dam Length |
1250 |
Dam Height |
67 |
River Or Stream |
FARMINGTON RIVER TR |
Primary Dam Type |
Masonry |
Surface Area |
850 |
Drainage Area |
31.9 |
Nid Storage |
40540 |
Outlet Gates |
Valve |
Hazard Potential |
High |
Foundations |
Rock |
Nid Height |
67 |
Begins Below The Tailrace Of The Lower Collinsville Dam To The Route 187 Bridge
The Confluence With The Nepaug River To A Point 0.2 Miles Below The Lower Collinsville Dam Tailrace
New Hartford/Canton Town Line To The Confluence With The Nepaug River
The Hartland Headwaters To The Confluence With The Salmon Brook Main Stem