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Wachusett Reservoir information


Wachusett Reservoir
Wachusett Reservoir and Dam from above Clinton, Massachusetts
Location of Wachusett Reservoir in Massachusetts, USA.
Location of Wachusett Reservoir in Massachusetts, USA.
Wachusett Reservoir
Location of Wachusett Reservoir in Massachusetts, USA.
Location of Wachusett Reservoir in Massachusetts, USA.
Wachusett Reservoir
LocationWorcester County, Massachusetts, United States
Coordinates42°22′10″N 71°44′18″W / 42.36944°N 71.73833°W / 42.36944; -71.73833
TypeReservoir
Primary inflowsQuinapoxet River, Stillwater River, Quabbin Aqueduct
Primary outflowsWachusett Aqueduct, Cosgrove Tunnel, South Nashua River
Catchment area108 sq mi (280 km2)
Basin countriesUnited States
Max. length7 mi (11 km)
Max. width1.1 mi (1.8 km)
Surface area7 sq mi (18 km2)
Average depth48 ft (15 m)
Max. depth120 ft (37 m)
Water volume65,000,000,000 US gal (0.25 km3)
Shore length121 mi (34 km)
Surface elevation384 ft (117 m)[1]
SettlementsClinton, West Boylston, Boylston, Sterling
1 Shore length is not a well-defined measure.

The Wachusett Reservoir is the second largest body of water in the state of Massachusetts. It is located in central Massachusetts, northeast of Worcester. It is part of the water supply system for metropolitan Boston maintained by the Massachusetts Water Resources Authority (MWRA). It has an aggregate capacity of 65 billion US gallons (250,000,000 m3) and an area of almost 7 square miles (18 km2). Water from the reservoir flows to the covered Norumbega Storage Facility via the Cosgrove Tunnel and the MetroWest Water Supply Tunnel. The reservoir has a maximum depth of 120 feet (37 m) and a mean depth of 48 feet (15 m).

The reservoir serves as both an intermediate storage reservoir for water from the Quabbin Reservoir, and a water source itself, fed by its own watershed. The reservoir is fed by the Quinapoxet and Stillwater rivers, along with the Quabbin Aqueduct, which carries water from the Quabbin Reservoir. It is part of the Nashua River watershed, forming the headwaters of the river. Because it is an intermediate storage reservoir, its water levels are kept relatively constant while the Quabbin Reservoir fluctuates based on precipitation and demand. At times when the Wachusett Reservoir becomes high due to its own watershed producing a large amount of runoff such as during snow melting, the flow from the Quabbin is shut off and water from the Ware River flows backwards down the Quabbin Aqueduct into the Quabbin Reservoir for storage.

  1. ^ "Wachusett Reservoir". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.

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