Total streamflow across the Shetucket River was last observed at 2,015 cfs, and is expected to yield approximately 3,997 acre-ft of water today; about 85% of normal. Average streamflow for this time of year is 2,374 cfs, with recent peaks last observed on 2021-07-10 when daily discharge volume was observed at 19,310 cfs.

Maximum discharge along the river is currently at the Shetucket River At Taftville reporting a streamflow rate of 1,070 cfs. This is also the highest stage along the Shetucket River, with a gauge stage of 6.66 ft at this location. This river is monitored from 2 different streamgauging stations along the Shetucket River, the highest being situated at an altitude of 156 ft, the Shetucket River Near Willimantic.

The Shetucket River is located in eastern Connecticut and is approximately 20 miles long. It has a rich history dating back to the 1600s when it was used by Native Americans for fishing and transportation. The river has been harnessed for hydroelectric power since the late 19th century, with several reservoirs and dams constructed along its course. The largest of these is the Mansfield Hollow Dam, which forms the Mansfield Hollow Reservoir. The river is also used for recreational purposes, including fishing, kayaking, and hiking along its scenic trails. Additionally, the river is an important source of water for agriculture and provides irrigation to the surrounding farmland. Despite its many uses, the Shetucket River has faced challenges including pollution and habitat loss, prompting conservation efforts to protect its unique ecosystem.