Total streamflow across the
Naugatuck River
was last observed at
446
cfs, and is expected to yield approximately
885
acre-ft of water today; about 62%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
723 cfs,
with recent peaks last observed
on
2021-09-02 when daily discharge volume was observed at
14,338 cfs.
Maximum discharge along the river is currently at the
Naugatuck River At Beacon Falls
reporting a streamflow rate of 330 cfs.
However, the streamgauge with the highest stage along the river is the
Naugatuck River At Thomaston
with a gauge stage of 2.23 ft.
This river is monitored from 2 different streamgauging stations along the Naugatuck River, the highest being situated at an altitude of 378 ft, the
Naugatuck River At Thomaston.
| Last Updated | 2025-12-04 |
| Discharge Volume | 885 ACRE-FT |
| Streamflow |
446.0 cfs
-201.0 cfs (-31.07%) |
| Percent of Normal | 61.65% |
| Maximum |
14,338.0 cfs
2021-09-02 |
| Seasonal Avg | 723 cfs |
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Naugatuck River At Thomaston
USGS 01206900 |
116 cfs | 2.23 ft | -30.12 | |||||
|
Naugatuck River At Beacon Falls
USGS 01208500 |
330 cfs | 2.11 ft | -31.39 |
The Naugatuck River is a 40.2-mile-long (64.7 km) river in the U.S. state of Connecticut. Its waters carve out the Naugatuck River Valley in the western reaches of the state, flowing generally due south and eventually emptying into the Housatonic River at Derby, Connecticut and thence 11 miles (18 km) to Long Island Sound. The Plume and Atwood Dam in Thomaston, completed in 1960 following the Great Flood of 1955, creates a reservoir on the river and is the last barrier to salmon and trout migrating up from the sea.