Total streamflow across the
Swift River
was last observed at
266
cfs, and is expected to yield approximately
528
acre-ft of water today; about 30%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
898 cfs,
with recent peaks last observed
on
2014-04-16 when daily discharge volume was observed at
9,130 cfs.
Maximum discharge along the river is currently at the
Swift River Near Roxbury
reporting a streamflow rate of 220 cfs.
This is also the highest stage along the Swift River, with a gauge stage of
2.27 ft at this location.
This river is monitored from 2 different streamgauging stations along the Swift River, the highest being situated at an altitude of 619 ft, the
Swift River Near Roxbury.
The Swift River is a major tributary of the Chicopee River in Massachusetts, USA.
| Last Updated | 2026-04-24 |
| Discharge Volume | 528 ACRE-FT |
| Streamflow |
266.0 cfs
Past 24 Hours: -21.0 cfs (-7.32%) |
| Percent of Normal | 29.61% |
| Maximum |
9,130.0 cfs
2014-04-16 |
| Seasonal Avg | 898 cfs |
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Swift River Near Roxbury
USGS 01055000 |
220 cfs | 2.27 ft | -7.32 | |||||
|
Swift River At West Ware
USGS 01175500 |
44 cfs | 2.18 ft | 0 |
The Swift River is a river that begins in Yukon Territory and flows southwest into British Columbia to its mouth at the east side of Teslin Lake on the Teslin River system. The river drains the uppermost portion of the Cassiar Mountains and in its lower reaches traverses the Nisutlin Plateau, which lies along the east side of Teslin Lake north of the mouth of the Jennings River, which is to the south of the Swift.
The river is one of two in British Columbia known as the Swift, the other of the same name is tributary to the Cariboo River in the eastern parts of the region of the same name.