Maximum discharge along the river is currently at the reporting a streamflow rate of cfs. This is also the highest stage along the Cass River, with a gauge stage of ft at this location. This river is monitored from 1 different streamgauging stations along the Cass River, the highest being situated at an altitude of ft, the .
The Cass River is a 61-mile-long river located in eastern Michigan. The river was named after Lewis Cass, a politician who served as Governor of Michigan, Secretary of War, and Secretary of State. The Cass River flows through several counties, including Tuscola, Saginaw, and Bay. It is a tributary of the Saginaw River, which ultimately flows into Lake Huron. The river is known for its diverse aquatic life, including several species of fish such as walleye, northern pike, and smallmouth bass. Several reservoirs and dams are located on the river, including the Tobico Dam, which was built in 1924 to help regulate water levels in the Saginaw Bay. The Cass River is used for recreational activities such as fishing, canoeing, and kayaking. Additionally, the river is used for irrigation and agriculture in the surrounding areas.
Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
---|---|---|---|---|---|---|---|---|
Cass River At Frankenmuth
USGS 04151500 |
264 cfs | 4.72 ft | 26.94 |
The Cass River is an alpine river in the Canterbury Region of the South Island of New Zealand. It rises in the Hall Range immediately below Rankin Pass, and also receives water from the nearby Huxley Glacier. After dropping 600 metres (2,000 ft) very rabidly the river flows south with braided channels along a flat-bottomed valley for 25 kilometres (16 mi). The Leibig Range and Gamack Range are to the west, and the Haszard Range to the east.
The river flows into the west side of Lake Tekapo where it has built up a gravel delta.The Cass River is named for Thomas Cass, Chief Surveyor of Canterbury Province from 1851 to 1867.