Maquoketa River

Total streamflow across the Maquoketa River was last observed at 10,290 cfs, and is expected to yield approximately 20,410 acre-ft of water today; about 261% of normal. River levels are high. Average streamflow for this time of year is 3,939 cfs, with recent peaks last observed on 2019-03-16 when daily discharge volume was observed at 30,150 cfs.

Maximum discharge along the river is currently at the Maquoketa River Near Maquoketa reporting a streamflow rate of 9,050 cfs. This is also the highest stage along the Maquoketa River, with a gauge stage of 19.41 ft at this location. This river is monitored from 2 different streamgauging stations along the Maquoketa River, the highest being situated at an altitude of 920 ft, the Maquoketa River At Manchester.

The river stretches for approximately 150 miles, starting from its source in Hancock County, Iowa and ending at its confluence with the Mississippi River in Jackson County, Iowa. The river is known for its rich history, including Native American settlements and European exploration. Today, the river is used for a variety of recreational activities such as fishing, boating, and camping. The river also serves as a source of irrigation for agricultural purposes. However, the river has faced challenges due to the construction of several dams and reservoirs that have altered its natural hydrology. These include the Backbone Lake Dam and the Lake Delhi Dam, which have been the subject of controversy due to their environmental impact.