Total streamflow across the Coosawattee River was last observed at 2,944 cfs, and is expected to yield approximately 5,839 acre-ft of water today; about 134% of normal. River levels are high. Average streamflow for this time of year is 2,203 cfs, with recent peaks last observed on 2016-01-01 when daily discharge volume was observed at 23,440 cfs.

Maximum discharge along the river is currently at the Coosawattee River Near Pine Chapel reporting a streamflow rate of 1,260 cfs. This is also the highest stage along the Coosawattee River, with a gauge stage of 6.35 ft at this location. This river is monitored from 3 different streamgauging stations along the Coosawattee River, the highest being situated at an altitude of 1,218 ft, the Coosawattee River Near Ellijay.

The Coosawattee River is a 49-mile-long river located in northern Georgia. It flows through the Appalachian Mountains and is a tributary of the Oostanaula River. The river has a rich history, and Native American tribes have lived in the area for thousands of years. The name "Coosawattee" comes from the Cherokee language and means "old town." The river is an important source of water for irrigation and hydroelectric power generation. There are several dams and reservoirs along the river, including the Carters Lake Dam and the Coosawattee Dam. These dams provide recreational opportunities for fishing, boating, and swimming. The river is also used for agricultural purposes and provides water for crops and livestock.