Licking River

Total streamflow across the Licking River was last observed at 2,104 cfs, and is expected to yield approximately 4,174 acre-ft of water today; about 14% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 15,064 cfs, with recent peaks last observed on 2025-04-07 when daily discharge volume was observed at 154,549 cfs.

Maximum discharge along the river is currently at the Licking River At Catawba reporting a streamflow rate of 808 cfs. This is also the highest stage along the Licking River, with a gauge stage of 6.43 ft at this location. This river is monitored from 5 different streamgauging stations along the Licking River, the highest being situated at an altitude of 864 ft, the Licking River Below Mason Fork Nr Salyersville.

The river has a rich history, dating back to the pre-colonial era, when it was used as a major trade route for Native Americans. The Licking River also played a significant role in the development of the region's agriculture and industry. The river is home to several dams and reservoirs, including the William H. Harsha Lake and the Cave Run Lake, which provide drinking water, flood control, and hydroelectric power. The Licking River supports a wide range of recreational activities, including fishing, boating, and camping. Additionally, it is an important source of irrigation water for many farms in the area, and supports the growth of crops such as corn and soybeans. Despite its importance, the Licking River faces several challenges, including pollution and habitat destruction, which threaten its long-term health and vitality.