Total streamflow across the Conemaugh River was last observed at 538 cfs, and is expected to yield approximately 1,067 acre-ft of water today; about 17% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 3,107 cfs, with recent peaks last observed on 2018-09-10 when daily discharge volume was observed at 46,200 cfs.

Maximum discharge along the river is currently at the Conemaugh River At Seward reporting a streamflow rate of 400 cfs. However, the streamgauge with the highest stage along the river is the Conemaugh River At Tunnelton with a gauge stage of 2.62 ft. This river is monitored from 3 different streamgauging stations along the Conemaugh River, the highest being situated at an altitude of 1,133 ft, the Conemaugh River At Minersville.

The Conemaugh River is a 90-mile-long tributary of the Allegheny River in western Pennsylvania. The river has a rich history dating back to the Native American tribes and later played a significant role in the industrialization of the region. The river's hydrology has been impacted by several dams and reservoirs, including the Conemaugh Dam and the Johnstown Flood Control Reservoir. These structures have helped to regulate the river's flow and prevent flooding in nearby communities. Today, the Conemaugh River is a popular destination for recreational activities such as fishing, kayaking, and hiking. It also supports agricultural activities in the surrounding areas. Despite its importance, the river faces ongoing threats from pollution and environmental degradation.