A strong cold front moved across the Ohio River Valley during the afternoon of March 1. Strong storms had developed near this cold front well to the west the day before, and raced through the middle Ohio River Valley early on the 1st as a severe squall line producing widespread damaging wind gusts. Heavy rainfall from training storms also produced flash flooding as 1-2 inches of rain fell over several hours. The flash flooding combined with the wet ground eventually lead to river and stream flooding during the afternoon of the 1st through the 2nd.
The Muskingum river at Beverly, spilled over its banks on the evening of the 1st, and remained in flood stage for several hours. The river had a crest of 29.3 feet, just above the flood stage of 29 feet. This caused minor flooding of several homes, roads and lowlands next to the river.
The Hocking River at Athens rose out of its banks just after noon on the 2nd, and remained above flood stage through mid morning on the 3rd. The river crested at just over 21 feet, about a foot over flood stage of 20 feet. This resulted in minor flooding of lowlands and campgrounds along the river.
Other smaller creeks and streams, such as Duck Creek, the Little Muskingum, Raccoon Creek, Shade Creek and Symmes Creek all rose out of their banks. The Raccoon Creek was the last to return below bankfull, early on the 4th. According to the Ohio DOT, various roads were closed due to the flooding across Southeast Ohio.