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Great Dayton Flood

Natural disaster in Ohio, US in 1913

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  • 6 chapters

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Through Flood, Drainage basin and Tributary

The flood was caused by a series of severe winter rainstorms that hit the Midwest in late March. Within three days, 8–11 inches (200–280 mm) of rain fell throughout the Great Miami River watershed on already saturated soil, resulting in more than 90 percent runoff. The river and its tributaries overflowed. The existing levees failed, and downtown Dayton was flooded up to 20 feet (6 m) deep. This flood is still the flood of record for the Great Miami River watershed. The volume of water that passed through the river channel during this storm equaled the monthly flow over Niagara Falls.

The Great Miami River watershed covers nearly 4,000 square miles (10,000 km2) and 115 miles (185 km) of channel that feeds into the Ohio River. Other Ohio cities also had flooding from these storms but none as extensive as those along the Great Miami, which included Dayton, Piqua, Troy, and Hamilton.

Background

Dayton was founded along the Great Miami River at the confluence of its three tributaries: the Stillwater River, the Mad River, and Wolf Creek. Dayton's central business district developed within 1 mile (1,600 m) of the confluence of these waterways. When Israel Ludlow laid out Dayton in 1795, the local Indigenous Peoples warned him about the recurring flooding.

Prior to the 1913 flood, the Dayton area had suffered major floods nearly every other decade, with major water flows in 1805, 1828, 1847, 1866, and 1898. Most of downtown Dayton was built in a natural flood plain, which seemed advantageous in the early years when cities depended on rivers for transportation needs.

The storms that caused the flood at Dayton continued over several days and affected an area across all or parts of more than a dozen states, most notably states in the Midwest and along the Mississippi River. Heavy rain and snow saturated the soil and produced widespread flooding, known as the Great Flood of 1913, across Indiana, Ohio, Kentucky, New York, and Pennsylvania.

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