| Trudy
E. Bell, M.A,, now considered
the foremost national authority on the Flood of 1913, in describing
the effects of the flood is quoted as saying—
"This mammoth storm system
with its ferocious tornadoes and floods set records for fatalities
and flood heights that still stand today - and which dwarfed both
Sandy and Katrina in geographical extent - created institutions
that evolved into today's United Way, Red Cross, Rotary, IBM,
and Cox Communications."
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Map of 1913 Flood Plain
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Marooned by flood on Park Avenue
Niles Ohio March 26th, 1913.
Credit for photo is given to Kestner & McIntyre
|
Photographs
of the 1913 Flood in Niles, Ohio
Newspaper account of 1913 Flood.
Flooding from the four-day rain
that began on Easter, March 23, 1913, however, was unprecedented
and never to be equalled in the century that followed. “It
was attributable solely to an almost unceasing rain of four days
and four nights, something akin to the biblical deluge,”
Joseph Butler wrote in his first-hand account of the
event. Although Mahoning River dwellers were forced to flee their
homes, “it was the industries that suffered worst,”
wrote Butler, the industrialist who founded the Butler Institute
of American Art in Youngtown.
“All of these located in the
river valley were put hopelessly out of operation, the water standing
many feet deep in the mill buildings and covering the machinery.”
Immediately after the 1913 flood,
the Ohio Legislature allowed the formation of conservancy districts
and authorized counties to form three-member boards to construct
and maintain flood-control structures.
In the Mahoning Valley, the Lake
Milton dam was completed in 1916, forming the lake that would
increase Youngstown’s industrial water supply and begin
the creation of water-storage capacity to alleviate flooding here.
In the decades that followed, dams
were built to create and regulate the water levels of Berlin,
West Branch, Mosquito and Shenango River Lake reservoirs. Those
lakes became part of a vast U.S. Army Corps of Engineers-managed
network of water-storage lakes that would reduce downstream flooding,
help maintain consistent river water depths and provide recreational
boating opportunities. Each fall, the Corps reduces water levels
in these lakes to increase their capacity to store snow melt and
spring rains, and thereby reduce downstream flooding.
“It was officially called
the ‘reservoir design flood,’” for Berlin, Mosquito
and West Branch, said Werner Loehlein, a hydraulic engineer
with the Corps in Pittsburgh. Those lakes and dams were designed
to withstand a recurrence of the 1913 flood, but with some water
going over the dams’ emergency spillways, he explained.
“From a volume standpoint,
it was a record flood,” Loehlein said. The 1913 flood consisted
of “a bunch of intense rainstorms with short periods of
little or no rain in between,” he added. Over the four days,
the Mahoning Valley got between 7 and 9 inches of rain, Loehlein
said, adding that rainfall averages were 8.8 inches in the west
branch basin of the Mahoning River, 7.15 inches on the river’s
main stem and 8.35 inches along Mosquito Creek, which flows into
the river in Niles. — By PETER H. MILLIKEN
| milliken@vindy.com
|
| 
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The Gilmore Restaurant and
Manhattan Hotel on South Main Sreet and
Water Street during the 1913 flood.
Visible are people watching from
second
floor windows and standing on the roof.
The building is dated 1892. |

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Looking North, the Gilmore
Restaurant and Manhattan Hotel on South Main Sreet and Water
Street during the 1913 flood. |

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Main Street looking south from
Mill Street (State Street) during flood, March 1913.
The Gilmore Restaurant and
Manhattan Hotel are visible on the right of the image. |

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View of Furnace Street, later State
Street, during 1913 Flood. |

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A postcard photo from the 1913
flood, showing Mill Street (now West State Street). The Flory
Boarding House is located center rear at the corner of Chestnut
and State. |

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Downtown area during the 1913 Flood.
View is of Water Street, looking
east, with the Manhattan Hotel on the left. |