On May 28, 1889, a storm formed over Nebraska and Kansas, moving east. When
the storm struck the Johnstown-South Fork area (Item D on map below) two days later it was the worst
downpour that had ever been recorded in that section of the country. The US
Signal Service estimated that 6 to 10 inches (150 to 250 mm) of rain fell in 24
hours over the entire section. During the night small creeks became roaring
torrents ripping out trees and debris. Telegraph lines were downed and
rail-lines were washed out. Before daybreak the Conemaugh River that ran through
Johnstown was about to leave its banks.
During the day, things only got worse as water rose in the streets of Johnstown.
Then, in the middle of the afternoon of May 31st, the South Fork Dam 14 miles
(23 km) upstream burst, allowing the water formerly held back in the 3 mile (5
km) long Lake Conemaugh to cascade down the Little Conemaugh River.
When the wave reached the two-mile long
oxbow in the river it split. Part of the
wave left the river channel here, crossed
the oxbow, and hit the 75-foot-high stone
viaduct. Because the water was choked with
debris by this time, it was temporarily
dammed at the arch. The greater part of the
flood followed the oxbow, and crashed into
the viaduct six to seven minutes later. For
a brief moment, the wreckage at the viaduct
created a second dam for Lake Conemaugh.
When the viaduct collapsed, it did so with
even greater violence than the South Fork
Dam. (Item E on map below)
The wave headed toward East Conemaugh. A
witness said the water by now was almost
obscured by the debris, resembling "a huge
hill rolling over and over, "tossing up logs
high above its surface. Before the flood hit
East Conemaugh, train engineer John Hess
tried to warn the residents by tying his
train whistle down and racing toward town
ahead of the wave. His warning saved many,
but 50 people died, including about 25
passengers on trains that had been stranded
in the town by earlier flooding caused by
the rain. (Item F in map below)
The inhabitants of the town of Johnstown
(Item G in map below) were caught by surprise as the wall of
water bore down on the village, travelling at 40 miles per hour (64 km/h) and
reaching a height of 60 feet (18 m) in places. Some, realizing the danger, tried
to escape, but most people were hit by the surging flood water. Many people were
crushed by pieces of debris, and others became caught in barbed wire from the
wire factory upstream. For those that sought safety in attics, and for those
that managed to stay aloft of the flood water on pieces of floating debris, the
worst was to come, as they were forced to wait for hours for help to arrive.
At Johnstown, the Stone Bridge, (Item H
in map above) which was a substantial arched structure,
carried the Pennsylvania Railroad across the Conemaugh River. Some people who
had been washed downstream became trapped in an inferno as debris that had piled
up against the Stone Bridge caught fire, killing 80 people. The fire at the
Stone Bridge burned for three days. After, the pile of debris there covered 30
acres (120,000 mē).
Abbreviations used in the list of dead
and missing:
GCG:German Catholic
Cemetery (Geistown)
GC-PL: Grandview Cemetery Private Lot
GC-PP: Grandview Cemetery Public Plot-Bodies
found but not recovered by family/friends
GCS: German Catholic Cemetery (Sandyvale)
LYC: Lower Yoder Catholic Cemetery
Missing: Body Never Recovered
NCR: No Cemetery Record
OCG: Old Catholic Graveyard (Conemaugh
Borough)
SC: Sandyvale Cemetery
SM: St. Mary's Cemetery (Lower Yoder)
There is some minor popping noise in the video.
Notes About Book and Database:
Source:Historical information
was sourced from: The Johnstown Horror!
or, Valley of Death, being A Complete and
Thrilling Account of the Awful Floods and
Their Appalling Ruin, by James Herbert
Walker. Published by H. J. Smith & Co. 1889.
Map was built using
ComChart's tools. Original map was from the
National Park Service.
Video is from old
Universal News Film.
Online Publication: The manuscript was
scanned and then ocr'd. In depth proof
reading has been done on this manuscript and
it is free of errors. The punctuation and
spelling from the original text have been
faithfully preserved. Only obvious
typographical errors have been corrected.
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