On June 9, 1972 the unusual and excessive rainfall was the result of a strong low-level easterly air flow that forced moist air upslope over the hills. This sustained orographic effect helped the air to rise, cool, become very unstable, and release its moisture in repeating thunderstorms. Another important contributing factor was the unusually light winds at higher altitude. These light winds did not disperse the moist air or move the thunderstorms along to prevent the extreme concentration of rainfall. Instead, these conditions allowed heavy rainfall to remain almost stationary along the eastern slopes of the Black Hills. The first reports of significant rainfall were at 3:00 p.m. and by 6:00 p.m. there was a solid line of storms from Sturgis to Keystone on a line east of Pactola Dam which remained stationary until slowly moving eastward beginning about 10:00 p.m. In Rapid City the heaviest rain continued until approximately midnight with light rain falling until 4:00 a.m. on June 10th.
The Uniview image you now see includes the stream watershed areas for the eastern Black Hills and overlaying this we have turned on the isohyetal map showing the lines of equal rainfall during the 12 hour period on June 9 & 10. The levels are represented by differing shades of blue with the darkest representing 14 inches of rainfall to the lightest at 2 inches . As you can see the heaviest rainfall fell between Pactola and Rapid City on a line from Sturgis to the north and Keystone to the south. The worst flooding occurred on Rapid Creek, Spring Creek, Box Elder and Battle Creek. On Rapid Creek, the total drainage area above Canyon Lake is 371 square miles; however, just 14% of this area or 51 square miles of drainage downstream of Pactola Reservoir contributed to the flood runoff into Rapid City. The peak discharge on Rapid Creek just above Canyon Lake was 31,200 cubic feet per second, while the discharge from Pactola never exceeded 74 cfs, the normal discharge from the dam.
At approximately 10:00 p.m. water began to flow over the spillway on Canyon Lake with creek levels increasing 12 feet between 9:15 and 11:15 p.m. The gates on the spillway were opened to lower the level but were soon clogged with debris. The water level continued to rise and soon overtopped the entire dam. Although the main break in the dam probably washed out fairly rapidly, it was reported that water flowed over the top of the dam for approximately 45 minutes before the dam gave way at 10:45 p.m. The peak flow of 12,500 cfs from Cleghorn Canyon just above Canyon Lake coincided with the breaching of the dam. The total of these two flows accounts for 86% of the estimated peak flood in Rapid City of 50,000 cfs along Omaha Street. The size of Canyon Lake compared to the flood flow along Rapid Creek over and through the lake is minimal; however when the dam did fail it likely added to the 50,000 cfs rampage, resulting in additional loss of life. This image shows the boundaries of the 1972 flood from Canyon Lake through Rapid City. The area of the flood is depicted in this layer in red; and to provide some perspective on the amount of water flooding Rapid City on that night the next layer compares the volume of Pactola Reservoir in the near square mile to the flood waters in the taller square mile patch - the equivalent of 14.5 Pactola volumes flooded Rapid City.
Uniview cues
Geoscope:
Toggle wvn09_1972_rapid_creek_isohyetal_v3.kmz for isohyetal rainfall map for 1972 storm.
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1972 Hydrograph for 1972 storm hydrograph slide.
2007 Stage for 2007 storm peak stage slide.
2007 Streamflow for 2007 storm streamflow slide.
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Fly to RapidCity to fly to view of Rapid City.
Geoscope:
Toggle Orthoimagery/USGS_EDC_Ortho_NAIP for high resolution NAIP WMS imagery.
Toggle wvn09_1972_flood_extent_v2.kmz for extent of 1972 storm in Rapid City.
Custom Events:
Fly to Blocks to fly to distant view of water volumes.
Blocks Close-Up to fly to distant view of water volumes.
Toggle wvn09_1972_storm_rainfall_v3.kmz for cubic volume of water from 1972 storm.
Toggle wvn09_pactola_reservoir_v4.kmz for cubic volume of water for Pactola Reservoir.