My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD05245
CWCB
>
Floodplain Documents
>
Backfile
>
4001-5000
>
FLOOD05245
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:48:42 PM
Creation date
10/5/2006 1:22:57 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Stream Name
All
Basin
Statewide
Title
Floods of September, 1970 in Arizona, Utah, Colorado, and New Mexico
Date
1/1/1978
Prepared For
State of Colorado
Prepared By
USGS
Floodplain - Doc Type
Flood Documentation Report
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
69
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />24 <br /> <br />FLOODS OF SEPT. 1970 IN ARIZ., UTAH, COLO., AND N. MEX. <br /> <br />CENTRAL ARIZONA <br /> <br />25 <br /> <br /> <br />FIGURE 1O.~Cabin damaged by the flood in Tonto Creek near Kohl Ranch. <br /> <br />parallel with the channel of Tonto Creek. High-water marks at the <br />confluence were 18 ft (5.5 m) above the bed ofTonto Creek and only 2ft (0.6 <br />m) above the top of the bar. The gravel bar and the high-water marks <br />indicate that the peak discharge of Houston Creek was nearly coincident <br />with that of Tonto Creek. <br />Although the discharge of Rye Creek was comparable to that of Tonto <br />Creek, only minor flood damage occurred in the Rye Creek basin. The flood <br />near the mouth of Deer Creek, a tributary to Rye Creek, was reported by <br />T. P. Hughes (local resident, oral commun., 1970) as being the largest since <br />1932. In the broad valley of Tonto Creek near Punkin Center, most of the <br />terrace that borders the wide gravelly channel was inundated, and an area as <br />much as one-half mi (0.8 km) wide was flooded (pi. I). <br />The peak discharge of 18,400 [(' Is (521 m'l s) in Tonto Creek below Kohl <br />Ranch (fig. 7, No. 85), 11,900 ft'ls (337 m'/s) in Christopher Creek (fig. 7, <br />No. 86), and a large flow from Haigler Creek produced a peak discharge of <br />38,000 ft'ls (1,080 m'/s) in Tonto Creek near Gisela (fig. 7, No. 88). The <br />peak discharge of 44,400 ft'/s (1,260 m'/s) in Rye Creek near Gisela (fig. 7, <br />No. 89) entered Tonto Creek 2 hours before the peak moving downstream in <br />Tonto Creek. The peaks were of extremely short duration, which caused two <br />separate peaks 2~ hours apart 5 mi (8 km) downstream at the Tonto <br />Creek above Gun Creek, near Roosevelt gaging station (fig. 7, No. 91). The <br />higher of the two peaks-53,000 ft'ls (1,500 m'/s)-is the maximum <br />discharge recorded since the station was established in 1940. Downstream <br />from Tonto Creek above Gun Creek gaging station, records from two <br />abandoned staff gages indicate that the flood of 1970 may have been the <br />largest since the early 1900's. <br />Tonto Creek flows into Roosevelt Lake-the uppermost reservoir in the <br />Salt River Reservoir system. On September 4, storage in the reservoir system <br />was at a minimum for the year, and all the flow that entered Roosevelt Lake <br />from Tonto Creek on September 5 was stored in Roosevelt Lake and the <br />other three lakes that make up the Salt River reservoir system (fig. 7, No. 93). <br /> <br />are on a natural levee, which was inundated by about I ft (0.3 m) of water. <br />One person was drowned when wading from the levee through the deeper <br />water adjacent to the levee. Mr.. Eddie Potter (local resident, oral commun., <br />1970) stated that the flow tossed boulders several feet into the air at the <br />embankment of State Highway 160. Boulders and cobbles were strewn on <br />the highway, and a large cottonwood tree was jammed through an <br />unoccupied cabin by the force of the water; the cabin was damaged so <br />severely that it was later torn down. <br /> <br />Tonto Creek is in a steep-walled canyon for several miles downstream <br />from Christopher Creek. No serious damage was reported or observed <br />during an aerial reconnaissance of Bear Flat, the only development in the <br />area. Tributaries to Tonto Creek downstream from the canyon carried <br />extremely high flows. Long reaches of bedrock were exposed along Haigler <br />Creek, as the flood cleared everything in its path including timber and soil <br />cover. The flood in Houston Creek filled a diversion ditch with sand and <br />gravel-the first such occurrence since the ditch was constructed a few <br />decades ago. A gravel bar 16 ft (4.9 m) high was deposited at the mouth of <br />Houston Creek. The downstream end of the bar forms an escarpment that is <br /> <br />SYCAMORE CREEK BASIN <br /> <br />During September 3-6, at least 7 inches (180 mm) ofrain fell in the upper <br />part of the Sycamore Creek basin, and as much as 10 inches (255 mm) was <br />recorded at one precipitation station. Long-time residents reported that the <br />flood of 1970 was the largest known in the area. Many stock tanks built in the <br />last few decades were breached by runoff. Three persons were killed as a <br />result of flooding in Sycamore Creek. An Arizona State Highway patrolman <br />on an emergency call was killed when his patrol car plunged into Sycamore <br />Creek at the washed-out bridge 5 mi (8 km) south of Sunflower, and two <br />persons were drowned a short distance upstream from Sunflower (pi. I). <br />According to L. T. Walker (local resident, oral commun., 1970), several <br />motorists proceeded on State Highway 87 near Sunflower as the flood began <br />
The URL can be used to link to this page
Your browser does not support the video tag.