Laserfiche WebLink
<br />Twice in the last 85 years, in March 1955 and February 1962, ice <br />jams caused water stages in the White River to reach Main Street <br />between Colorow Street and Birch Avenue. These floods caused <br />damage to homes, businesses, and public utilities. Ice jam floods <br />have been observed as far back as 1891, when Rangely consisted of a <br />saloon, blacksmith shop, store, and hotel. <br /> <br />In the late summer of 1910 or 1911, a thunderstorm produced flood <br />stages almost to the 1962 level. Another thunderstorm in the 1920s <br />raised the White River to approximately the location of the Rangely <br />Hotel, but the water was 1 foot lower than the 1955 flood. <br /> <br />Two of the largest thunderstorms to produce local flooding occurred <br />in August 1946 and July 1953. In the 1946 flood, one downtown <br />office building had from 6 to 8 inches of water covering the floor. <br />On July 31, 1953, 1.42 inches of rain was measured in slightly over <br />1 hour at the Rangely gage, and resultant local flooding washed out <br />a road and tore away a bridge outside of Rangely. In town, runoff <br />caused drainage ditches to overflow, and damage from the <br />floodwaters was aggravated when the high water picked up oily mud <br />from around a local oil well. <br /> <br />Less than 2 years later, in March 1955, an ice jam in the White <br />River caused the river to leave its banks, and at one time the town <br />water supply was cut off when 6 feet of floodwater covered the <br />water filtration plant. <br /> <br />Water supply was aga1n interrupted by ice jams above and below the <br />town in February 1962. The flood of February 1962 was the largest <br />flood of record. In March 1966, another ice jam diverted the flow <br />of the White River and several ranches experienced flooding. Most <br />recently, flooding as a result of an ice jam occurred in March <br />1983. <br /> <br />Local residents agree that damaging floods occur on the average of <br />once every 7 to 10 years, with the majority resulting from ice <br />jams. Shallow flooding, with water characteristically less than 3 <br />feet deep, occasionally occurs in some southern portions of Rangely <br />as a result of rampant thunderstorm runoff from ravines and washes. <br /> <br />Due to a lack of streamflow records for the immediate vicinity of <br />Rangely, data basic to estimating the frequency of past floods are <br />not available. <br /> <br />2.4 Flood Protection Measures <br /> <br />There are no Federal flood control projects affording protection to <br />Rangely, and none are under consideration. Most new development in <br />Rangely is being kept out of potential flood damage areas. <br /> <br />College Canyon Draw has been channelized between South White Avenue <br />and County Highway 2 to increase channel capacity. <br /> <br />6 <br />