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GENERAL39784
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Last modified
8/24/2016 7:59:08 PM
Creation date
11/23/2007 10:21:38 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
General Documents
Doc Date
2/28/1986
Doc Name
PROPOSED DECISION & FINDINGS OF COMPLIANCE FOR PR1
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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<br />-2s- <br />aspen, mountain brush and coniferous vegetation types. These drainages are <br />either perennial or dependably contain flows sufficient to allow diversion <br />during the irrigation season (Alvin Jones, personal communication). The land <br />use map and discussion with Mr. Jones, Range Conservationist with the Soil <br />Conservation Service in Meeker, document that it is not the regional practice <br />to irrigate alluvial deposits associated with ephemeral drainages contained <br />within the 9 - 12 inch precipitation zone in Rio Blanco County. . <br />C. Salinity hazard of surface water based on data in the ERO study would be <br />classified as "high" based on USGS criteria (USGS, 1970). <br />D. Vegetation and soil pit information in the ERO Document indicate that <br />Greasewood (Sarcobatus vermiculatus), the most prominent vegetation species on <br />the alluvial terraces a ,7ace3' nt to the Red Wash Channel is probably <br />subirrigated. Greasewood is a salt tolerant phreatophyte and soil pits <br />indicate an alluvial zone of saturation at depths of between 5 and 8 feet. <br />Greasewood is not an agriculturally useful species and is, in fact, poisonous <br />to sheep under certain conditions. Data collected by the permittee do not <br />indicate the presence of agriculturally significant vegetation which might be <br />expected to benefit from the high water table. This is supported by <br />observations made on-site by Division staff in September, 1983. <br />The potential agricultural importance of the high water table and <br />subirrigation is negated by the high electrical conductivity (EC) of the <br />alluvial ground water. Analyses of ground water quality samples collected for <br />Alluvial Well Qa1 - 2 located at the confluence of Red Wash and the White <br />River indicate a range in EC levels from a low of 3,500 umhos/cm to a high of <br />12,000 umhos/cm between March, 1981 and August, 1982 (ERO, 1982). Based on a <br />USGS irrigation water rating chart (USGS, 1970), the salinity hazard of such <br />water could be rated "very high". <br />References Cited <br />ERO Resources Corporation, 1982. Red Wash Drainage Basin Alluvial Valley <br />Floor study. 30 pp. <br />Jones, Alvin, 1983. SCS Range Conservationist. Personal Communication. <br />United States Department of Agriculture, 1976. Land Use and Natural <br />Plant Communities Map, Rio Blanco County, Colorado. 3 sheets. <br />United State Geological Survey, 1970. Study and Interpretation of the <br />Chemical Characteristics of Natural Water. United States <br />Government Printing Office. 363 pp. <br />Western Fuels-Utah, Inc., 1980. Deserado Mine Mining Permit Application. <br />2. Scullion Gulch <br />The AVF finding regarding Scullion Gulch has not changed from the original <br />findings document. The Division and OSM concluded that Scullion Gulch is not <br />an alluvial valley floor, on the following basis: <br />
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