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APPCOR10132
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APPCOR10132
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Entry Properties
Last modified
8/24/2016 6:26:33 PM
Creation date
11/19/2007 2:08:29 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981034
IBM Index Class Name
Application Correspondence
Doc Date
4/9/1982
From
WESTERN ASSOCIATED COAL CORP
To
MLR
Media Type
D
Archive
No
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Nlenro to Grand <br />April 6, 1982 <br />Page Two <br />hl~a Coal Company File • <br />- Ponderosa Pine (not subirrigated) <br />- Fir <br />- Poa sP. (80;; phreatophyte) - very limited <br />Site ;3 - flood irrigated field southwest of Brimstone <br />Corner (hay field-harvested); T2 terrace <br />- Poa sp. (8090 phreatophyte) <br />Site n4 - meadoo-+ clear of trees northr•+est of Brimstone Corner; <br />T2 terrace (r+ith small irrigation ditch on east side) <br />- Curleycup Gumr•+eed (indicative of disturbed area or overgrazing) <br />- Fringed Sage (common upland plant on gravelly to loamy soils) <br />3. The only area visited r•+hich appeared to be clearly subirrigated <br />was the area to the north of the southern gaging station along <br />Ward Creek. This area is dor•+nstr-eam of the area to be mined, <br />and a number of springs and seeps v+ere located in this area. <br />Hor+ever, the Tl terrace r•+hich is subirrigated is thin (generally <br />less than 25 feet on each side of the creek), and this area has <br />limited agricultural usefulness due to the rugged and steep <br />terrain of the area (e.g., the Rollins Sandstone outcrop). <br />4. From the reconnaissance site visit, it r•+as apparent that areas <br />of agricultural significance in the Ward Creek and l•lilliams <br />Creek valleys are flood irrigated fields on cleared areas on the <br />T9 and higher terraces (which are considerably higher than the <br />creek and not subirrigated). <br />Therefore, based on the above reasoning, test pits to study subirrigation <br />are not recommended at this time. However, piezometers in the alluvial <br />ground r•+ater system and a more thorough vegetation survey will provide <br />definitive information to determine the extent and importance of subirriaa- <br />tion along Ward Creek and Williams Creek. The piezometers will also help <br />determine the relationship of tine shallor•+ ground o-+ater to the streams and <br />ditches. <br />13 <br />
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