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1986-03-03_REPORT - C1981013 (4)
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1986-03-03_REPORT - C1981013 (4)
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Entry Properties
Last modified
12/27/2020 5:19:48 AM
Creation date
12/7/2012 1:14:02 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981013
IBM Index Class Name
Report
Doc Date
3/3/1986
Doc Name
1985 Annual Hydrology Report (Part 1 0f 2)
From
Wyoming Fuel Company
Annual Report Year
1985
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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1.1 Site Description <br /> The mine sites are located approximately six miles west of Weston in Las Animas <br /> County, Colorado (T33S, R68W) and are situated in mountainous terrain which provides <br /> numerous canyons contributing runoff to the series of ephemeral, intermittent, and <br /> perennial streams of the area. The surface facilities are adjacent to the Purgatoire River <br /> which is the primary stream drainage of the area. The general direction of stream flow is <br /> easterly to the confluence with the Arkansas River, also in Las Animas County. <br /> The closest weather station to the site is located at the Trinidad Airport (elevation <br /> 5,746 feet) approximately 30 miles east. Over a recording period of 50 years, total <br /> precipitation averaged 13.5 inches. The majority of this precipitation occurs from April <br /> to September, July recording the most rainfall in the form of rapidly moving <br /> thundershowers. The mean temperature is 51.50 F, January and July having the lowest <br /> and highest temperature, respectively. The project area is approximately 1,650 feet <br /> higher in elevation than the Trinidad Airport and can be considered to have a somewhat <br /> lower mean temperature and higher average precipitation. Data collected from the <br /> Golden Eagle and New Elk precipitation stations (Tables 1 and 2 of Appendix 1) confirm <br /> that fact with 16.26 inches and 18.90 inches being recorded at each station for 1985, <br /> respectively. These stations are located approximately three miles apart (Figure 1) with <br /> the major difference in recorded precipitation being observed during mid-summer <br /> thunderstorms. Total precipitation measured indicates an average moisture year. <br /> Generally, soils of the area are shallow and coarse-grained being derived from the <br /> underlying sandstones and shales. Bedrock exposures are common and scattered <br /> throughout the area. The valley bottoms are underlain by alluvial deposits which are also <br /> coarse-grained, however, are deeper compared to soils of the mountain slopes. <br /> Vegetation varies from riparian in the valley bottoms to pinyon-juniper, oak brush, <br /> and pine cover on the side slopes. Vegetation cover ranges from 100% in the valley <br /> bottoms to near 0% on the steeper side slope rock outcrop areas. <br /> -2- <br />
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