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2020-10-27_GENERAL DOCUMENTS - C1981035
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2020-10-27_GENERAL DOCUMENTS - C1981035
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Last modified
10/29/2020 1:41:04 PM
Creation date
10/29/2020 1:05:13 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981035
IBM Index Class Name
General Documents
Doc Date
10/27/2020
Doc Name Note
For PR10
Doc Name
Proposed Decision and Findings of Compliance
From
DRMS
To
GCC Energy, LLC
Permit Index Doc Type
Findings
Email Name
JHB
THM
Media Type
D
Archive
No
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Surface Water Hydrology (4.05 and 4.07) <br />There are no perennial streams within the King Coal permit area. The surface facilities of the <br />King I and II Mines are located in ephemeral drainages that are tributary to Hay Gulch. Hay <br />Gulch does not have a stream channel in the vicinity of the permit area. Historically, surface <br />flow in Hay Gulch has been diverted into the irrigation ditch on the north side of the Gulch. This <br />ditch carries water that has been diverted from the La Plata River. Hay Gulch is a tributary of <br />the La Plata River, and their confluence is located about six miles downstream (southwest) from <br />the permit area. <br />Runoff from most of the undisturbed upper parts of drainages in King I and King II is diverted <br />around the disturbed areas through ditches and culverts. With the exception of runoff from main <br />haul roads, runoff from disturbed areas is passed through sediment control ponds which <br />discharge into Hay Gulch. <br />The King I workings extended southward beneath the Pine Gulch ephemeral drainage and other <br />small drainages. Pine Gulch flows into Hay Gulch approximately two miles downstream from <br />the permit area. Northwest of the King II Mine (overlying the workings of the OSMRE permit) <br />lies East Alkali Gulch, an ephemeral stream. East Alkali flows to the southwest and south, <br />ultimately joining Hay Gulch approximately seven miles downstream of the permit area. Two <br />of the proposed parcels surface runoff reports to East Alkali Gulch. <br />Additional information on surface water hydrology can be found in the permit application in <br />Sections 2.04.7, 2.05.3 and 2.05.6 and on Maps King I-007, King I-007a, and the King II — 007 <br />series of maps. <br />Climate (4.08) <br />The climate is semi -arid, characterized by hot summers, cold winters, and a limited amount of <br />precipitation each year. The prevailing winds are from the southwest and west with an average <br />annual precipitation rate varying from 15 to 19 inches. The growing season in the area varies <br />depending on elevation and exposure with a maximum of 96 frost -free days. <br />Soils (4.09) <br />Soil properties in the permit area vary widely depending on slope, aspect, and topographic <br />position. Deeper soils are found in the valley bottoms and on the tops of plateaus, while shallow <br />soils associated with rock outcrops dominate the side slopes. Two soil orders (Entisolls and <br />Aridisols) and one rock outcrop complex occur on the site. Both of the soil orders have an ustic <br />moisture regime. The results of soil analyses are provided in Appendix 6 of the PAP. <br />Vegetation (4.10) <br />The dominant vegetation in the King I and II Mine area is a mountain shrub community. Gambel <br />Oak is the most prominent shrub along the side slopes, forming dense stands. On the plateau top <br />above the King I Mine, the oak grows in clumps with open stands of grasses interspersed. A <br />juniper/pinyon community is found on the more xeric southern slopes, with scattered individuals <br />of Douglas Fir and Ponderosa Pine encountered on more mesic northern slopes. A <br />0 <br />
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