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2013-04-18_PERMIT FILE - C2009087 (6)
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2013-04-18_PERMIT FILE - C2009087 (6)
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Last modified
8/24/2016 5:19:38 PM
Creation date
5/1/2013 12:49:41 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C2009087
IBM Index Class Name
Permit File
Doc Date
4/18/2013
Doc Name
General Description of Hydrology
Section_Exhibit Name
2.04.5 General Description of Hydrology and Geology
Media Type
D
Archive
No
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RULE 2 - PERMITS <br />2.04.5 General Description of Hydrology and Geology <br />]'his application contains comprehensive and detailed descriptions and maps concerning the geology <br />and hvdrolog} of the proposed permit area. adjaCellt area. and the general area. The definitions of <br />these areas. as contained in Rule 1, Section 1.04, have been applied. in «hat PSCM believes to be a <br />reasonable nial ncr. to the lands surrounding the planned mining operation. The PSCM permit area <br />contains all lands on which the operator \\Ill conduct Illinilh) operations dlll'llh) the term Of the permit. <br />The adjacent area covers lands and resources outside the PSC 1\I perllllt area «hlch may be affected b} <br />minim, operations. The general area includes the topographic and groundwater basin surrounding the <br />area to be IllllleCl. 11]Cllldlllg one of more watersheds containing perennial streams and groundwater <br />s\ sterns. The general area is of sufficient size to allow assessments of curnulati� e hydrologic <br />impacts in the basin. This section specifically addresses the general area with regard to geology and <br />hydrology. The information presented in this section is based on research of available published <br />reports and documents: contacts with Federal. State. and local a0encies: site - specific investigations: <br />and ongoing monitoring activities. <br />A map of the larger region that contains the Hayden Syncline Basin general area is shown on Map <br />2.04.5 -M1, Regional Geology and Hydrology. The PSCM permit area includes all lands to be <br />undermined or disturbed by mining activities over the life of the mine. It is drained primarily by <br />Grassy Creek and its tributaries towards the north. and minor tributaries of Fish Creek towards the <br />south and southeast. The proposed general area for surface water hydrology includes the entire <br />watershed of Grassy Creek to its confluence with the Yampa River, and the western tributary <br />\�atcrshcds of fish Creek lying within the ` OLItlet fish Creek" hydrologic unlit, ending at the <br />confluence of Fish Creek with Trout Creek. A logical structurally defined boundary for geology <br />and hydrogeology for the PSCM general area is the anticlinal axes of the Tow Creek anticline on <br />the east and south and the Fish Creek anticline on the x\est. <br />Information on the geology and surface and groundwater systems for all lands within the PSCM <br />permit area and adjoining area described above is included under Sections 2.04.6 and 2.04.7 of this <br />application. <br />Regional and General Area Geology <br />The PSCM is situated within the southeastern synclinal portion of the Sand Wash Structural Basin <br />of northern Colorado and central Wyoming (Bass et al., 1955), also known as the Yampa Coal <br />Field. Figure 2.04.5 -F1, presents a geologic depiction of the Yampa Coal Field. The Sand Wash <br />Basin is part of the greater Green River Region which includes the Washakie Basin, the Great <br />Divide Basin, and the Green River Basin. The sub - basins are separated by uplifts caused by <br />deformation of basement rock. The Sand Wash basin is bordered to the southwest by the Axial <br />Basin Anticline, to the north by Cherokee Arch, and the east by the Park Range Uplift, or Anticline <br />(CGS, 2003). The Sand Wash Basin covers approximately 5,600 square miles and is primarily <br />located in Moffat and Routt Counties, Colorado (EPA, 2004). <br />Topography in the region ranges from gently sloping valleys to deeply incised slopes and vertical <br />cliffs. The form of the land surface is greatly affected by the lithologic and structural setting of the <br />local area. Deeply incised slopes occur primarily on the eastern limbs of the Sage Creek, Fish <br />Creek, and Tow Creek Anticlines while low- relief, gently rolling terrain overlies the axis of the <br />Sage Creek and Hayden Syncline. <br />Midterm Review 2.04 -15 Revision 04/2013 <br />
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