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2014-11-21_PERMIT FILE - C1996084 (23)
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2014-11-21_PERMIT FILE - C1996084 (23)
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Last modified
8/24/2016 5:55:33 PM
Creation date
11/24/2014 11:00:59 AM
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Template:
DRMS Permit Index
Permit No
C1996084
IBM Index Class Name
Permit File
Doc Date
11/21/2014
Section_Exhibit Name
SECTION 2.04 INFORMATION ON ENVIRONMENTAL RESOURCES
Media Type
D
Archive
No
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Rule 1: Permits <br />• The Poison Canyon Formation consist of distal and proximal fan deposits. The Poison Canyon <br />distal facies consists of massive buff to red arkosic sandstone and conglomerates with thin yellow <br />shale beds. The larger grain size and unweathered feldspar grains distinguishes the distal and <br />proximal Poison Canyon from the Raton Formation. <br />The igneous geology encountered in the permit area consists of intrusive sills associated with the <br />Spanish Peaks. Outcrops of basalt occur th areas located in Little Jeff Canyon, Puertecito Canyon <br />and Cow Canyon. The basalt is weathered in these areas and predominantly consists of fine <br />grained, dazk grey rocks. The sills are the cause of metamorphism of coal to natural coke in the <br />Raton Basin and possibly the permit area. <br />The major geologic structure in the area is the Raton Basin which was undergoing gentle down <br />warping during the time of depositions of the coal. After deposition of the basin sediments, <br />deformation with intense folding and subsequent thrust faulting occurred west of the site. Shears <br />developed in an east-west pattern, and normal tension faults have developed in a complimentary <br />set of fractures. The La Veta Syncline bisects the site with the location of the axis located roughly <br />through Lorencito Canyon. Structure contour maps of the primary coal seams to be mined, the <br />Ciruela and Primero coal seams, aze presented in Exhibit 6, Geology Technical Report. Dips on <br />the top of the Ciruela coal seam average 1.5 degrees toward the axis of the syncline. Dips on the <br />top of the Primero coal seam average 1.7 degrees toward the axis of the syncline. <br />• The stratigraphy of the units included within the permit area can be divided into six hydrogeologic <br />units. The six hydrogeologic units identified are: <br />alluvium, which includes the unconsolidated valley fill material in drainages; <br />overburden, defined as the unit overlying the Ciruela coal; <br />Ciruela coal; <br />interburden, the units located between the Ciruela coal and the Primero coal; <br />Primero coal; and <br />underburden, the unit that underlies the Primero coal. <br />Four past exploration activities have been conducted at the site prior to the 1996 field drilling <br />program. A total of 79 boreholes were drilled across the site as shown in Map 2.04.6-1. A <br />geologic map of the permit area is included as Map 2.04.6.2. Exhibit 6, Geology Technical <br />Report, includes geologic cross sections of the permit area. Lithologic and electric logs are also <br />included in Exhibit 6, Geology Technical Report. <br /> <br />PERMIT.revUpril3l, 1941 2.04-6 (revised 4/21/97) <br />
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