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2010-05-07_PERMIT FILE - C2009087 (8)
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2010-05-07_PERMIT FILE - C2009087 (8)
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Entry Properties
Last modified
8/24/2016 4:11:40 PM
Creation date
5/26/2010 11:14:39 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C2009087
IBM Index Class Name
Permit File
Doc Date
5/7/2010
Doc Name
Soils Resource Information
Section_Exhibit Name
2.04.9 Soils Resource Information
Media Type
D
Archive
No
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RULE 2 - PERMITS <br />• • Winevada - Splitro complex, three to 25 percent slopes <br />• Bulkley silty clay, 12 to 25 percent slopes <br />• Cryoborolls, cryorthents soils, rock outcrop, 25 to 99 percent slopes <br />• Winevada fine sandy loam, 25 to 65 percent slopes <br />• Impass (formerly Binco) silty clay loam, 12 to 25 percent slopes <br />• Yampatika silty clay, 25 to 65 percent slopes <br />• Phippsberg (formerly Aaberg) clay loam, 25 to 65 percent slopes <br />• Bulkley silty clay, three to 12 percent slopes <br />• Yampatika silty clay, 12 to 25 percent slopes <br />• Dunckley- Skyway complex, 25 to 65 percent slopes <br />Map 2.04.9 -M1, Soil Types, shows the locations and boundaries of the mapped soil units within the <br />general PSCM permit area. Table 2.04.9 -T1, contains the acreages of each soil map unit within the <br />PSCM permit area. <br />Over 17 percent of the proposed PSCM permit area is mapped as the Winevada - Splitro Complex <br />with slopes ranging from three to 25 percent. A soil complex consists of areas of two or more soils, <br />so intricately mixed or so small in size that they cannot be shown separately on the soil map. Each <br />area of a complex contains some of each of the two or more dominant soils, and the pattern and <br />relative proportions are about the same in all areas. The Winevada series is a moderately deep soil <br />formed in residuum and colluvium derived from sandstone. The soil has approximately 24 inches <br />of fine sandy loam and loam textures over weathered sandstone bedrock. The Splitro series consists <br />• of shallow soils over sandstone that is formed in alluvium, residuum, and eolian deposits. <br />Approximately nine percent of the PSCM permit area is comprised of the Bulkley silty clay series <br />which consists of a very deep soil formed from alluvium derived from shale. These soils can have <br />B horizons at depths greater than five feet. However, borrow depths can be limited due to high <br />percentages of clay size particles. Soils more prominently mapped near or in the proposed <br />disturbance area include the Impass silty clay loam, Phippsberg clay loam, and a reclaimed area <br />classified as Arrents ( Arents) to the suborder level only. Arents are poorly developed soils which <br />have three percent or more (by volume) fragments of diagnostic horizons that are not arranged in <br />any discernible order at depths between 25 and 100 centimeters. <br />Site - Specific Soils Mapping and Characterization <br />The Order I soil survey map of the PSCM disturbance area, conducted by Jim Nyenhuis, is presented <br />on Map 2.04.9 -M2, Order I Soils Survey — Surface Disturbance Area. Based on the available Order I <br />soil survey, the existing soils which have the potential to be disturbed by mining and related <br />activities are limited to nine soil mapping units (approximately 391 acres). Two of these map units <br />(approximately 232 acres) are reclaimed land and/or previously disturbed lands, one map unit is <br />classified as rockland and one map unit is classified as open water. The majority of the remaining <br />five map units consist of the Binco clay and the Aaberg silty clay. The Binco soil series has been <br />renamed the Impass and the Aaberg soil series has been renamed the Phippsberg in this area due to <br />changes in soil taxonomy and available weather data. <br />• <br />PSCM Permit App. 2.04 -120 Revision 12/17/09 <br />
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