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2012-02-28_REVISION - M1980244 (97)
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2012-02-28_REVISION - M1980244 (97)
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Last modified
8/24/2016 4:49:13 PM
Creation date
3/9/2012 12:41:39 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
REVISION
Doc Date
2/28/2012
Doc Name
VOL. 3, Appendex 3: Baseline Technical Report
From
CRIPPLE CREEK & VICTOR GOLD MINING COMPANY
To
DRMS
Type & Sequence
AM10
Email Name
TC1
Media Type
D
Archive
No
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Baseline Technical Report <br />ARCADES Report for Soils and Biological <br />Resources, MLE2 Project Area <br />2.1.9 SI. Ivywild- Catamount complex, 30 to 70 percent slopes <br />Within the Cresson Project area, these soils are found on north - facing mountainsides <br />in association with the dense conifer - dominated woodland vegetation type, and some <br />areas of transitional aspens. Both unit components have formed from colluvium and <br />residuum derived from granite. Both soils are somewhat excessively drained, <br />shallow, and consist of gravelly sandy loam or loamy coarse sand. This soil unit is <br />not present within the survey area. <br />2.1.10 Sz. Seitz very gravelly loam, 20 to 50 percent slopes <br />Seitz series soils are found on mountainsides with the dense conifer - dominated <br />woodland vegetation type and in some areas of transitional aspen forests. Typically, <br />these soils consist of very gravelly loams and clay loams to a depth of approximately <br />24 inches, which overlie a subsoil composed of very angular cobbles. A thin surface <br />layer composed of decomposing conifer needles (duff) is often present within the <br />survey area. Approximately 24 percent of the survey area (103 acres) is comprised <br />of this soil unit. Portions of the northern Cresson Project area previously mapped as <br />Seitz series soils have been disturbed by timbering and land- clearing operations. <br />2.2 Growth Medium Resources <br />As part of the ongoing mining operations at the Cresson Project, CC &V salvages soil <br />that is suitable for assisting with revegetation. Soil recovered for use during <br />reclamation is termed growth medium. The soils information presented in Table 2 -3 <br />is generally representative of growth medium within the District. However, the depth <br />figures for these soil map units are not representative of the depths that can be <br />salvaged. The volume of growth medium that can be salvaged from areas proposed <br />for disturbance is based primarily on the depth of the upper soil horizons, but also is <br />influenced by slope, surface rock, areal extent, and vegetative cover. Regardless of <br />these factors, depths of less than 6 inches are typically considered to be <br />unsalvageable due to the large size of the equipment used to recover soil for <br />reclamation purposes. Growth medium depths vary greatly depending on their <br />position on the terrain, with the shallowest soil on the upper slopes and deepest at <br />the toe of the slope. The presence of rock outcrops in some areas renders salvage <br />operations unmanageable. By removing large roots and stumps and pushing slash, <br />unavoidable mixing of the soil horizons occurs. Many soils within the project area are <br />very to extremely cobbly at shallow depths, which may limit their usefulness as <br />growth medium during reclamation. Field tests of soil pH did not indicate any <br />additional limitations to use of project area soils as secondary growth medium. <br />CCV Baseline Soils Biology Resource Report (11- 17- 11).doc 9 <br />
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