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2020-10-12_REVISION - C1981010
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2020-10-12_REVISION - C1981010
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Entry Properties
Last modified
10/13/2020 8:24:40 AM
Creation date
10/12/2020 1:34:08 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Revision
Doc Date
10/12/2020
Doc Name
Proposed Decision and Findings of Compliance
From
DRMS
To
Trapper Mining Inc
Type & Sequence
PR10
Permit Index Doc Type
Findings
Email Name
JLE
RAR
Media Type
D
Archive
No
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The climate of the Craig, Colorado area is characteristic of semi-arid steppe regions. Average annual <br /> precipitation for the town of Craig, six miles north of Trapper, is 13. 5 inches, of which over one <br /> third is snowfall (averaging 66. 5 inches/year). Trapper Mine's average annual precipitation is 16.7 <br /> inches. Mean annual temperature in Craig is 43°F, with recorded extremes of-45°F and 100°F. <br /> Winds predominate from the west,but are locally modified by topographic features. The growing <br /> season for the area in the vicinity of Craig averages 77 frost-free days. <br /> Soil Types, Characteristics and Distribution <br /> Three soil orders are found in the permit area: <br /> 1. Aridisols <br /> 2. Entisols <br /> 3. Mollisols. <br /> Characteristic of fairly steep, semi-arid regions of northwestern Colorado,they represent soils <br /> grading from recently developed soil bodies with minimum horizon development(Entisols)to older <br /> soils comprising well defined diagnostic horizons(Mollisols). Overall,the soils found in the permit <br /> area are relatively deep and well drained exhibiting effective rooting depth ranges from two to sixty <br /> inches. The deepest soils yielding the greatest rooting depths occur in valleys and on the leeward <br /> sides of ridges. Soil reaction is slightly acid to moderately alkaline over the permit area with the <br /> exception of inclusions of small scattered areas with saline substrata. These small areas have <br /> probably formed in place from weathered sodic shale. <br /> Vegetation Distribution <br /> Vegetation in the area grows largely in response to macro-climatic influences of the region. The <br /> north-facing slopes,having moderate to deep soils characterize a relatively mesic moisture regime <br /> and favorable levels of insolation throughout the year, exhibit well-developed mountain shrub <br /> communities. On colluvial toe slopes, communities dominated by sagebrush and grasses occur. <br /> On the south-facing slopes behind the ridgeline of the Williams Fork Mountains,vegetative <br /> communities are less developed with respect to cover, density, and production due to the less <br /> favorable soils,moisture regime, and increased solar insolation. The trend in these areas is toward <br /> communities dominated by juniper,pinon,mountain mahogany and xerophytes. <br /> Historical farming and ranching within the current permit area modified,to varying degrees,natural <br /> vegetative communities. Much of the land along toe-slopes and valley bottoms was cleared of native <br /> vegetation and is currently used for dry land agriculture. Most of the north-facing slopes in the area <br /> have been historically used for the grazing of sheep and/or cattle. These activities produced a <br /> mosaic of vegetation communities in the permit area comprised of mountain shrub, sagebrush/grass, <br /> and pinon/juniper. <br /> Wildlife <br /> Fauna are diverse in and adjacent to the permit area due to the wide variety of habitat types and <br /> include: Antelope,Mule deer, Elk, Blue grouse, Columbian sharp-tail grouse,and sage grouse. All <br /> are residents or occasional residents of the permit area, as are numerous types of waterfowl, song <br /> birds and raptors. The area provides habitat and migration routes for antelope, elk and mule deer. <br /> Raptors, several species of game birds, and numerous smaller mammals are found in the Williams <br /> Fork Mountains and surrounding areas. <br /> 8 <br />
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