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2020-10-12_GENERAL DOCUMENTS - C1981010
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2020-10-12_GENERAL DOCUMENTS - C1981010
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Last modified
10/13/2020 8:24:40 AM
Creation date
10/13/2020 7:50:41 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
General Documents
Doc Date
10/12/2020
Doc Name Note
For PR10
Doc Name
Proposed Decision and Findings of Compliance
From
DRMS
To
Trapper Mining Inc
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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