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2018-01-23_PERMIT FILE - C1981041A (4)
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2018-01-23_PERMIT FILE - C1981041A (4)
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Last modified
12/13/2022 9:05:43 AM
Creation date
3/8/2018 10:44:46 AM
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Template:
DRMS Permit Index
Permit No
C1981041A
IBM Index Class Name
Permit File
Doc Date
1/23/2018
Section_Exhibit Name
Tab 10 Vegetation Information
Media Type
D
Archive
Yes
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3.0 RESULTS AND DISCUSSION <br />3.1 ENVIRONMENTAL CHARACTERISTICS <br />The climate of the area is arid to semi-arid, with a precipitation <br />at Palisade of about 9 inches a year. See Table 1. Precipitation at <br />Palisade is distributed somewhat uniformly throughout the year, with a <br />s I i ght peak dur i n~y'^.;5ep'~'EtabeLSy -~R$..nG~fjee . The growing season i s <br />relatively long, extending from the beginning of April through the end of <br />October, Z00 days. <br />The Colorado River, flowing southwesterly, bisects the permit area. <br />Numerous ephemeral streams in narrow, steep-walled canyons drain the permit <br />area. Jerry Creek and Coal Creek flow easterly to the Colorado while <br />Rapid Creek and an unnamed stream flow north and westerly, The topography <br />is rough and steep with sheer cliffs hundreds of feet high common to much <br />of the area. Mesas are common above the 6,000 foot elevation. There is <br />one extensive mesa at the 5,000 foot elevation just to the east and south <br />of the Roadside Mine. The elevation ranges from a low of 4,800 feet along <br />the Colorado River to a high of about 7,300 feet. <br />1 The geology of the permit area is characterized by sandstones and <br />• shales. The three study areas are all within the Mesa Verde group of the <br />Cretaceous age. Younger formations above respectively include the Wasatch <br />} and Green River, both of Tertiary age. <br />1 The lower elevations of the permit area are mapped as saltbush- <br />* •greasewood by Kuchler (19661 and as saltbush by ShelFord (19631. Higher <br />!] elevation potential natural vegetation are identified as mountain mahogany- <br />oak shrub by Kuchler (19661 and as pinyon-juniper by Shelford (19631. <br />~ These mappings may accurately depict the regional climax vegetation types <br />but are not of sufficient detail to reflect vegetational changes related <br />~ to exposure and substrate variations. <br />' The permit area and adjacent sites are characterized by nine different <br />vegetation types. A riparian woodland with cottonwoods Pvpu.(ua de.Ltvide.~, <br />wi I lows Sa.lix spp., skunkbrush qua davmatica ssp. #~ei.Cvbata, and chokecherry <br />• /oaunua v<agiru ana is present in moist habitats along the Colorado River and <br />extends as a narrow band into the tributary drainages. Moist Stream <br />• drainage habitats along the Colorado River and its tributaries with salty <br />soils as well as saline seeps on some slopes are characterized by a black <br />greasewood $aacvGatue veitm<cu.Catu~ vegetation type. Fourwing saltbush <br />• A#icipC¢x cnne~cvnn, alkal i seepweed $uaeda cf. ,fiuvltiw~a, and cheatgrass <br />l3avmue #ectvzum are also common in this vegetation type. A rubber rabbit- <br />! brush Ch~~evthamnua nau4evau~ vegetation type occurs on streamside distur- <br />~_ bances in Jerry Creek and Coal Creek. This linear vegetation type, too <br />small to map, is contained within the greasewood vegetation type. <br />• The steep slopes, dry and often unstable, are characterized by a <br />' shadscale shrubland vegetation type. This community occurs on all slopes <br />-5- <br />
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