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There are three major soils types at the Niew Hodzon Mane 2 area (sce Soils Map of the. perrm <br />application): Progresso-Bond Complex, 2 to 1.5 Pa=t slopes, Bari sandy loam, 1 to 4 percent <br />slopes; and Haptaquolls, 1 to 3 percent stages <br />The Progresso-Bond complex is comprised of Oil peroent Progresso, 40 peroet?t Bond, 10 percent <br />Bari (sae below), '5 percent Travesilla, and 5 perxat Bowdisb series soils. The Progresso series is <br />classified as a fine-loamy, mixed, mesic, Ustollk 1Haplargid. The Bond series is a loamy, mixed, <br />tnesic Lithic Ustollic Haplargid. The main dim between these two is the distance to bedrock; <br />Bond soils are shallow (17 to 19 inches to bedr k) while Progresso soils are fairly deep (36 inches <br />to bedrock). "This complex, is found on goody to strongly sloping irrigated uplands over much of the <br />New Horizon Mine 2 area. The soils are shallow to moderately deep, well-drained sandy lomns <br />formed in sandstone derived alluvium. Topsoil quality is good to an average depth of 2.1 feet. <br />The Barx soil is found in the southeast <br />-t rife as a fine-loamy, nuxJ j. mesas <br /> <br />2 hermit area. It is <br />it <br />been <br />and was =latu ed as <br />the USDA - <br />Z. Part <br />with a <br />service), <br />Tbeepbeumal "nages of the New Horizon Mine 2 area contain three families of Haplaquoll sails; <br />Uthic, Litbic/"f'ylric,, and Typic Haplaquolls. The loamy, mixed rnesic, i ithic Haplaquolls are found <br />in the-upper aches of the swales in the area end are the shallowest of the three series OMdrock at l l <br />inches). LitlricfTypic F oils (coam loamy, mixed, mesas, moderately deep Typic liaplaquolls) <br />g n th of about <br />are found in the maid to lower reaches of ?hwaies and ?rthe low r reaches of <br />24 inches: The fine-loamy, mixed, meat , deep Typ HaPlagnalls are found the swales and along Calamity Draw. These soils We sandy loam and barn textu ellto a s b depth of <br />about four feet with sandy clay loam below that. The soils were classified as HapbAudu water. Tli <br />soil wetness. However, this diagnostic factor is artificially induced because of irrig <br />soils were foamed in the alluvium of the swales. Pair to good quality topsoil exists in the swale areas <br />in thirAmess from 1.2 to ovtr 4 feet. <br />In association with Permit Revision No. 5, a ntwv soul survey encompassing approximately 376 acres <br />ved New Horizon 2 persuit area was conducted. The Order 1 <br />to the northwest of tine previously apprn differ fironn previous surveys due to recent <br />survey was conducted in 1998. Map unit designations <br />units idettGtfied in the 1998 survey y include <br />changes in NRCS soil taxonomy. Dominant map atrdMon in lue <br />Bowbac.Bowdish Complex. 0 to 3% slope, Davey-Barx complex, 0 to 3% slope, <br />Sandy Loam, 0 to 10% slope. The Bowbac-Bowdish and Darvey-Bari complex units are used <br />primarily for irrigated hayland or pastureland. Portions of the Motuemo unit are developed for <br />irrigated pastureland, while other portions of the unit support native sagebrush rangeland. Other rmap <br />units from which soil salvage wilt occur within the revision area ed £ ? laeiswal?En and seuepts <br />A?ssbeiation, which occurs primarily along artificially subirrig _ will bt <br />upland soil types which support native sagebtus ? rrangeland. A two lift salvage elatively upland soils F'Valley City- Rock <br />utilized on all map units. with the exception of tw y shallow <br />10