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• <br />designed to confirm that the operation is not causing material damage pursuant to <br />Rules 2.06.8(5)(a)(iii) and 4.24. This information has not been provided in the PR-03 <br />application. <br />Colo wyo Response: <br />Colowyo has had multiple discussions with the Division regarding the Gossard <br />Loadout area designation as an alluvial valley floor during the course of negotiations <br />involving TR-72. Colowyo continues to contend this area, including the Collom area <br />coal transport road, etc. can no longer be described as an alluvial valley floor due to <br />the natural massive down cutting of Wilson Creek's stream channel in the mid-1980's <br />and subsequent lowering of the water table, precluding "re-establishment of hydrologic <br />function" to pre-mass wasting event conditions. Colowyo has provided the Division <br />with additional information that illustrates significant downcutting of the stream <br />channel both above and below the intended path of disturbance as illustrated on Map <br />25E Sheet 5 of 9 (Collom Access Road Plan/Profile). Utilizing the evaluation criteria <br />and conclusions reached for alluvial valley fill determination in the Collom Gulch and <br />Jubb Creek drainage areas, Colowyo has amended Section 2.06.8 to reach the <br />reasonable conclusion the Gossard Loadout Area and area to be disturbed by the <br />construction of the Collom Access Road do not qualify as alluvial valley floors. The <br />following commentary has been added to the end of Section 2.06.8: <br />• <br /> <br />"The same conclusions may be reached for the area of proposed disturbance for <br />construction of the Collom Access Road in the vicinity of the Gossard Loadout Facility <br />(Map 25E Sheet 5 of 9): <br />• Alluvial materials are present in the valley bottom of the Gossard Loadout complex, <br />and lower reaches of the Lower Wilson drainage, but the materials are intermixed with <br />significant fractions of colluvium and sheetwash from adjacent slopes and the mass <br />wasting event experienced in 1983-1984. <br />• Based on an average depth to groundwater of approximately 21 feet for the existing <br />alluvial groundwater well know as "Gossard Well" (2009 Annual Reclamation Report) <br />since 1983, subirrigation within this valley bottom is very limited. Monitoring well <br />MW-95-02, located in the area hydrologically above the proposed road corridor <br />portrays similar depth to water conditions averaging 25.1 feet from 13 measurements <br />taken in 1996, 1997 and 2005 (Table I - Groundwater Parameters, from August 16, <br />2005 letter to Jim Stark from Walsh Environmental). <br />• Active erosion in the stream channels is causing further incision and reduced flood <br />frequency, reducing the ability of this valley bottom to support any agricultural use <br />other than rangeland or dryland agriculture. There is no evidence of "modern <br />terracing" in the area proposed for disturbance near the Gossard Loadout facilities. <br />• Local and regional agricultural economics are prohibitive to developing irrigation <br />projects within this valley bottom, and such practices are in decline locally. <br />• Historical irrigation activities associated with the "diversion structure and ditch" <br />located hydrologically above the proposed access road path, diverted water around the <br />existing grain fields, under County Road 17, outside the current permit boundary to the <br />Colowyo Mine C-1981-019 <br />page 8 of 16 <br />25 March 2010 <br />Permit Revision 03 - Collom Permit Expansion