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spring to early summer declining to low volume base flows later in <br />the year, with short duration elevation of base flow in response to <br />localized thunderstorm events. <br />The geology of the area is an important factor relative to both <br />subsidence projections and evaluation of subsidence effects. The <br />study area is located on the southwestern flank of the locally <br />significant Twentymile Park syncline. The Wadge coal seam and <br />overlying units are part of a sequence of coalbearing strata <br />forming the base of the Williams Fork Formation. This sequence <br />contains, in order of deposition the Wolf Creek seams, Wadge seam <br />and Lennox seam interbedded with shales claystones, siltstones and <br />sandstones. The Wadge seam along with certain units within the <br />immediately overlying sequence may have sufficient permeability and <br />continuity to function as local groundwater aquifers. <br />The overlying member is a marine shale, referred to in Maleki, <br />1987, as "Tongue of Lewis Shale", averaging 600 feet in thickness. <br />Except in areas where faults may affect groundwater movement, this <br />shale sequence effectively acts as an aquiclude minimizing <br />hydraulic communication between the underlying coalbearing sequence <br />and other potential aquifers higher in the stratigraphic sequence. <br />The Twentymile Sandstone, a massive, white to cream-colored, well <br />cemented, cross-bedded sandstone approximately 200-250 feet thick <br />overlies the Lewis shale and serves as a key mapping unit. Given <br />it's thickness, competency, lateral extent and physical separation <br />from the Wadge seam in the sequence, the Twentymile Sandstone may <br />significantly influence the nature and extent of mining related <br />subsidence. <br />The Twentymile Sandstone is overlain by several hundred feet of <br />interbedded sandstones, siltstones and mudstones. These units, <br />along with limited deposits of geologically recent <br />alluvial/colluvial materials form the surficial geologic units in <br />the study area. <br />The following activities were completed to evaluate potential <br />subsidence affects within the designated Fish Creek AVF area due to <br />proposed longwall mining: <br />• Review existing available data <br />• Conduct literature review <br />• Evaluate existing available information <br />• Develop and implement data collection plan for required <br />supplemental information <br />• Project anticipated mining related subsidence <br />• Evaluate effects on designated Fish Creek AVF area based <br />on subsidence projections <br />• Develop and implement monitoring plan to verify <br />assumptions and determine effects <br />The information presented in the technical revision represents the <br />completion of the above activities, except for the installation of <br />the proposed monitoring systems. The hydrologic monitoring system <br />