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( layers . The lowest potential aquifer is the Rollins sand- <br /> stone member of the `Iesaverde Formation . Tne Rollins is the <br /> base of the coal Series , overlieing the Mancos Shale <br /> Four distinct coal beds have been identified <br /> in the Coal Basin strata : the lowest is the bed ; above <br /> it , the "B" bed ; above it the "M" or diddle bed; abode it <br /> the "rlacita" bed . Coal is mined from the B bed and the <br /> ggee Isopach maps at Exhibits III-D-1 and III-D-2 for <br /> Middle beds . / In addition, fragments of the "Sunshine" seam, <br /> those two seams . <br /> which is mired some 10 miles to the north (by another <br /> operator) , have been detected . The coal occurs above sand- <br /> stone units . The Rollins Sandstone is beneath the ri and B <br /> beds ; the diddle Sandstone is beneath the Middle bed ; and <br /> the Upper Sandstone is beneath tn.e Piacita bed . <br /> The .•zesaverde is zustor-naril.: described in <br /> terms of a lower formation , called the Iles , and an upper <br /> formation called the Williams Fork. The Iles Formation <br /> overlies the Mancos Shale and, as noted , the Wif ll'-a-ms Fork <br /> Formation overlies the Iles . <br /> The Iles Formation consists of two sandstone <br /> me �beTj i'7idt'd by a 1 , 000 ' " tongue" of Shale . The lower <br /> member , the Cozzette, is a 6-foot layer of verb' tine grained , <br /> si I t v Sandstone , which overlies a 40-1ooc thick layer of <br /> s=1t; to sandy shale . <br /> The uvoer sandstone member of the Iles forma- <br /> tion known as the Rollins is 120 - i-0 ' ?_--hi ck , and worms <br /> the base of the coal series . s-ale tongue of 5 ' to 30 ' <br /> � f% <br /> 9 <br />