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a~ 4 0 <br />c y <br />' o ~ a c <br />Y ~ ~ O <br />U L VI ~ a+ <br />C ~ ~ of <br />A ~ '" ~ - v <br />L ~ N to Y <br />8400 ~ a v u N i 8400 <br />~ c Ai <br />~ a v v ~ v <br />~ '- <br />;' 8200 j /~; ~ N E ~ ~ _°' 8200 <br />fee[ ~/.~~, Feet <br />8000 ~~ ~ ~~~~~/ ' ~ o o' 8000 <br />i. j%j...... / , . <br />' O L Q~ <br />7800 . / • ~ /... /~~ %/~~ . I 7800 <br />' 7600 ~ /%/~ / ~ ////// ~/ 7600 <br />I /, / <br />Williams Fork Formation Iles Formation <br />' Scale: 1"=500' <br />{ ' Figure G.8(a). Cross section showing units of the 1';illiams <br />Forl: and Iles Forr:~ations in Sunlight ?`line. <br />I' , <br />I' <br />(b). Explanation to Figures G.S, G.6, G.7 and G.8(a) <br />' (,hl AlluvitLm <br />' Tb Tertiary basalt lava flows undifferentiated <br />'Itvo i9asatch Formation-0hio Creek Conglomerate <br />Kwf Williams Fork Formation <br />Ki Iles Formation <br />' Kr Rollins Sandstone 6fember <br />l;m Mancos Shale <br />Kc Cozzette Sandstone Member <br />I, ---Geologic contact, dashed where approximate <br />4 1° <br />--L Strike and dip <br />l' -~ Mine portal <br />SL-R-1 Overburden sampling station inside mine <br />I' O Sandstone <br />L' ® Coal <br />L D Shale <br />Shaky sandstone or sandy shale <br />I' <br />2z <br />