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<br />• <br />• <br />OPEEK <br />w `~~~ <br />~ •.e <br />'~. ~, <br />U i ~ ~ ~i ~ <br />o <br />`a <br /> <br />o <br /> <br />OF v <br />i I <br />' <br /> <br /> <br /> <br />08' <br /> <br /> <br />i ~ <br /> <br />Meeker <br />40 <br />,200 ~ <br />~ ~ <br />' <br />, 1 <br />-L CI ~ <br />'µ {/ <br />~ 4 <br />` I alb <br />U <br />~//~ <br /> <br />Z <br />C G, ch • • <br />o <br />m ._ <br />5 `s o <br />a • $ <br />~ <br />Y <br />5~ <br />yy <br />3 1 • <br />~ G <br />/ ~ <br />t . <br />i <br />~] i <br />i ~c ~ • U, <br />I 0 ^~ < ,~ <br />/ <br />~ <br />I ~ / / \ <br />Base from U.S. Geological Sun~ec ~ <br />/ - <br />State base map, 1A5~ ' <br />LEGEND <br /> N <br />-300- Line of equal saturated o s ]0 ~11LE5 <br />thickness -Interval 100 feet o ~ M <br /> ErEas <br />• Well <br />~1 American Soda <br />lU Piceance Site <br /> (Robson and Saulnier 1930) <br />• Figure 7-13 Saturated thickness of the Parachute Creek Member <br />above the Mahogany Zone. <br />