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11 <br />DAUB 8 ASSOCIATES <br /> <br />CONSULTING GEOLOGISTS _ <br />.-'±"I~Y'~'•"':9lrfj~7-•,; <br />, <br />; <br />~ <br />_ ~~' v ' ... ti•Rtr... 1980 SOUTH 6ROAOWAY <br />ION.CO 8t507~9593 <br />~~~~ <br />~ <br />~ <br />~~ <br />~ ~~~"~~-' <br />1 t <br />" <br />' <br />~~' ~'~ <br />"'~ J03 <br />11-096g <br />e{q ~ {eedlg{ pr{h_ ~ Sen t_ ~ Coggents <br />4-30 4.16. I.2 I 1 overly! vg tha cevitie• batrseg <br /> Sps S4¢ sf Sps l4j4! sad eeg 34:1! <br /> fees lpsye shg di •galutjvv <br /> gsftsea_ The rock quality above 41 <br /> this interval ha• already been <br /> "signlfleently reduced" by nsturel <br /> processes. <br />4-30 9.16.1.3 1 1 9odlus •lverel• rlthly the L-56 <br /> ssa, lying. .. <br /> She L-6{ 1• a bed rlthin the L-6 <br /> :one. <br />4-70 4. le. I.4 L I quellty of the refer In the 49 <br /> lorerlegt pelt pt the lower <br /> aquifer because... <br />N It le entieiDatad that Che water <br />N <br />` leeedlete Ly above the dlesolutlov <br />~ •urfece is the only pert of the <br /> lover equlfer that would be <br /> effected. <br />4-30 4.18.1.4 I 2 7hle Dotentlel lepeet would occur <br /> oa1T gfser ev greg gaeg6rj6{ 100 <br />0! <br /> _ <br />{ j000' rgs datelogeg agd ronld be <br /> the result of cavity collapse. 38, <br /> 49, <br /> The condltiov would •teb111ze )Q <br /> after a cerlely Deriod of ties wd <br /> would not "persist for the <br /> foresee eb le future". <br />4-90 4.18.1.5 7 1 Mhet l• the eLM referrlvg to when <br /> they •tete "water eonteeinetivn"? <br /> She water would have a slightly 14 <br /> higher SO6 value. <br /> Tha creel eetavt of tha effected <br /> lands is not evticipeted to be <br /> very let{a. <br />2l <br />ii <br />DAUB b ASSOCIATES <br />CONSULTING GEOLOGISTS .-;+'1 ~"Lid~':~1;:6}~+..~.~ <br />•' ~ ~~ ~o taeO SOUTN eeonowAr <br />.:.,.: :,..~... R,~.. <br />r'""' '~~1Y,!>"y'R t.. GRAND JUNCTION. CO fitSOJ~9697 <br />j!{q ~ 9aedig{ <br />9-91 4.16.1.11 <br />4-91 4.18.2.2 <br />4-31 4.18.2.2 <br />4-32 4.18.2.30 <br />4-32 4.16.3.2 <br />4-92 4.18.9.2 <br />Pr{h_ ~ 9ev t_ 1 Coggeg is <br />2 1 Cousrelel-wale •odlus <br /> davelopvent •Ight ndversely <br /> lvfluence g ggelj grog jeI the <br /> developvent.... ]8 <br /> The •urfaee dlsturbevice of the <br /> co oerclel-seals •odiuv protect t• <br /> evtlelpeted to be •ivisel. <br />1 9 quellty of the rater <br /> jg~edigtelf gboT4 Ip9 gj4{sjgsls{ <br /> gurfsce iv the lover aquifer... <br /> 49 <br /> The lorervost pert of the lover <br /> equlfer L• tha only pert of the <br /> hydrologic •ect ivv rhich rauld De <br /> effected. <br />1 4 Shl• potential leDect would !pear <br /> sitar glale{ hgd de.eiolgg !! ![!! <br /> 1000' { 1000'. <br /> 38 <br /> It t• not evtielpeted that thane 49 <br /> eonditiovs rould persist for the )Q <br /> foreseeable future •ivice <br /> cavdltion• would stabilize over <br /> e Deriod of five. <br />1 1 ... setivieles in end •rouvd the <br /> eves gg= shift to... 49 <br /> It 1• not kvorv Sf recreettovel <br /> ectlvlClee would deflvltaly •hlf! <br /> to other erase. <br />1 2 •• 9uellty of the velar <br /> j!lsgjetejg spots tpa 9jge4jsijle <br /> •uEfsce ;g the Isrerlpgt gert of <br /> <br />shg IeweT equlfer because of the )Q <br /> evount... <br />1 3 The coadltioe• would •tebllle• <br />22 <br />