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i <br />JUL-26-99 MON 12115 PM FIRST COLORADO MTG, FAX N0, ~~3 444 3972 P, O1 <br />'~ ~ III Illlllllllllllll <br />Presentation to I>ivision of Minerals and Geology (D1+tC,) regarding Pcnuit Applic:r[iun 111-99-018. <br />Facu based on Lneasunmcnu front topographical map, visual measurements, and recorded Icgal <br />documents, <br />L.lxationofGravelYit '1GN 'tJlli)1 OW,IOS,NE'b5,3,125~~, <br /> feet cast oL thl' west line, 1,871 <br /> south of the north lice <br />m <br />Location of Spring Storage Box Wpty~. 1'GN, R90W, 105, Sr ''/.,yof the <br />il <br /> ~7~~ ~{Q~,,rµ,~. NW '/. section at a point 21 G7 i <br /> feet east of tkLC wLS[ line and i <br /> <br />~ 1,7D3 feet south of QLC north line 'i <br /> _ ofSeetiml ]0 <br />Llcvation of Gravel Pit _ <br />- G,377 feet (23 feet el its decpast) <br />Distance between nearest -~ -_ 875 Ccct to springbnx (serves six <br />su~ucllirc mtd gravel pit residences as water sourer) <br /> 8SD Il'Ct frnlll 1315CI1p b1111th11~' <br /> 2,000 icel from Ashbaugh <br />_ bnildins <br /> <br />I)istaiiccbctwcen water salrees __ <br />~ _ __ <br />S7S fuLa to springbnx y <br />andpj~avelpit I11asure;; t <br />I•;Icvation of spring _ ,~ <br />M' G,3G0 feet at springbnx <br /> yo.~ G390 (estimated origin out of <br />_ ground) <br />UiCli:nnec in elevation of spring w 17 feet between spring>boc and <br />and gravel pit gravel pit <br /> (13) fee[ bchvccn origin of spring <br /> from the g[ouud and ills gravel <br /> pi[. The spring is higher )han the <br />,..__ _ __ gravel it in this instance. <br />68oioa~ 4 gelaulW to uolslnlp 1 ~ ~t~ (~S~~i nr, ~c m n 1 Ftct.~ <br />sssi sz inr 1~ ;303 - g~3a~~c,co <br /> <br /> <br />