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<br />from 26 to 77 feet below the land surface. <br /> <br />Thedep.th ,towa.t'et~ranged~c" <br />. <br />The'Cotlfigliration Of' the' <br /> <br /> <br /> <br />} t?,~r}::;. ~~ <br />F~,:{f"} <br />'o'l"jtj, <br />'-'-'~':--~It <br />',!!::j~~~, <br />n; ,',',;:- <br />iV <br />;j'-'> <br />, ''!j;:?' <br />~~ ;',~;;~, <br />-ttl:J <br /> <br />i <br /> <br />1~2~Sg: <br /> <br />.""-- <br /> <br />Core samples 'were collected from 14 of the t'est holes 'at 122, " <br /> <br />selected intervals. Core samples were obtainedby'drivinga"'split"'" <br /> <br />spoon core b~rrel ahead of the auger bit.1.ab,oratory, ,moisture det~rw' <br /> <br />, , <br />minationswere made ,!n core samples-"'SS by the U.'S. Geological Survey' <br /> <br />Hydrologic Laboratory, in Denver and 67 by the.Gentral,Great ,Plains' <br /> <br />Field Station. <br /> <br />All test holes were converted to observation wells by casing with <br /> <br />Ilj-inch steel pipe equipped with a sandpoint. The wells wereclearied" <br /> <br />, and develope~ by pumping water' 'downtheca"ing, <br /> <br />were open to'the aquifer. Water'levels in ,the observation"wells were' <br /> <br />measured on July 3, 1969. <br /> <br />',-" <br />fl- <br />- t(: <br />~" <br /> <br />water table and location of test holes are shown on figure 2. <br /> <br />A <br /> <br />sununary ofrErsults oftest-holecaugering at the Fi<:>ld Station'is giv,en ' <br /> <br />in tab le 1. <br /> <br />6 <br /> <br />,..;... ~,-_,_il.__.. _~'." <br /> <br />; ,/0: <br />/;a:....A.L~ ;k,----<...di.., .:-',",-_ ..j,.~,."~'''"___,_~.__~---,,,- <br /> <br />--'";,,.. <br /> <br />/.- ~ <br />