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<br /> <br />'" ",' <br />,""'"- <br />kind of rocks they penetrate. :\Iuch of what he <br />i~ intl:r~:>ted in i~ helOh the depth of ordinary <br />exc3\"ation~, and he cannot afford to drill a hell <br />or te"t holt- in ewry plan' where he need~ infor- <br />mation. Records of wells wht'f(' the driller ha... <br />carefully lng-g:f'd tht. depth and tyfX' of different <br />rock ~trata arc helpful. A really t1-.eful w('1l record <br />will include the following: sampl~ of thl' rock...; <br />information on which "trata yield watcr and how <br />freely: "here the \\ater Ie\el ..tood in the well a-" <br />each "uH"e"..i\.dy deeper 'lratum was petlclrated: <br />and data -from :1 pumping: or hailing te:->t of earh <br />water-hearing- "traturn shoh ing hm\ much wate:r <br />W.I-" yielded and hm\ much lht. water Ien'llow- <br />cn'd at the ~>in:11 rate of pumping or hailing:. <br />The hydwlog:i~t \\ ill thcn make a contuur map <br />of tht, u'ata tablc. The water tablt, is the top of <br />the zont' of s.1.turation- the zonc in which all the <br />rock.\. are saturated hith water (6,C:. 3). The <br />hydrolol.,>iq mea.,urC'!i the depth from the land <br />surface to the water table at wells. :'\cxt ht' de- <br />termines, eithn from a topographic map or by <br />"un'eyillg'. how high Iht' land is abon' "t'a le\.el, <br />Finally'. he draw.. lin~ [0 ("onnen all the point~ <br />of equal elt'vation of the wal("f table. so that the <br />map -"hows the "hape of the watn table, in the <br />same way that a \Opographic map shows tht' <br />shapt. of the land ..urfalT, Tilt. waitT-table map <br />is {'specially impnrl.1nt !Je{'3U-"l' it gin-s a c1ut' not <br />only to Ihe deplh below which ground watn i" <br />~tored, hUI also In tht. din'clioll in "hich tht' water <br />is mO\lng, H then' is am- slope tD the water tabl~. <br />tht' water mows in the direflion Df the slope <br />(fig, el), <br />".hert' there art' no welk or not t'llOugh infDr- <br />mation Dn ('xi~ling ont"'. the hy'drolo.c:ist may haw <br /> <br />, .\ <br />~ \) <br />~', <br /> <br />. _ , 0 o~ : o. 0 <br />~ .. .~. <br />'0. ...... . <br /> <br />. .0 ~ .-. <br />" ,< < t ~ ,.0 <br />:_--~- ..... ~ <br />- ....:::--==-~"'::.."'::..-::.- <br />-... -- <br />-:::'-:- <br /> <br />-- <br />.... --: --- -...-- <br />:~....- --...........:::::~:...-- <br /> <br /> <br />. <br />". <br />.............. <br />" - <br />'..~-- - - <br />-:;..::::-:-===;:::... <br />. -- <br /> <br />II I' <br /> <br />FIGI'RF 'J.-Fold..d alld d15plaud Tock,_ <br /> <br />4 <br /> <br />to put down some t("<ot holes. If only a shallow <br />holt' has 10 bt. put down. a small power auger. <br />hhich hill bore to a depth of aOOm 100 fect. can <br /> <br /> <br />A,-SMAll STREAM WHERE IT fiRST HAS <br />WATER IN CHANNEL <br /> <br />- <br /> <br /> <br />. <br /> <br />lW<lI..,t<lbl.. <br /> <br />~D <br />~~ <br />,~-,;;;:;;O~ <br />...".,' <br />-:r~:' <br />'oS <br /> <br />....o....no.. <br />ld"'..,,,onol <br />fro.. <br /> <br />-._.t",,~':.L. . <br />. .'" <br />!. ~>~ ~i~~}~~t'"' <br />':s..~_, ..~ <br />-'.~,_.-;- .""" <br /> <br />"i;lj' <br />...''"' -~ <br />~, .' <br />..... <br />',:r-.I. <br />i;;.'. <br /> <br />'. <br /> <br />'.'_. <br /> <br />.....,i:: <br /> <br />B,-DRY ZONE LIfTED UP TO SHOW <br />SURfACE Of SATURATED ZONE <br /> <br />FIGI'RE 3--Th~ u:r:rn tab/t' and mor'(ment of <br />l:round .t.ala. <br /> <br />