Report of Investigations No. 42 ;-,- ,,, I __ I I .I -I- EXPLANATION Decre in ioezometrc levels (November 1959 to May 1962) S L: 0-5 reel [ 10-20 feet S- 5-10 feet 1 More than 20 feet SNELL- ;BUSHNELL', iV > I - I er)),) -MT ~ ~ I K 33.j c-~ [MONT- '" I 7 *-7 I I I NT- III - 5,1tt~lt i~t 107' I- L Lz -~ 4 0 i-I, z zo 0ri o 2 I' r~r 1010 III -- I ~iI 15' ----- 2r A 5 f5 0 0 5 8L O O h e 15' ZEPHYRHILL:f7, I*:5' 10 : 05' 82*00 a-' (n- LAKE- POLK / 2 2 PA" I III, Z "Z 1.- -4I 4h a cW2 1622 -T.-IF I I 1., ES .7 C i u Ioh 0 I 2 3 4 5 6 7 8 9 10 ml, Figure 37. Map showing decline in piezometric surface of the Floridan aquifer, November 1959 to May 1962. 1'30 28o45 40 1 122 itz Lok rAWQT .AA ase token from U S Geole Icol Survey toagrayphIC quadronges 25' -,, .2 : "T - GE COUNTY 41COUNTY g20 ;P LK 15' o i. Z 10, J 05 -2 2 77- 35 81'3U 1^ __ _\ _ V-.f^- l-t_^,^ 1.~l' ^ 1 4;AIES ~' -^ - S^ -11 ^ ^"" - -z:-:- 1-__1-_-1 n-I 2800' 35' 81 50' C II 7 I 4r L ra- C-I- z- D 0 -0 Q 2t -o r > - ---- _ r I I L '` ' T b2 4. -t Rd, c-c I I.L I I I I I I It tn I - I- Ij. I ._~ou_~ .~~--L__ '-117~~f~BLi: i. I-I~ .,. _. - a ---I -. --14~ C` " 8200 Ji ll~i c -A~r- p o p po 4 _J I I I.