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<br /> <br /> T14ffiE 1 ~ <br /> \ <br />S[IIR~F1ItS( OF SPRIldG SURVEY OFC'CA <br />~ 2) ~[~a~ts <br />~ <br />be 1) Flow (crcxnl Field ParmnetP YS <br />1 0.5 T = 5o'C Fla+ing for short a; ~a*+~ in drainage bott.®. Fliotite gneiss <br /> sc = 450 outcrop on west side of drainage. Drainage follows NE-SW <br /> pH = 7.4 fault zore. Neari~y shaft itRersec.'ts water table. <br />2 0 - No flow observed. Neatest outcrop is biotite gneiss. Silting <br /> is locate3 in probable N-S fault zo¢~e. <br />1 <0.5 T = 9qC Two minor seeps. Deciduws trees growirzl near seeps. Neatt+y <br /> sc = 065 outcrop consists of altered biotite gneiss. Seeps emanate <br /> pH = 7.5 frria N-S fault zone. <br />4 0 - Cattr~rn~ood area. No flow observed. rL>ct~ gtern vegetation in <br /> area. Fault juix-tune? <br />5 0 - Itvn oucide spring. Iron a;.,aa cobbles observed in cx'eek but <br /> no observed flaw. <br />6 0 - No flow observed. Fliatite gneiss float. <br />7 0 - e~amd is saturated. However, no a; ~**+~hle flow was <br /> observed. GYY'a..s very gzeen. Pink granitic gneiss artcivps <br />nearby <br />8 11 T = l0gC Series of springs along unnamed Rico Seoo tributary, No near <br /> sc =580 by outcrop was observed. <br /> pH = 7.8 <br />9 <0.5 T = 15aC Iron oxide spring. Very minor flow. No nearby, outcaop. <br /> sc = 610 <br /> pH = 6.8 <br />1) NYmir+r Iefers to locati~ on Figure 1. Stuvey Ci7l13UCted on May 13, 1989. <br />2) T = tetQerature in degrees C.enkigrade. <br />sc =specific oonductarne in micro~os/ao. <br />pH = in standard units. <br />