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' i•Iemo to Trrin nines from L, G, Plhite, Dec. 6, 19u~ Page 4 <br />c) Coal Creel: developed its wells in the upper pool of the <br />mine, (Ses Drawing TP-6 and TP-7) There mere definitely <br />tyro pools f vrater in t'r_e mine when the source of crater <br />eras de~.el~ ed as men mere in the mine in 1969 or 1970 and a. <br />dry hole v~ drilled in the slope in 1970. <br />d) iidjacent mir_ :•rorkings did r.ot r'e~lete the u7per water pool. <br />r-) The source of ring rater contributing to the u_rper pool <br />is not from the ~otentia-1 aquifer belol:~ the coal seam, It <br />appears probably that its source is the possible fault zone <br />that crosses the ;ir shaft, Coal Creek, and other drainage <br />courses up din from the mine, <br />f) `Phe development of Ttivin Pines T:o. ~ Iline dorm dip from the <br />l:~ell trill not affect the quality or quantity of the tivater <br />I in the Caldirola IJO. 2 I°Line ~+lell. <br />~~~~~ <br />Lai:~rence G, SJhite, P. E, <br />\J <br /> <br />