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r; <br /> f' Transit Mix Concrete Co. <br /> o _oa ,za "'°° Gaining No Changeach <br /> FEET Losing Reach <br /> 0.45 Us Little Turkey Creek <br /> Flow Measurement <br /> and Location <br /> \ J <br /> -rows as <br /> i F \ / <br /> 0 <br /> 6,950 <br /> 7.os <br /> o � <br /> 0.41 CFs - <br /> 2200 7,o7z o To ail <br /> �0? <br /> took / o <br /> TS1 ' <br /> 7,024 �..� h <br /> ine 0.39CF5 <br /> nt Ji ��llJ( <br /> tockpi z0p 7,157® i y' 0 20 Crs <br /> 1 <br /> Q rry � � � ,b <br /> �®6,722 <br /> 6,759 <br /> _'zsp Are �i[�. _ % / 6,771 <br /> J, i r� o <br /> > 3 <br /> /l�/��(/` <br /> Figure G-7 <br /> Gaining and Losing reaches along Little Turkey Creek (October 24, 2016) <br /> Little Turkey Creek surface water flow rate steadily declines as the creek flows east across the <br /> fault zone between the West and East Faults and eventually over the sedimentary Fountain <br /> Formation to the east of the East Fault. These declining surface water flows indicate that the <br /> creek is losing water to, and recharging, the underlying groundwater system. This is consistent <br /> with potentiometric data from monitoring sites GW 2, GW-6 and GW-7 which show water levels <br /> significantly below the creek water level and a downward vertical hydraulic gradient component. <br /> The lateral hydraulic gradient within the fractured rocks underlying the reach of the Little Turkey <br /> Creek valley between the West and East Faults is about 0.1. The significant steepening of the <br /> hydraulic gradient within this reach suggests that the ability for the fractured rock to transmit <br /> groundwater flow within this reach is considerably lower than that in the valley bottom to the west <br /> of the West Fault. <br /> Hitch Rack Ranch Quarry Permit Application <br /> October 3, 2017 G-34 <br />