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<br />014&,000 <br /> <br />MONUMENT CREEK <br /> <br />FOUNTAIN CREEK <br /> <br />1916-88 <br />306 <br /> <br />1976-88 <br />142 <br /> <br />U <br />m 0 <br />::l <br />U <br />~ <br />~ <br />00 <br />-'z <br />~8 <br /><l:w <br />w", <br />a: a: <br />r-w <br />"'0.. <br />"'.... <br />5~ 10 <br />wu.. <br />z <br /><l: <br />.... <br />z <br /><l: <br />r- <br />'" <br />~ <br /> <br /> 1916-88 <br />1,000 249 <br /> 1984..88 <br /> 1917-88 93 G <br /> 209 8 9 <br /> ~ 0 <br />100 <br /> <br />1960-88 8 <br />100 <br />0 ~ <br /> 1976-88 <br /> 267 <br />9 0 <br />~ e <br />$ <br /> <br />1976.88 <br />116 <br /> <br />o <br /> <br />1976-88 <br />266 <br /> <br /> <br /> 0,1 <br /> 07103747 07103780 07104000 07104905 07103700 07105500 01105530 07105905 07106500 <br /> U.S, GEOLOGICAL SURVEY STATION NUMBER <br /> Figure 3.--Variations in instantaneous streamflow. <br />a: 6.000 MONUMENT CREEK FOUNTAIN CREEK <br />w 1916-88 0 <br />.... 265 <br />w 0 <br />:e <br />;:: <br />z 5,000 <br />w <br />U <br />a: <br />w <br />c.. <br />'" <br />Z'" 0 <br />w::l 4,000 <br />:eiii <br />UJ-' ~ <br />-UJ <br />"'U <br />0", <br />a:UJ lJ <br />!dUJ 3,000 ~ <br />:ea: <br />z~ 1976-88 <br />-:0 141 <br />UJ", <br />UN <br />Z.... B <br /><t<t 2,000 <br />r- 1976-88 lJ <br />U 1976-88 <br />::l 283 116 <br />0 1976-88 <br />Z 1980-88 259 Q <br />0 1976-88 100 <br />U 1,000 1984-88 243 $ <br />U 87 T <br />u: 1977.88 8 $ + <br />u 206 0 <br />UJ ~ <br />c.. ~ <br />rJl ~ <br /> 0 <br /> 07103741 07103780 07104000 07104905 07103100 07105500 07105530 07105905 07106500 <br /> U.S, GEOLOGICAL SURVEY STATION NUMBER <br /> Figure 4.--Variations in specific conductance. <br /> 31 <br /> <br />