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Water Quality Variations and Trends in Monument and Fountain Creeks
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Water Quality Variations and Trends in Monument and Fountain Creeks
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Last modified
7/20/2010 3:30:27 PM
Creation date
6/29/2010 10:11:55 AM
Metadata
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Template:
Water Supply Protection
Description
ARCA
State
CO
KS
Basin
Arkansas
Water Division
2
Date
1/1/1993
Author
Barbara C. Ruddy, U.S. Geologic Survey, Colorado Springs Department of Utilities
Title
Water Quality Variations and Trends in Monument and Fountain Creeks
Water Supply Pro - Doc Type
Report/Study
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o J 4 g 100 <br />OC <br />W <br />H <br />J 80 <br />w <br />CL <br />Q <br />CC <br />C7 <br />J 60 <br />J_ <br />Z <br />W <br />a <br />OC 40 <br />O <br />J <br />2 <br />U <br />0 <br />W <br />J <br />20 <br />V) <br />W <br />0 <br />104' <br />O 1983 -88 <br />69 <br />O <br />,977 -88 <br />MONUMENT CREEK FOUNTAIN CREEK 110 <br />1981 -85 <br />37 <br />1977 -88 13 103 <br />1977 -88 O <br />1984 -88 â <br />61 B <br />° B <br />1977 -88 <br />83 <br />â <br />1977 -85 <br />32 <br />9 <br />z <br />w <br />U <br />U- <br />LL <br />z <br />07103747 07103780 07104000 07104905 07103700 07105500 071obb30 u n uba0b uiIMOW <br />U.S. GEOLOGICAL SURVEY STATION NUMBER <br />Figure 11. -- Variations in concentrations of dissolved chloride. <br />600 <br />MONUMENT CREEK FOUNTAIN CREEK <br />1977 -85 <br />32 <br />OC <br />w <br />Fâ <br />J <br />w <br />CL <br />N <br />Q 400 <br />C7 <br />J <br />J_ <br />Z <br />W <br />H <br />Q <br />LL <br />J <br />cn 200 <br />0 <br />W <br />J <br />O <br />' A l <br />1977 -88 <br />98 <br />1983 -88 <br />69 <br />1977 -88 <br />99 <br />1982 -85 <br />25 <br />1977 -88 <br />98 <br />O <br />z <br />z <br />w <br />U <br />LL <br />LL <br />Z) <br />U) <br />z <br />0 <br />1984 -88 <br />56 <br />O <br />1977 -88 <br />78 rl <br />°t° <br />07103747 07103780 07104000 07104905 07103700 07105500 07105530 07105905 0710650 <br />U.S. GEOLOGICAL SURVEY STATION NUMBER <br />Figure 12. -- Variations in concentrations of dissolved sulfate. <br />35 <br />
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