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<br /> <br />6~J~t~ <br /> <br />/~~{{~- <br />;\r:.~r>.';/ <br /> <br /><<tAl' ( <br />,~ ,(l/,<./t.': <br />. )..,- <br />~" <br /> <br />;,'..<-' <br /> <br />.'-"'" <br /> <br />::_~{?,,:~ <br />;J;-::~{ <br /> <br />IN REPLY REFER TO: <br /> <br /> <br />,*, <br />~~ <br />~-.- <br /> <br />INFOR}~TION FOR THE PRESS <br /> <br />SUBJECT: Quantity and Quality of Drainage from the Argo Tunnel and <br />Other Sources Related to }letal Mining in Gilpin, Clear Creek, <br />and Park Counties, Colorado <br /> <br />RELEASE DATE: Immediately <br /> <br />FOR }~DITIONAL INFOfu~TION CONTACT: <br /> <br />i.,,,D 2;",'fE!f$l'f???rJ~' --, <br />; f!(-LL~J-1:1 r c;v!fJ1 <br />'i [fe T' , ,n <br />!'t::-~~_ Z 5 1917;JJ!J1lI <br /> <br />COIO~ IU <br />~E - , WA1}~R <br />RVAliON <br />BOARD <br /> <br />According to a recent U.S. Geological Survey, Department of the Interior report, <br />18 metal-mine drainage sources have been located >vithin the Hissouri River <br />basin in Gilpin, Clear Creek, and Park Counties, Colorado. At least 13 of <br />these sources contain high ac'idity and (or) trace-element concentrations or <br />contribute >vater to adversely aff~cted streams. One of the major drainage <br />sources--the Argo Tunnel in Idaho Springs--exhibited relatively constant '" ter <br />quality during the period March 1976 to March 1977. Average total trace.- <br />element concentrations, in micrograms per liter, were as follows: arsenic, <br />140; cadmium, 150; copper, 5,800; iron, 180,000; lead, 100; manganese, 94,000; <br />and zinc) 4L~, 000. Except for lead, the trace elements ,,,ere mostly dissolved <br />(82 percent or greater) and appear to represent baseline concentrations. <br />Spring chemical flushes containing higher than baseline trace-element concen- <br />trations occurred in the Argo Tunnel in 1973 and 1974, but not in 1975 or <br />1976, and probably not in 1972. The spring chemical flushes appear to be <br />associated with increased infiltration from snov:melt in the catchment of the <br />tunnel. Long--term degradation of >vater flowing from the Argo Tunnel is shOml <br />by incr~ases of at least 2,5 to 8.0 times for dissolved solids, dissolved <br />iron, calcium, magnesium, and sulfate since 1906. Acidity of the >vater has <br />chang~d from neutral to a median pH of 2.9 in 1976-77. Management alternatives <br />for mine'-drainage abatement are present~d and discussed in the report in <br />regard to general applicability in the study area. <br /> <br />J. E. Biesecker, District Chief <br />U.S. Geological Survey, h~ <br />Colorado District; Mail Stop 415 <br />Box 25046, Denver Federal Center <br />Lake>vood, Colorado 80225 <br />Telephone: 234-5092 <br />234-3815 <br />234-3458 <br /> <br />,jO\..llT10-v <br /> <br /><l'~~ <br />~ ~ <br />(3 '" <br />_ m <br />(!. <: <br />~ ~ <br />'.v~ ~ <br />1'>'>6-;91'" @ <br /> <br />(yt~. <br />",:'.~~:- :';' <br />.':'",;.'.: <br />:~':tt?~- <br />.",'. <br />-;"...." <br />......".:. <br />".,.:--,:,.-~, <br /> <br /><.;:.5<: <br />'.:-;:. "~'.- <br /> <br />:;'C <br /> <br />.;-.- <br /> <br />.,',..', <br />...., ,'- ~:.: <br />