Promoting the Berkeley Pit and Industrial Heritage in Butte, Montana
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Superfund Sites Yield New Drugs/Tourist Attractions
Fact or Fiction? Jack W. Dini 1537 Desoto Way Livermore, CA 94550 E-mail: [email protected] Superfund Sites Yield New Drugs/Tourist Attractions In 1993, Travel and Leisure Magazine The 1.5-mile wide, 1,800-foot deep pit, fi ght migraines and cancer.4 ran an article on the Continental Divide. part of the nation’s largest Superfund site, In recent years, more than 40 small It was tough on Butte: “the ugliest spot in has been fi lling for the last 20 years with organisms have been discovered in the lake Montana - despite a spirited historic dis- a poisonous broth laced with heavy metals and these hold much potential for agricul- trict amid the rubble, the overall picture is and arsenic - a legacy of Butte’s copper ture and medicine. It’s even thought that desolate.” It called nearby Anaconda “a sad mining days. When mining offi cials aban- some of these organisms can be employed sack mining town dominated by a smelter doned the pit and stopped the pumps that to reclaim the lake and other similarly con- smokestack.”1 Today things are somewhat kept it dry, they opened the spigots to about taminated waters by neutralizing acidity different for these two sites. 3 million gallons of water per day. Today, and absorbing dissolved metals. the lake is about 850 feet deep and contains Andrea and Don Stierle and their col- Butte, Montana - Lake Berkeley more than 3 billion cubic feet of water.3 leagues have found a strain of the pitho- Edwin Dobb reports, “At one time Butte Lake Berkeley, also known as The myces fungi producing a compound that provided a third of the copper used in the Berkeley Pit, covers almost 700 acres of bonds to a receptor that causes migraines United States - all from a mining district the former open-pit copper mine. -
Health Consultation
Health Consultation Evaluation of Residential Soil Arsenic Action Level ANACONDA CO. SMELTER NPL SITE ANACONDA, DEER LODGE COUNTY, MONTANA EPA FACILITY ID: MTD093291656 OCTOBER 19, 2007 U.S. DEPARTMENT OF HEALTH AND HUMAN SERVICES Public Health Service Agency for Toxic Substances and Disease Registry Division of Health Assessment and Consultation Atlanta, Georgia 30333 Health Consultation: A Note of Explanation An ATSDR health consultation is a verbal or written response from ATSDR to a specific request for information about health risks related to a specific site, a chemical release, or the presence of hazardous material. In order to prevent or mitigate exposures, a consultation may lead to specific actions, such as restricting use of or replacing water supplies; intensifying environmental sampling; restricting site access; or removing the contaminated material. In addition, consultations may recommend additional public health actions, such as conducting health surveillance activities to evaluate exposure or trends in adverse health outcomes; conducting biological indicators of exposure studies to assess exposure; and providing health education for health care providers and community members. This concludes the health consultation process for this site, unless additional information is obtained by ATSDR which, in the Agency’s opinion, indicates a need to revise or append the conclusions previously issued. You May Contact ATSDR TOLL FREE at 1-800-CDC-INFO or Visit our Home Page at: http://www.atsdr.cdc.gov HEALTH CONSULTATION Evaluation of Residential Soil Arsenic Action Level ANACONDA CO. SMELTER NPL SITE ANACONDA, DEER LODGE COUNTY, MONTANA EPA FACILITY ID: MTD093291656 Prepared By: US Department of Health and Human Services Agency for Toxic Substance and Disease Registry Division of Health Assessment and Consultation Atlanta, Georgia 30333 Anaconda Co. -
Geochemistry and Stable Isotope Composition of the Berkeley Pit Lake and Surrounding Mine Waters, Butte, Montana
Applied Geochemistry Applied Geochemistry 20 (2005) 2116–2137 www.elsevier.com/locate/apgeochem Geochemistry and stable isotope composition of the Berkeley pit lake and surrounding mine waters, Butte, Montana Damon A. Pellicori a,1, Christopher H. Gammons a,*, Simon R. Poulson b a Department of Geological Engineering, Montana Tech of The University of Montana, Butte, MT 59701, United States b Department of Geological Sciences and Engineering, University of Nevada-Reno, Reno, NV 89557-0138, United States Received 31 January 2005; accepted 28 July 2005 Editorial handling by R. Fuge Abstract Samples of mine water from Butte, Montana were collected for paired geochemical and stable isotopic analysis. The samples included two sets of depth profiles from the acidic Berkeley pit lake, deep groundwater from several mine shafts in the adjacent flooded underground mine workings, and the acidic Horseshoe Bend Spring. Beginning in July-2000, the spring was a major surface water input into the Berkeley pit lake. Vertical trends in major ions and heavy metals in the pit lake show major changes across a chemocline at 10–20 m depth. The chemocline most likely represents the boundary between pre-2000 and post-2000 lake water, with lower salinity, modified Horseshoe Bend Spring water on top of higher salinity lake water below. Based on stable isotope results, the deep pit lake has lost approximately 12% of its initial water to evaporation, while the shallow lake is up to 25% evaporated. The stable isotopic composition of SO4 in the pit lake is sim- ilar to that of Horseshoe Bend Spring, but differs markedly from SO4 in the surrounding flooded mine shafts. -
Long Term Changes in the Limnology and Geochemistry of the Berkeley Pit Lake, Butte, Montana Christopher H
Mine Water and the Environment (2006) 25: 76–85 © IMWA Springer-Verlag 2006 Technical Article Long Term Changes in the Limnology and Geochemistry of the Berkeley Pit Lake, Butte, Montana Christopher H. Gammons1 and Terence E. Duaime2 1Dept of Geological Engineering, Montana Tech, Butte MT 59701, USA; 2Montana Bureau of Mines and Geology, Butte MT 59701; corresponding author’s e-mail: [email protected] Abstract. The Berkeley pit lake in Butte, Montana is one of the largest accumulations of acid mine drainage in the world. The pit lake began filling in 1983, and continues to fill at a rate of roughly 10 million liters d-1. This paper details how changes in mining activities have led to changes in the rate of filling of the pit lake, as well as changes in its limnology and geochemistry. As of 2005, the Berkeley pit lake is meromictic, with lower conductivity water resting on top of higher conductivity water. This permanent stratification was set up by diversion of surface water - the so-called Horseshoe Bend Spring - into the pit during the period 2000 to 2003. However, the lake may have been holomictic prior to 2000, with seasonal top-to-bottom turnover events. The present mining company is pumping water from below the chemocline to a copper precipitation plant, after which time the Cu-depleted and Fe-enriched water is returned to the pit. Continued operation of this facility may eventually change the density gradient of the lake, with a return to holomictic conditions. A conceptual model illustrating some of the various physical, chemical, and microbial processes responsible for the unusually poor water quality of the Berkeley pit lake is presented. -
Mine Name Date of Incident Last Name Year G N RR C W AABLE 11
Mine Name Date of Incident Last Name Year G N RR C W AABLE 11/11/1909 AABLE 1909 MOUNTAIN CON FRANCIS ABBOTT 9/04/1924 ABBOTT 1924 LEONARD JOHN ABEGG 3/18/1907 ABEGG 1907 MINNIE HEALEY ISAAC ABRAHAM 2/26/1904 ABRAHAM 1904 BOSTON & MT JOHN ABRAMOVICH 10/07/1916 ABRAMOVICH 1916 BLACK ROCK WILLIAM ABT 4/22/1929 ABT 1929 BA&P RR GEORGE ACCOLA 8/30/1927 ACCOLA 1927 ANACONDA FIDENCIO ACEBEDO 8/15/1928 ACEBEDO 1928 NETTIE WILLIAM ACKLER 12/07/1923 ACKLER 1923 PITTSMONT SAM ADAMOVICH 1/31/1917 ADAMOVICH 1917 MOUNTAIN CON LASLIE ADAMS 2/14/1952 ADAMS 1952 TRAMWAY CHARLES ADAMS 4/05/1919 ADAMS 1919 TRAMWAY EDWARD ADAMS 7/16/1931 ADAMS 1931 ANACONDA JOHN ADVICH 7/26/1919 ADVICH 1919 PHILADELPHIA ALVIN AFFEN 12/16/1896 AFFEN 1896 PARROT WILLIAM AHERN 12/23/1906 AHERN 1906 BADGER TOIVO AHO 4/05/1925 AHO 1925 BELL DIAMOND DOMINICK AINARDI 3/15/1919 AINARDI 1919 PENNSYLVANIA JOHN ALEXANDER 3/26/1922 ALEXANDER 1922 ANSELMO JACOV ALEXSICH 11/25/1944 ALEXSICH 1944 GRANITE MTN FRANCIS ALLEN 6/08/1917 ALLEN 1917 HIBERNIA COLMAN ALLEN 6/25/1921 ALLEN 1921 MOUNTAIN CON PETER ALLEN 11/24/1924 ALLEN 1924 SEYMOUR MONTAGUE ALLEN 9/03/1924 ALLEN 1924 UNIDENTIFIED MINE JAMES ALLEN 9/27/1891 ALLEN 1891 RARUS FRANK ALOTATO 10/06/1905 ALOTATO 1905 PENNSYLVANIA GEORGE ALQIRE 4/30/1915 ALQIRE 1915 MOUNTAIN CON WALTER ALTONEN 11/17/1956 ALTONEN 1956 LEONARD FRANK AMBROSE 8/21/1927 AMBROSE 1927 BADGER JULES AMIET 8/10/1931 AMIET 1931 ANACONDA SMELTER KNUTE AMUNDSON 2/11/1916 AMUNDSON 1916 STEWARD MICK ANDERLY 6/19/1930 ANDERLY 1930 ANACONDA SMELTER JOHN ANDERSON 6/21/1916 -
Hydrologic Investigation. Silver Bow Creek Superfund Site, Montana
Hydrologic Investigation: Silver Bow Creek Superfund Site, Montana David Stiller President and Principal Hydrogeologist Stiller and Associates, Inc. Helena. MT 59626 The upper Clark Fork River basin in western Montana has the dubious distinction of containing no fewer than three Superfund sites, all of which owe their status to the legacy of Montana's hard rock mining industry. Perhaps the best known and most significant of these sites is Silver Bow Creek. The site extends from within the City of Butte near the southwest edge of the Berkeley Pit, down Butte's Metro Storm Drain, and along the length of Silver Bow Creek to and including the Warm Springs Treatment Ponds near Warm Springs, Montana. Below the Warm Springs Treatment Ponds the Clark Fork River is formed by the confluence of four streams: Silver Bow, Warm Springs, Mill, and Willow Creeks (see map). The Silver Bow Creek site may well be the largest Superfund site in the nation. The predominant "contaminants" to which the site owes its hazardous nature are a direct result of over 100 years of mining and milling for gold, silver, and, most recently and significantly, copper. Too much of a good thing may be the case, because the precious and industrial metals which gave birth to the mining district are the same that have now created public health and related environmental problems. The following metals are of particular concern to the site: copper, zinc, lead, cadmium, and arsenic. These metals presumably originate with abandoned mill tailings presently occupying flood plain positions from within Butte to well below the Warm Springs Treatment Ponds along the Clark Fork River. -
Butte, Montana: the Berkeley Pit, Changes in Water Quality and Water Sampling Quality and Water Changes in Water
B138 Butte, Montana: The Berkeley Pit, Butte, Montana: The Berkeley Pit, Changes in Water Qualityand W The BerkeleyPit,Changes inWater Butte, Montana: Changes in Water Quality and Water Sampling Methods, 1982–2017 Terence E. Duaime and Steven F. McGrath Bulletin 138 2019 ater SamplingMethods,1982–2017DuaimeandMcGrath Cover Photos: Top, Berkeley Pit looking west towards the “Big M,” 1983. Bottom, Berkeley Pit looking southwest, “Big M” in the upper right, 2017. Photos by Ted Duaime, MBMG. Bulletin 138 Butte, Montana: The Berkeley Pit, Changes in Water Quality and Water Sampling Methods, 1982–2017 Terence E. Duaime and Steven F. McGrath Montana Bureau of Mines and Geology 2019 Montana Bureau of Mines and Geology Bulletin 138 CONTENTS Abstract .................................................................................................................................................... 1 1.0 Introduction ......................................................................................................................................... 3 1.1 Methods ........................................................................................................................................ 4 2.0 Underground Mining and Berkeley Pit Development and Operation ..................................................7 3.0 Suspension of Mining and Early Flooding of the Berkeley Pit and Underground Mines (1982–1984) ..................................................................................................................................... 13 -
Geochemistry of the Berkeley Pit Lake, Butte, Montana
GeochemistryGeochemistry ofof thethe BerkeleyBerkeley pitpit lake,lake, Butte,Butte, MontanaMontana Chris Gammons, Ph.D. Dept. of Geological Engineering Montana Tech of The University of Montana Talk overview •• SiteSite orientationorientation •• HistoryHistory ofof minemine floodingflooding •• GeochemicalGeochemical profilesprofiles inin spacespace andand timetime •• WhyWhy isis waterwater qualityquality soso bad?bad? – Geological controls – Evapoconcentration – Bad influent groundwater – Subaqueous pyrite oxidation •• ConceptualConceptual limnolimno--biobio-- hydrohydro--geogeo--chemicalchemical modelmodel Extent of Butte mine workings (as of 1980) Over 15,000 km of underground mine workings Continental Pit old leach Tailings Pond pads U D HSB Berkeley Pit Image courtesy of NASA History of mine flooding Water balance Water inputs Water outputs • Direct precipitation • Evaporation – Only ~ 12”/yr – Roughly 24”/yr • Pitwall runoff – Not quantified, believed to be minor • Groundwater seepage ~ 10 million L/day • Surface water inputs – Horseshoe Bend – Diverted storm water deep Berkeley Pit chemistry… changes with time 100000 B-Pit 30 to 60 m depth Cu recovery 10000 SO4 1000 Fe Zn Cu 100 dissolved concentration, mg/L 10 Jan-82 Jan-84 Jan-86 Jan-88 Jan-90 Jan-92 Jan-94 Jan-96 Jan-98 Jan-00 Jan-02 Jan-04 Jan-06 Shaded regions show when HSB dumped into pit Shallow Berkeley Pit chemistry… changes with time 100000 B-Pit surface Cu recovery 10000 SO4 Fe 1000 Zn Cu 100 dissolved concentration, mg/L 10 Jan-82 Jan-84 Jan-86 Jan-88 Jan-90 Jan-92 Jan-94 -
Berkeley Pit Water Treatment and Resource Recovery Strategy
PNL- 10786 UC-602 Clean Option - Berkeley Pit Water Treatment and Resource Recovery Strategy M.A. Gerber R. J. Orth M. R. Elmore B.F. Monzyk 'Battelle Memorial Institute September 1995 Prepared for the U.S. Department of Energy under Contract DE-AC06-76RLO 1830 Pacific Northwest Laboratory Richland, .Washington 993524999 DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document, Summary The U.S. Department of Energy (DOE), Office of Technology Development, established the Resource Recovery Project (RRP) in 1992 as a five-year effdto evaluate and demonstrate multiple technologies for recovering water, metals, and other industrial resources fi-om contaminated surface and groundwater. Natural water resources located throughout the DOE complex and the arid western states have been rendered unusable because of contamhation fi-om heavy metals. The Berkeley Pit, a large, inactive, open pit copper mine located in Butte, Montana, along with its associated groundwater system, has been selected by the RRP for use as a feedstock for a test bed facility located there. The test bed facility provides the infrastructure needed to evaluate promising technologies at the pilot plant scale. Data obtained from testing these technologies was used to assess their applicability for similar mine drainage water applications throughout the western states and at DOE. The objective of the Clean Option project is to develop strategies that provides a comprehensive and integrated approach to resource recovery using the Berkeley Pit water as a feedstock. The strategies not only consider the immediate problem of resource recovery from the contaminated water, but also manage the subsequent treatment of all resulting process streams. -
2019 Anaconda Edition
Volume 7, Issue 1 cfwep.org A Publication of the Clark Fork Watershed Education Program July, 2019 AnacondaAnaconda Remediation and Mount Haggin Waste Voices from the Watershed: Restoration Update Management Area Anaconda Students Page 5 Page 10 Page 12 AnacondaThis is part two in our watershed series. For the Headwaters Edition Edition see cfwep.org/montana-steward A view of Mount Haggin and Anaconda from Stucky Ridge. Photo by Kayla Lappin. Ask Dr. A: What is the Origin of the Town of Anaconda Dr. Arlene Alvarado Located in southwest Montana in Deer Lodge the “copper kings,” founded the town for his soldier of the Civil War, was inspired by Valley at the foot of the Anaconda Range employees to work at the Washoe Smelter, Horace Greeley, who said, “go west, young (locally known as the Pintler’s), Anaconda is refining the copper ore extracted from man.” And westward Hickey headed, a small town, spanning just 737 square miles. Daly’s Anaconda Mine in Butte. In the mid- bringing with him another Greeley quote Presently, she is home to about 9,100 residents, 1890’s, Daly unsuccessfully campaigned to concerning the Civil War. Greely stated that a large town by Montana standards. Anaconda have Anaconda designated as Montana’s Union armies would “encircle Lee’s forces is rich in history, culture and personality, and state capital, losing out to William A. Clark, and crush them like a giant anaconda.” The is surrounded by beautiful natural areas like another copper king, who pushed to keep image of this awesome snake stayed with Mount Haggin Wildlife Management Area Helena as the state capital. -
Liber Ignis Prospectus
liber ignis is the fifth volume in a collaborative project of appropriations, constructs, and inventions documenting the ongoing civilization of the American West by PETER RUTLEDGE KOCH Serial collage poem (composed in counterpoint to the images) by ADAM CORNFORD Engineering design, image manipulation, and binding structure by JONATHAN GERKEN EDITIONS KOCH Q BERKELEY 2015 Copper rod and linen thread binding detail. In May of 2013, Susan Filter and I visited the Städl Museum in Frankfurt, Germany and turning a corner I found myself in a small gallery in which the atmo- sphere seemed saturated with ashes and the grey shades of suffering. I felt I had entered into a set designed to stage a reading of Charles Baudelaire’s poem “La Béatrice” Dans des terrains cendreux, calcinés, sans verdure, Comme je me plaignais un jour à la nature, Et que de ma pensée, en vaguant au hasard, J’aiguisais lentement sur mon coeur le poignard, Je vis en plein midi descendre sur ma tête Un nuage funèbre et gros d’une tempête, Qui portait un troupeau de démons vicieux, Semblables à des nains cruels et curieux. “Through ashen fields, burnt to a cinder, where no green thing grew, one day I lamented…” I had chanced upon an exhibition of selected works by Joseph Bueys, Anselm Kiefer, and Sebastião Salgado, three artists deeply affected by the dark side of human nature. The massive lead sculpture Zweistromland, a shelf of mysterious and impenetrable volumes by Kiefer and Salgado’s photographs of the Serra Palada gold mine in Brazil acted upon me as catalytic forces while I stood transfixed in the gallery. -
Reclaiming Recreation
Reclaiming Recreation BRADFORD WATSON Montana State University In 1912, Walter Harvey Weed wrote “Heaps of We found the place to be endlessly rich and stimulating, waste are everywhere prominent, attesting by their a thousand times more interesting than the fakery of a great size the extent of the underground workings” Disneyland. foreshadowing the environmental impact of mining One of my early playgrounds was a stretch of mine waste on the Butte Hill. In 1983 the EPA designated the bordered by a stream that ran orange and yellow. We called it region as a Superfund Site with clean up beginning in Shit Creek. Today, it’s the site of the concentrator, where ore 1987 to protect human health and the environment. bearing small amounts of copper and molybdenum is prepared Due to the EPA’s findings of the Practical Infeasibility for smelting. Another playground, when I visited my older to remove the hazardous materials (over 660 million cousins on the Hill, was the Steward Mine. We played there metric tons of material have been displaced) a Waste while the mine operated. It helped to be lucky. It also helped to be able to run fast and scale fences quickly.1 Left in Place strategy was implemented. This process has resulted in large swaths of the town that are AN EXTRACTION COMMUNITY unoccupiable native grass fields as the cap is only The process of extraction has a profound impact on the tasked with providing protection for people and the environment, transforming and disfiguring the land through environment. This fragile surface protection has not the sorting of geological conditions that has resulted in the created places of value and in many instances has Anthropocene age.