The Berkeley Pit is a former open pitcoppermine located in Butte, Montana, United States. It is long by wide with an approximate depth of. It is filled to a depth of about with water that is heavily acidic, about the acidity of Coca-Cola, lemon juice, or gastric acid. As a result, the pit is laden with heavy metals and dangerous chemicals that leach from the rock, including copper, arsenic, cadmium, zinc, and sulfuric acid. The mine was opened in 1955 and operated by the Anaconda Copper Mining Company, and later by the Atlantic Richfield Company, until its closure on Earth Day in 1982. When the pit was closed, the water pumps in the nearby Kelley Mine, below the surface, were turned off, and groundwater from the surrounding aquifers began to slowly fill the Berkeley Pit, rising at about the rate of a month. Since its closure, the water level in the pit has risen to within of the natural water table. The Berkeley Pit is currently one of the largest Superfund sites. The water, with dissolved oxygen, allows pyrite and sulfide minerals in the ore and wall rocks to decay, releasing acid. If the pit water level reaches the natural water table, the pit water will reverse flow back into surrounding groundwater, polluting Silver Bow Creek, which is the headwaters of Clark Fork of the Columbia River. The acidic water in the pit carries a heavy load of dissolved heavy metals. One of its owners, Montana Resources, has mined copper directly from the water. The first plans for solving the groundwater problem were devised in the 1990s. Water flowing into the pit has been diverted by the Horseshoe BendWater Treatment Plant to slow the rise of the water level. Construction started on a water treatment facility in September 2018, with the goal to have the facility fully operational five years before the pit's water level rises high enough to contaminate the groundwater of Butte. The Berkeley Pit is a tourist attraction, with an adjacent gift shop. An admission fee is charged to go out on the viewing platform.
History
The underground Berkeley Mine was located on a prominent vein extending to the southeast from the main Anaconda vein system. When open pit mining operations began in July 1955, near the Berkeley Mine shaft, the older mine gave its name to the pit. The open-pit style of mining superseded underground operations because it was far more economical and much less dangerous than underground mining. Within the first year of operation, the pit extracted 17,000 tons of ore per day at a grade of 0.75% copper. Ultimately, about 1,000,000,000 tons of material were mined from the Berkeley Pit. Copper was the principal metal produced, although other metals were also extracted, including silver and gold. Two communities and much of Butte's previously crowded east side were consumed by land purchases to expand the pit during the 1970s. The Anaconda Company bought the homes, businesses and schools of the working-class communities of Meaderville, East Butte, and McQueen, east of the pit site. Many of these homes were either destroyed, buried, or moved to the southern end of Butte. Residents were compensated at market value for their acquired property. The Berkeley Pit is a part of the Silver Bow Creek/Butte Area Environmental Protection Agency Superfund site, considered one of the largest in America, and the pit itself was added to the federal Superfund site list in 1987. It is one of sixteen Superfund sites in Montana, and the Berkeley Pit is the final unrestored section of the Silver Bow Creek/Butte Area site. In 1995, a flock of migrating geese landed in the Berkeley Pit and died. A total of 342 carcasses were recovered. ARCO, the custodian of the pit, denied that the toxic water caused the death of the geese, attributing the deaths to an acute aspergillosis infection that may have been caused by a grain fungus, as substantiated by Colorado State Universitynecropsy findings. These findings were disputed by the State of Montana on the basis of its own lab tests. Necropsies showed their insides were lined with burns and festering sores from exposure to high concentrations of copper, cadmium, and arsenic. On November 28, 2016, several thousand snow geese died after a large flock landed in the pit's water to avoid a snow storm. Immediately after the event, officials made efforts to scare birds away and prevent more from landing in the area. An official report issued in 2017 by the U.S. Fish and Wildlife Service found that the 3,000 to 4,000 snow geese that died at the Berkeley Pit were killed by exposure to sulfuric acid and heavy metals. The Berkeley Pit started utilizing Phoenix Wailers, which have been effective in deterring birds from landing at or staying in Berkeley Pit for an extended period of time. Studies have shown that the Wailers have been effective in limiting bird deaths in most cases, but they have not worked as well when faced with a large number of birds. Construction began on a treatment plant at the Berkeley Pit in September 2018. The facility will be able to treat the existing waters of the Pit before the water level hits the critical point of above sea level. This number was set by federal order from the EPA and is intended to protect groundwater from being contaminated by the water in the pit. The treatment facility will be able to treat ten million gallons of water per day. The companies working jointly to build the plant, Montana Resources and Atlantic Richfield, aim to have the facility open by mid-2019. In August 2019, construction of the $19 million facility was complete, and testing was slated to begin, with the prospect of making its first discharge of treated water in September 2019.
Important dates
1994 – September, EPA/DEQ issue Record of Decision for Butte Mine Flooding Operable Unit.
1996 – April, Montana Resources and ARCO divert Horseshoe Bend drainage water away from Berkeley Pit to slow filling rate, per ROD.
2000 – July, MR suspends mining operations due to high energy costs; HSB water allowed to flow back into pit, increasing pit filling rate.
2002 – March, USEPA and Montana Department of Environmental Quality enter into a Consent Decree with BP/ARCO and the Montana Resources Group for settlement of past and future costs for this site.
2002 – Fall, USEPA and MDEQ issue order for Settling Defendants to begin design of water treatment plant for HSB water. Settling Defendants issue contract and begin construction of treatment plant.
2003 – November, MR resumes mining operations.
2003 – November 17, HSB water treatment plant comes on line slowing pit filling rate.
The Butte mining district is characterized by the Late Cretaceous Boulder batholith which metamorphosed surrounding rocks during the Laramide orogeny. Ore formation occurred with the intrusion of the Butte quartzmonzonitepluton. Mining of sulfide minerals began in the district in 1864. Placer deposits were mined out by 1867. Silver vein lodes were then the most productive until copper was discovered in 1888. Open-pit mining started in 1955. Copper has historically been the main metal produced, though lead, zinc, manganese, silver and gold have been produced at various times.
Organisms in the water
A protozoan species, Euglena mutabilis, was found to reside in the pit by Andrea A. Stierle and Donald B. Stierle, and the protozoans have been found to have adapted to the harsh conditions of the water. Intense competition for the limited resources caused these species to evolve the production of highly toxic compounds to improve survivability; natural products such as Berkeleydione, berkeleytrione, and Berkelic acid have been isolated from these organisms which show selective activity against cancer cell lines. Some of these species ingest metals and are being investigated as an alternative means of cleaning the water.
