Operation Scarlift (also known as Project 500 or The Bond Issue Program [1] ) was a program carried out by the Pennsylvania government in the 1960s and 1970s. [2] Its mission was to repair environmental damage caused by abandoned mine lands, acid mine drainage, and other issues associated with historic mining. The operation began around the time that the Land and Water Conservation and Reclamation Act was passed and became inactive in the 1970s due to a lack of funding. During the operation, a total of $141,000,000 was spent on a variety of tasks, including remedying pollution in hundreds of streams, extinguishing dozens of mine fires, and constructing acid mine drainage treatment plants. Numerous reports on mining-impacted streams were produced during the operation, many of which continue to be used for assessing watersheds.
On May 16, 1967, voters in Pennsylvania approved a $500 million bond issue for the purpose of resolving environmental problems. [1] In 1968, Pennsylvania passed the Land and Water Conservation and Reclamation Act, which was the first act in the United States concerning abandoned mine reclamation. It was this act that led to the formation of Operation Scarlift to repair damage caused by abandoned mines. [3] A chunk of the money from the $500 million bond issue was used to fund the operation. [1]
Operation Scarlift is so-named because of its mission to remove the "scars" left by historical mining activities in Pennsylvania. [4]
The purpose of Operation Scarlift was to remedy the environmental damage that historic mining in Pennsylvania has caused to the land, water, and air. [2] [3] The operation carried out abandoned mine reclamation projects. [1] These projects addressed such environmental issues as abandoned strip mines, open underground mine shafts, burning refuse banks, mine fires, identifying and gathering data on acid mine drainage sites across Pennsylvania. [1] [2] The operation built a series of lime neutralization stations to remedy acid mine drainage. [5] Additionally, it produced dozens of studies on mining-impacted areas, including watersheds and mine complexes. [2] These reports were created between 1968 and 1982. [1]
The actions taken by Operation Scarlift used a total of $141,000,000. [3] It used the money to carry out 500 stream pollution abatement projects, eliminate 150 areas of mine subsidence, extinguish 75 mine fires, and alleviate air pollution at 30 burning refuse banks. [3] Between 1968 and 1981, approximately $78,000,000 were spent on remedying stream pollution and approximately $64,000,000 was spent on the other tasks carried out by the operation. [1] By 1976, 48 miles (77 km) of streams had been made free of pollution by the operation and another 140 miles (230 km) had had their pollution levels reduced. A total of 32 deep mine complexes were sealed and 2,600 acres (11 km2) were reclaimed. [4]
Operation Scarlift was first administered by the Department of Mines and Mineral Industries. Later, that role passed to the Pennsylvania Department Environmental Resources (now known as the Pennsylvania Department of Environmental Protection). [1] Operation Scarlift became inactive in the 1970s after using up all the money provided by its revenue bond. [5]
Operation Scarlift had two main methods for remedying stream pollution by acid mine drainage. These methods were source correction and treatment. Source correction methods in deep mines included deep mine sealing and reducing the flow of surface water into deep mines. The operation also carried out various source correction procedures on strip mines and refuse banks. Where source correction was impractical, treatment was used instead. Treatment sometimes used lime or limestone and was successful at reducing acidity and iron concentrations. However, due to the high cost involved, the operation rarely attempted to treat high sulfate concentrations except when remedying pollution in sources of potable water. [4] Nevertheless, several chemical treatment plants were constructed, and were largely successful. However, several were shut down due to the high cost involved in maintaining them. In the 1980s, some of the remaining funds were used to attempt to construct passive treatment systems such as aerobic and anaerobic wetlands and ponds. However, these systems were mostly ineffective. [6]
While Operation Scarlift was underway, the Pennsylvania Department of Environmental Protection periodically created updates on the status of the operation. These updates were known as Bond Issue Report and the last one was published in 1990. It serves as a historical summary of the operation's work. [7]
Operation Scarlift has been described as achieving "limited success" with acid mine drainage abatement. [6] Despite being several decades old, the information in the reports produced by Operation Scarlift "still provides much valuable background information for groups assessing their watershed", as described by the Abandoned Mine Reclamation Clearinghouse. [2] A number of the reports on mining-impacted watersheds "remain the best descriptions and outlines of the AMD problems in the watersheds". [1] The reports were scanned and digitized in the 2000s. [2]
Acid mine drainage, acid and metalliferous drainage (AMD), or acid rock drainage (ARD) is the outflow of acidic water from metal mines or coal mines.
The Office of Surface Mining Reclamation and Enforcement (OSMRE) is a branch of the United States Department of the Interior. It is the federal agency entrusted with the implementation and enforcement of the Surface Mining Control and Reclamation Act of 1977 (SMCRA), which attached a per-ton fee to all extracted coal in order to fund an interest-accruing trust to be used for reclamation of abandoned mine lands, as well as established a set environmental standards that mines must follow while operating, and achieve when reclaiming mined land, in order to minimize environmental impact. OSMRE has about 500 employees, who work in either the national office in Washington, DC, or of the many regional and field offices.
Shamokin Creek is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately 32.4 miles (52.1 km) long and flows through Mount Carmel, Mount Carmel Township, Coal Township, Shamokin, Ralpho Township, Shamokin Township, Snydertown, Upper Augusta Township, and Sunbury. The watershed of the creek has an area of 137 square miles (350 km2). It experiences significant impacts by abandoned mine drainage and many abandoned mine drainage discharges are in its watershed. Various other impairments also affect parts of the creek's watershed. Shamokin Creek is in the Appalachian Mountains section of the Ridge and Valley physiographic province. Rock formations consisting of sandstone, shale, and anthracite deposits occur in the watershed.
Spring Creek Debris Dam is an earthfill dam on Spring Creek, a tributary of the Sacramento River, in Shasta County in the U.S. state of California. Completed in 1963, the dam, maintained by the U.S. Bureau of Reclamation, serves primarily to collect severe acid mine drainage stemming from the Iron Mountain Mine. The dam forms the Spring Creek Reservoir, less than 1 mile (1.6 km) long. Spring Creek and South Fork Spring Creek flow into the reservoir from a 16-square-mile (41 km2) watershed. The dam is directly upstream from the city of Keswick, California and the Keswick Reservoir. The operation is part of the Trinity River Division of the Central Valley Project.
Environmental impacts of mining can occur at local, regional, and global scales through direct and indirect mining practices. Impacts can result in erosion, sinkholes, loss of biodiversity, or the contamination of soil, groundwater, and surface water by the chemicals emitted from mining processes. These processes also have an impact on the atmosphere from the emissions of carbon which have effect on the quality of human health and biodiversity. Some mining methods may have such significant environmental and public health effects that mining companies in some countries are required to follow strict environmental and rehabilitation codes to ensure that the mined area returns to its original state.
Solomon Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 8.8 miles (14.2 km) long and flows through Fairview Township, Hanover Township, and Wilkes-Barre. The creek is affected by acid mine drainage and has significant loads of iron, aluminum, and manganese. The creek's named tributaries are Spring Run, Sugar Notch Run, and Pine Creek. The Solomon Creek watershed is located in the Anthracite Valley section of the ridge-and-valley geographical province. Major rock formations in the watershed include the Mauch Chunk Formation, the Spechty Kopf Formation, and the Catskill Formation.
Twomile Run is a tributary of Kettle Creek in Clinton County, Pennsylvania, in the United States. It is 4.5 miles (7.2 km) long. Tributaries of the stream include Huling Branch and Middle Branch Twomile Run. The stream flows through Leidy Township and Noyes Township. The stream's watershed has an area of approximately 9 square miles. Coal is mined in the watershed. Most of the acid mine drainage in Kettle Creek comes from Twomile Run.
The Quakake Tunnel is a mine drainage tunnel in Carbon County, Pennsylvania, in the United States. The tunnel is several thousand feet long and has a discharge of thousands of gallons per minute. It was the subject of an Operation Scarlift report. The tunnel is a major contributor of acid mine drainage to the watershed of the Lehigh River.
Cranberry Creek is a tributary of Stony Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 4.4 miles (7.1 km) long and flows through Hazle Township. The creek is affected by acid mine drainage. It also contains metals such as iron, manganese, and aluminum. It is in the drainage basin of the Jeddo Tunnel. Major roads in the creek's watershed include Pennsylvania Route 924, Pennsylvania Route 309, and Interstate 81. At least one bridge has been built over it. The creek has undergone restoration and there are plans to construct an area known as the Cranberry Creek Gateway Park in its vicinity.
Nanticoke Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 4.4 miles (7.1 km) long and flows through Hanover Township and Nanticoke. The watershed of the creek has an area of 7.57 square miles (19.6 km2). The creek has one named tributary, which is known as Espy Run. Nanticoke Creek impaired by pH and metals due to abandoned mine drainage. Abandoned mine drainage discharges in the creek's watershed include the Truesdale Mine Discharge and the Askam Borehole. The creek is located in the Northern Middle Anthracite Field and is in the Anthracite Valley Section of the ridge and valley physiographic province. The main rock formations in the watershed include the Mauch Chunk Formation, the Pottsville Group, and the Llewellyn Formation. The surficial geology consists of coal dumps, surface mining land, alluvium, Wisconsinan Outwash, Wisconsinan Till, urban land, and bedrock.
The Askam Borehole is a borehole that is located in Luzerne County, Pennsylvania, in the United States. It is situated in the watershed of Nanticoke Creek north of PA 29 and Dundee Road and contributes several million gallons of acid mine drainage to that creek daily. The borehole also discharges large loads of iron and other substances. It was constructed by the Pennsylvania Department of Environmental Protection in the early 1970s and drains mine water from the South-East Mine Pool Complex. The discharges of the borehole have been treated by active treatment systems and artificial wetlands.
Laurel Run is a tributary of the Lackawanna River in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.6 miles (5.8 km) long and flows through Jefferson Township and Archbald. The watershed of the stream has an area of 2.72 square miles (7.0 km2). The stream is somewhat affected by mine drainage. A reservoir known as the Laurel Run Reservoir is in the watershed and is dammed by the Cawley Dam. Waterfalls, ravines, ledges, and slides occur on some reaches of the stream. Additionally, the stream is a source of flooding in the borough of Archbald. Its drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.
Aylesworth Creek is a tributary of the Lackawanna River in Lackawanna County, Pennsylvania, in the United States. It is approximately 4.9 miles (7.9 km) long and flows through Carbondale Township and the boroughs of Mayfield and Archbald. The watershed of the creek has an area of 6.73 square miles (17.4 km2). Part of the creek is impaired by abandoned mine drainage and/or resource extraction. The creek tends to be slightly acidic, but its iron, manganese, and aluminum concentrations do not need reduction to meet its total maximum daily load requirements. Its watershed is in the Appalachian Mountain section of the ridge and valley physiographic province. The headwaters of the creek are in the Moosic Mountains. The rock formations in the watershed mainly consist of interbedded sedimentary rock and sandstone.
Powderly Creek is a tributary of the Lackawanna River in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.3 miles (3.7 km) long and flows through Carbondale Township and Mayfield. The watershed of the creek has an area of 1.77 square miles (4.6 km2). The creek is an impaired stream. It is impacted by flow loss and is also affected by acid mine drainage. Its waters tend to be acidic. The watershed of the creek is in the Appalachian Mountain Section of the Ridge and Valley physiographic province. The main rock formations in the watershed include interbedded sedimentary rock and sandstone. Culm and silt are deposited in the creek's vicinity and it flows through a large silt basin known as the Bushwick silt basin. A major underground coal fire is burning on a hill near the creek.
Coal Brook is a tributary of the Lackawanna River in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.2 miles (3.5 km) long and flows through Fell Township and Carbondale. The watershed of the stream has an area of 1.93 square miles (5.0 km2). The stream experiences flow loss and is impaired by flow alterations and metals. Most of its length is heavily impacted by past mining and the lower reaches are in an underground culvert. The Coal Brook Colliery was historically in the stream's watershed. Coal Brook is a first-order stream and is designated as a Coldwater Fishery and a Migratory Fishery.
Carbon Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 5.2 miles (8.4 km) long and flows through Zerbe Township, Coal Township, and Shamokin. The watershed of the stream has an area of 8.78 square miles (22.7 km2). Carbon Run is impaired due to metals from acid mine drainage, which colors the stream orange. Metals such as manganese, iron, aluminum, and others occur within its water. The watershed of the stream is in the Coal Region of Pennsylvania. Much of the area in the vicinity of the stream consists of spoil piles and abandoned mining land.
North Branch Shamokin Creek is a tributary of Shamokin Creek in Columbia County and Northumberland County, Pennsylvania, United States. It is approximately 4.8 miles (7.7 km) long and flows through Conyngham Township in Columbia County and Mount Carmel Township in Northumberland County. The watershed of the creek has an area of 5.73 square miles (14.8 km2). The entirety of the creek is designated as an impaired waterbody due to metals from abandoned mine drainage. It is acidic, but its pH has been increasing. Underground mine complexes occur within the watershed. The creek has a permeable streambed and experiences flow loss.
Abandoned mine drainage is a form of water pollution involving water that has been polluted by contact with mines, typically coal mines. Although it is sometimes called "acid mine drainage", not all abandoned mine drainage is acidic.
Rausch Creek is a tributary of Pine Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 1.7 miles (2.7 km) long and flows through Hegins Township. The watershed of the creek has an area of 9.55 square miles (24.7 km2). The creek has two named tributaries: East Branch Rausch Creek and West Branch Rausch Creek. Rausch Creek is designated as an impaired waterbody, with the cause of the impairment being metals and the probable source being abandoned mine drainage.
According to a survey completed by the Colorado Geological Survey between 1991 and 1999, the number of abandoned mines in Colorado is 18,382. The Arkansas Headwaters, Las Animas River, Rio Grande Headwaters, Alamosa, and Uncompahgre were the priority watersheds studied in this survey. In the survey, analysis was completed with Environmental Degradation Measures ranging from none to extreme. Results showed 26 abandoned mines with extreme degradation and mineral hazards, 219 with significant degradation, and 672 potentially significant hazards.