This article may be too technical for most readers to understand.(May 2015) |
The Askam Borehole is a borehole that is located in Luzerne County, Pennsylvania, in the United States. [1] 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. It is located at approximately 41.200509, -75.966600 GPS coordinates.
Water that flows from the Askam Borehole contains a significant amount of iron deposits. Upon exposure to air, the iron precipitates in the form of iron hydroxide, a reddish-orange compound that coats stream channels. [1] The borehole contributes pollution to Nanticoke Creek. [2]
In the 1970s, an Operation Scarlift report found the concentration of acidity in the discharges of the Askam Borehole to be 633 parts per million and the pH was measured to be 3.7. The concentration of iron was 384 parts per million and the sulfate concentration was 1936 parts per million. The daily load of acidity was found to be 29,100 pounds (13,200 kg) and the daily load of iron was 17,660 pounds (8,010 kg). [3]
The Askam Borehole discharges 3,500 US gallons (13 m3) of acid mine drainage per minute into Nanticoke Creek. The discharge of the borehole can reach up to 7,000 US gallons (26 m3) per minute during heavy rain. [4] In the 1970s, an Operation Scarlift report found the discharge of the borehole to be 5.51 million gallons per day. [3]
The Askam Borehole is located in Hanover Township, in the central part of Luzerne County. [1] [5] The borehole is in the watershed of Nanticoke Creek, whose watershed has been deep mined and strip mined in the past. The borehole is near Dundee Road and Pennsylvania Route 29. [1]
The Askam Borehole is one of two major outlets for mine water from the South-East Mine Pool Complex, with the other being the South Wilkes-Barre Boreholes. [6] The borehole itself has a diameter of 30 inches (76 cm). [7]
The Askam Borehole is the main point by which the T-B[ clarification needed ] mine workings discharge acid mine drainage into Nanticoke Creek. The borehole is the only source of water for the lower reaches of Nanticoke Creek. [7] It discharges in two different locations. [8]
The Askam Borehole is named after Askam, a nearby village. [1] It was drilled in the early 1970s by the Pennsylvania Department of Environmental Resources (later known as the Pennsylvania Department of Environmental Protection). [1] [7] The borehole was created for the purpose of alleviating water pressure from an underground mine pool that was causing groundwater to flood local basements. [1] In 1975, an Operation Scarlift report estimated that the cost of treating the borehole's discharge would be $1,011,600 per year in 1975 dollars. [3]
An active treatment system for the Askam Borehole was proposed by the Earth Conservancy by 2013. [4] As of 2014, the Earth Conservancy has been constructing, testing, and monitoring an abandoned mine drainage treatment system at the Askam Borehole. [2] The treatment system makes use of a technology known as the Maelstrom Oxidizer, which uses electricity to blow air across the surface of the water, causing iron to precipitate from the water before the water is moved to a holding pond and then into the stream. [2] [4] The treatment system is known as the Askam AMD Treatment System or the Askam Treatment System. [2] An artificial wetland has also been used to treat the borehole's discharges. [9] This wetland was constructed in May 1999 and has an area of 2.2 acres (0.89 ha). [5]
In the 2010s, the Earth Conservancy was awarded a $250,000 grant by the Pennsylvania Department of Environmental Protection to clean up the Askam Borehole discharges. [10] There are plans for the Eastern Pennsylvania Coalition for Abandoned Mine Restoration to continue to take biological stream samples and water quality measurements in the vicinity of the Askam Borehole. [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.
Black Creek is a long source tributary of Nescopeck Creek so part of the Susquehanna River drainage basin. It is also the second & longer stream of the same name recognized by the USGS GNIS system in Luzerne County, Pennsylvania, in the United States—compared to the Black Creek beyond the ridgeline of the drainage divide, so in the Lehigh River valley and Carbon County. The headwaters of both Black Creeks in Luzerne county are only a few miles apart, and both valleys were traversed by the Lausanne-Nescopeck Turnpike in the first half of the 19th-century.
Mahanoy Creek is a 51.6-mile-long (83.0 km) tributary of the Susquehanna River in Northumberland and Schuylkill counties, Pennsylvania. There are at least 35 sources of acid mine drainage in the creek's watershed. Anthracite was mined in the upper part of the Mahanoy Creek watershed in the 19th and 20th centuries. Mahanoy Creek's tributaries include Schwaben Creek, Zerbe Run, Little Mahanoy Creek, Shenandoah Creek, and North Mahanoy Creek. Little Mahanoy Creek and Schwaben Creek are two streams in the watershed that are unaffected by acid mine drainage. Schwaben Creek has a higher number and diversity of fish species than the main stem.
Dunkard Creek is a stream that flows 36.9 miles (59.4 km) through Greene County, Pennsylvania and Monongalia County, West Virginia, near the towns of Mount Morris, Pennsylvania, and Blacksville, West Virginia. It flows into the Monongahela River northwest of Point Marion, Pennsylvania, approximately three miles north of the Pennsylvania-West Virginia border.
The Audenried Tunnel is a drainage tunnel located in East Union Township, Schuylkill County, Pennsylvania, in the United States. It is approximately three miles long and drains the western portion of a coal basin near Kelayres. It is among the largest sources of acid mine drainage into Catawissa Creek. It also contributes up to 80% of the acidity to Catawissa Creek. The Audenried Tunnel's pH is approximately 4. However, there have been somewhat successful attempts at treating the tunnel outflow in the 21st century. The bedrock in the vicinity of the tunnel is mostly shale and sandstone.
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.
Newport Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is 4.9 miles (7.9 km) in length. Named tributaries of the creek include South Branch Newport Creek. The entire watershed of Newport Creek is considered by the Pennsylvania Department of Environmental Protection to be impaired.
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 Oneida Number Three Tunnel is a mine tunnel in Schuylkill County, Pennsylvania, in the United States. It is one of five major mine tunnels in the watershed of Catawissa Creek. The tunnel discharges into Tomhicken Creek downstream of the mouth of Little Tomhicken Creek. The tunnel was constructed in the 1930s and a passive treatment system was installed at the site of the tunnel in 2009. The tunnel is more than a mile long.
The Green Mountain Tunnel is a mine drainage tunnel in Schuylkill County, Pennsylvania, in the United States. It is one of five major mine drainage tunnels in the watershed of Catawissa Creek. The tunnel discharges into Catawissa Creek near the Audenried Tunnel and the Catawissa Tunnel. The tunnel was constructed in the 1930s and is slightly less than one mile long.
The Catawissa Tunnel is a mine drainage tunnel in Schuylkill County, Pennsylvania, in the United States. The tunnel discharges into Catawissa Creek further upstream than any other mine drainage tunnel in the watershed. The tunnel was constructed in the 1930s and a passive treatment system may or may not be installed at the site of the tunnel. The tunnel is several hundred feet long.
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.
Stony Creek is a tributary of Black Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 3.7 miles (6.0 km) long and flows through Hazle Township and West Hazleton. Its named tributaries include Cranberry Creek and Wolffs Run. Stony Creek is considered to be impaired by acid mine drainage and also has measurable concentrations of iron, aluminum, and manganese. The Llwellyn Formation and the Mauch Chunk Formation can be found near the creek. Land uses in its watershed include forested land and barren land. A reservoir has been constructed in the watershed and at least one bridge has been built over the creek. The creek is considered to be a coldwater fishery and a migratory fishery.
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.
Espy Run is a tributary of Nanticoke Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 2.4 miles (3.9 km) long and flows through Nanticoke and Hanover Township. The watershed of the stream has an area of 3.14 square miles (8.1 km2). The stream is affected by abandoned mine drainage and has been affected by sewage in the past. The Espy Run Wetlands and the Espy Run discharge are in the stream's vicinity. The surficial geology in the area consists of urban land, coal dumps, surface mining land, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, and bedrock.
Warrior Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 3.0 miles (4.8 km) long and flows through Warrior Run, Sugar Notch, and Hanover Township. The watershed of the creek has an area of 4.51 square miles (11.7 km2). It is designated as a Coldwater Fishery. However, it is considered to be impaired by abandoned mine drainage. The surficial geology in the creek's vicinity consists of alluvium, fill, urban land, strip mining land, Wisconsinan Till, and bedrock.
Operation Scarlift was a program carried out by the Pennsylvania government in the 1960s and 1970s. 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.
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.
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.