Overview | |
---|---|
Start | mines in East Union Township, Pennsylvania |
End | Tomhicken Creek in North Union Township, Schuylkill County, Pennsylvania |
Operation | |
Opened | 1930s |
Technical | |
Length | 7,000 feet (2,100 m) |
The Oneida Number Three Tunnel (also known as the Oneida #3 Tunnel [1] ) is a mine tunnel in Schuylkill County, Pennsylvania, in the United States. [2] It is one of five major mine tunnels in the watershed of Catawissa Creek. [1] 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 average discharge of the Oneida Number Three Tunnel is 3,820,000 gallons per day (approximately 2,653 gallons per minute). [1] The tunnel is the largest discharge of acid mine drainage to Tomhicken Creek. [3]
The pH of the water being discharged from the Oneida Number Three Tunnel ranges from 3.9 to 4.7. The average pH of the waters is 4.53. The concentration of acidity in the tunnel's waters is 17.35 milligrams per liter and the daily load of acidity is 552.8 pounds (250.7 kg). The acidity load requires an 89 percent reduction to meet its total maximum daily load requirements. The alkalinity concentration of its waters is 7.40 milligrams per liter and the load of alkalinity is 235.8 pounds (107.0 kg) per day. [1] The net concentration of acidity is 15.8 milligrams per liter. [4]
The concentration of iron in the discharge of the Oneida Number Three Tunnel is 0.18 milligrams per liter and the daily load is 5.7 pounds (2.6 kg). The iron load does not require any reduction to meet its total maximum daily load requirements. The manganese concentration is 0.59 milligrams per liter and the load of manganese is 18.8 pounds (8.5 kg) per day. The manganese load requires a 79 percent reduction to meet its total maximum daily load requirements. The aluminum concentration is 1.59 milligrams per liter and the daily load of it is 50.7 pounds (23.0 kg). The aluminum load requires a 71 percent reduction to meet its total maximum daily load requirements. [1]
The Oneida Number Three Tunnel discharges into Tomhicken Creek downstream of Little Tomhicken Creek. The tunnel is approximately 7,000 feet (2,100 m) long. [1] The upper end of the tunnel is in mines in the South Green Mountain Coal Basin, which it drains part of. [1] [3] The tunnel runs roughly northwards until it reaches Tomhicken Creek. [1] The tunnel is in East Union Township and North Union Township. [2]
The Oneida Number Three Tunnel is in the Eastern Middle Anthracite Field. [5] The tunnel is between Tomhicken Creek and a steep hill. [4]
The total maximum daily load document for Catawissa Creek suggests reclaiming mined land in the Green Mountain Coal Basin to reduce the discharge of the Oneida Number Three Tunnel. [1]
The Oneida Number Three Tunnel has a passive treatment system. The system was constructed in a similar manner to the way in which the Audenried Tunnel was constructed. However, it only has one limestone tank, as opposed to the Audenried Tunnel's three. There are plans to construct a second limestone tank for the passive treatment system. [6]
The Oneida Number Three tunnel was constructed during the 1930s. It was one of five mine drainage tunnels in the Catawissa Creek watershed to be constructed during this time (the others being the Audenried Tunnel, the Catawissa Tunnel, the Green Mountain Tunnel, and the Oneida Number One Tunnel). [1]
The Catawissa Creek Restoration Association started working on constructing a passive treatment system for the Oneida Number Three Tunnel as early as 2003. The organization's work was funded by the United States Environmental Protection Agency. [1] The construction of the passive treatment system was completed in December 2009. [5] The system was the third such system in the Catawissa Creek to be constructed. [6]
The Oneida Number Three Tunnel was damaged to the point of being useless during heavy rain in March 2011. It was repaired later in 2011. The tunnel's water quality was studied in the same year. [5] It was also studied shortly after the passive treatment system was constructed. [7]
As of 2003, the Oneida Number Three Tunnel is not listed on the Pennsylvania Section 303(d) of streams that are impaired due to pH. [1]
Catawissa Creek is a 41.8-mile-long (67.3 km) tributary of the Susquehanna River in east-central Pennsylvania in the United States. Its watershed has an area of 153 square miles (400 km2).
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.
The Jeddo Tunnel is a drainage tunnel at water level in Pennsylvania. It is one of the Coal Region's biggest discharges of mine water. The tunnel is five miles long and was constructed between 1891 and 1894, and at the time of its construction, was reputed to be the largest mine drainage tunnel in the world. It consists of major tunnels A and B, and minor tunnels C, D and X.
The Audenried Tunnel, also known as the Audenried Mine 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.
Tomhicken Creek, also known as Tomhickon Creek, is a stream in Luzerne County and Schuylkill County, in Pennsylvania, in the United States. It is approximately 11 miles (18 km) long and is the largest tributary of Catawissa Creek. Named tributaries of the creek include Little Crooked Run, Little Tomhicken Creek, Raccoon Creek, and Sugarloaf Creek. The watershed of the main stem has an area of 20.6 square miles. A number of mine tunnels discharge into the creek and its tributaries.
Sugarloaf Creek is a tributary of Tomhicken Creek in Luzerne County and Schuylkill County, in Pennsylvania, in the United States. It is approximately 3.5 miles (5.6 km) long and flows through Hazle Township and Black Creek Township in Luzerne County and North Union Township in Schuylkill County.
Lake Choctaw is a manmade lake and reservoir in Luzerne County and Schuylkill County in Pennsylvania, in the United States. It has a surface area of 22.1 acres. The lake is situated on Sugarloaf Creek. In the past, the lake had poor water quality and a low pH. However, after the installation of a treatment system on the nearby Oneida Number One Tunnel, the water quality rapidly improved and fish were introduced into it.
Little Tomhicken Creek is a tributary of Tomhicken Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 1.0 mile (1.6 km) long and flows through East Union Township and North Union Township. The watershed of the stream has an area of 4.31 square miles (11.2 km2). The creek is considered to be a Coldwater Fishery. However, it is devoid of fish life and is impaired by acid mine drainage. It also has low water quality. The main rock formations in the creek's watershed are the Mauch Chunk Formation and the Pottsville Formation and the main soil is the Hazleton soil. Nearly all of the creek's length is fairly close to a road.
The Oneida Number One Tunnel is a mine drainage 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 Sugarloaf Creek near Lake Choctaw and Lake Susquehanna. The water quality of the tunnel's discharge has improved significantly since the installation of a treatment system at the site of the tunnel in 2001.
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 Catawissa Tunnel is a mine drainage tunnel in Schuylkill County, Pennsylvania, in the United States. Its properties include the discharge, the pH, the chemical hydrology, and the water temperature. A total of 30 different metals and metalloids have been observed in the tunnel's waters. The hydrological data comes from a gauge on the tunnel at a location of 40°54'39" north and 76°03'59" west and an elevation of 1,440 feet (440 m) above sea level. Some of the most abundant metals in the waters of the tunnel include iron, aluminum, and manganese. These metals have concentrations on the order of several milligrams per liter. A number of other metals have concentrations on the order of micrograms per liter and some metals are found in even lower concentrations. Nonmetals such as nitrates, sulfates, fluorides, chlorides, and silica are also present in the tunnel. The concentrations of such nonmetals range between several micrograms per liter and several milligrams per liter.
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.
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.
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.
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.
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.