Location | |
---|---|
State | Wyoming |
Country | USA |
Coordinates | 44°22′59″N105°27′19″W / 44.38306°N 105.45528°W Coordinates: 44°22′59″N105°27′19″W / 44.38306°N 105.45528°W |
Production | |
Products | Coal |
History | |
Opened | 1990 |
Owner | |
Company | Western Fuels Association |
Website | www |
Year of acquisition | 1990 |
The Dry Fork mine is a coal mine located 8 miles north of Gillette, Wyoming in the United States in the coal-rich Powder River Basin. The mine is an open pit mine that utilizes truck and shovel mining method to mine a low-sulfur, sub-bituminous coal that is used for domestic energy generation and shipped to customers via railroad. In 2011, the mine is expected to begin supplying coal to the newly constructed Dry Fork power station that has been constructed adjacent to the mine. The mine is currently owned and operated by Western Fuels Association. [1]
As of 2009, Dry Fork had reserves of 330 mm tons of sub-bituminous coal and a maximum permitted production capacity of 15mm tons per year. Typical annual production has been in 5.2mm ton range for the last several years though. In 2008, the mine produced just over 5.2 million short tons of coal, making it the 37th-largest producer of coal in the United States. [2]
The average quality of the coal shipped from Dry Fork is 8,050-8,200 BTU/lb, 0.20-0.42% Sulfur, 3.8-5.1% Ash, and 1.50% Sodium (of the ash). Train loading operations at the mine are done with a batch weigh bin system that is coupled to a "weigh-in-motion" track scale system. Silo capacity at the mine's rail loop, which can accommodate a single unit train, is 10,800 tons. [3] [4]
The Dry Fork mine shipped its first coal to members of the Western Fuels Association in 1990 and is run by Western Fuels-Wyoming an associate of Western Fuels. Since opening, Dry Fork has shipped 69.5mm tons of coal.
Year | Coal production | Employees |
---|---|---|
2018 | 6,304,022 | 83 |
2017 | 6,045,618 | 82 |
2016 | 6,141,433 | 82 |
2015 | 6,369,206 | 79 |
2014 | 5,373,973 | 79 |
2013 | 5,433,936 | 78 |
2012 | 6,006,787 | 77 |
2011 | 5,776,092 | 79 |
2010 | 5,448,073 | 71 |
2009 | 5,232,451 | 67 |
2008 | 5,261,242 | 71 |
2007 | 5,310,716 | 70 |
2006 | 5,860,998 | 69 |
2005 | 4,093,611 | 61 |
2004 | 4,533,621 | 61 |
2003 | 4,363,683 | 61 |
2002 | 4,891,403 | 65 |
2001 | 4,029,100 | 68 |
2000 | 2,268,720 | 34 |
1999 | 1,219,590 | 9 |
1998 | 1,030,718 | 9 |
1997 | 918,224 | 8 |
1996 | 2,945,662 | 39 |
1995 | 3,606,453 | 47 |
1994 | 3,836,228 | 51 |
1993 | 3,279,801 | 49 |
1992 | 3,453,340 | 49 |
1991 | 2,786,946 | 43 |
1990 | 736,641 | 32 |
1989 | 0 | 3 |
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands—called coal forests—that covered much of the Earth's tropical land areas during the late Carboniferous (Pennsylvanian) and Permian times. However, many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras.
Bituminous coal, or black coal, is a type of coal containing a tar-like substance called bitumen or asphalt. Its coloration can be black or sometimes dark brown; often there are well-defined bands of bright and dull material within the seams. It is typically hard but friable. Its quality is ranked higher than lignite and sub-bituminous coal, but lesser than anthracite. It is the most abundant rank of coal, with deposits found around the world, often in rocks of Carboniferous age. Bituminous coal is formed from sub-bituminous coal that is buried deeply enough to be heated to 85 °C (185 °F) or higher.
Anthracite, also known as hard coal, and black coal, is a hard, compact variety of coal that has a submetallic luster. It has the highest carbon content, the fewest impurities, and the highest energy density of all types of coal and is the highest ranking of coals.
The Powder River Basin is a geologic structural basin in southeast Montana and northeast Wyoming, about 120 miles (190 km) east to west and 200 miles (320 km) north to south, known for its extensive coal reserves. The former hunting grounds of the Oglala Lakota, the area is very sparsely populated and is known for its rolling grasslands and semiarid climate.
Sub-bituminous coal is a lower grade of coal that contains 35–45% carbon. The properties of this type are between those of lignite, the lowest grade of coal, and those of bituminous coal, the second-highest grade of coal. Sub-bituminous coal is primarily used as a fuel for steam-electric power generation.
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Arch Resources, previously known as Arch Coal, is an American coal mining and processing company. The company mines, processes, and markets bituminous and sub-bituminous coal with low sulfur content in the United States. Arch Resources is the second-largest supplier of coal in the United States, behind Peabody Energy. As of 2011 the company supplied 15% of the domestic market. Demand comes mainly from generators of electricity.
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