Laurel Run mine fire

Last updated
Laurel Run mine fire
Laurel Run Road in Laurel Run, PA (4), Sept. 2023.jpg
Area along Laurel Run Road previously occupied by houses until the 1960s
DateDecember 6, 1915 (1915-12-06)
LocationRed Ash Coal Mine and surrounding areas, Luzerne County, Pennsylvania
CauseLit carbide lamp ignited coal bed
Property damageMuch of the community of Laurel Run destroyed

The Laurel Run mine fire is an underground mine fire near the communities of Laurel Run and Georgetown, in Luzerne County, Pennsylvania, in the United States. The fire started burning in 1915 at the Red Ash Coal Mine. Attempts to control it lasted from 1915 to 1957 and recommenced in 1966. [1] In the 1960s, the United States government and the Pennsylvania state government became involved in containing the fire. [2] Attempts at stopping the spread of the fire were erroneously declared successful in 1973, and the fire is still burning. [3]

Contents

Start of the fire and early history

The Laurel Run mine fire began on December 6, 1915, in the Red Ash Coal Mine. A miner accidentally left a carbide lamp hanging from a timber support, which caught fire. Because of the lack of a night watchman, the fire went unnoticed for the entire weekend. When it was noticed after work resumed the following week, attempts were made to block off its air supply by pouring sand in the area and filling the openings of the mine with concrete. The mine's owners then stated that the fire was under control. [1]

By 1921, it became evident that the mine fire had persisted and spread. The company operating the mine began placing temporary barriers to stop the spread of the fire so that the rest of the mine could continue to be worked. Mining in the area ended in 1957. At this point attempts to stop the spread of the fire also ceased. [1]

Later history

Over the years, the Laurel Run site became known as 'the burning mountain' because of smoke vented from a number of fissures leading to the abandoned underground works. In September 1962, a number of residents of the nearby community of Laurel Run were forced to abandon their homes due to subsidence (due to removal[ clarification needed ] of the mine's pillars in the area) and fumes from the mine fire. [1] [2] The pillars were columns of anthracite coal that were left to support the ground above the mine. Legitimate miners would "rob" them through mining when they couldn't otherwise meet their coal quotas, and "outlaw" miners, not affiliated with a given mine, would subsequently rob them as well when the mines were closed. The resulting subsidence at the surface could cause dangerous sink holes. The community at this point became aware of the presence of an uncontrolled mine fire in the area. [1]

In the early 1960s, the then governor of Pennsylvania William Scranton and the congressman Daniel J. Flood arrived at the area of the Laurel Run mine fire and called upon the Appalachian Regional Commission to aid in containing it. [2]

By 1964, local plant life was dying out and residents of Laurel Run were experiencing adverse symptoms such as headaches. In February 1964, high levels of carbon monoxide and carbon dioxide were detected in the area, and mine gases reaching the surface gave off a blue glow at nights. [2] On March 19, 1964, the Defense Materials, Manufacturing and Infrastructure Standing Committee announced a $1,000,000 cleanup project for the Laurel Run area. The state of Pennsylvania contributed $500,000. [4] In 1965, evacuation of Laurel Run began in earnest, led by the Appalachian Regional Commission. [2]

On April 23, 1966, a plan to control the mine fire was put into action. [1] [2] A series of boreholes were dug in the area to determine the scope of the fire. It was found that it had spread under the community of Laurel Run and also to the community of Georgetown. However, in Georgetown, the ground was relatively stable and the fire did not cause problems aboveground. [1] Clay and sand were injected into the boreholes to contain the fire. The containment efforts occupied 800,000 square feet. Amy Randolph of the Pennsylvania Department of Environmental Protection estimated that the efforts would cost $4,000,000. This figure was later revised to $9,000,000. [2] Meanwhile, the United States Department of Housing and Urban Development relocated 850 residents who lived over the mine fire. The area of the fire that was below Georgetown was controlled by blocking off the tunnels in the vicinity, robbing it of the necessary oxygen to continue burning. [1]

In 1973, the containment of the mine fire was stated to be complete, but it continues to burn into the 21st century. [1] [2] [3] The people of Laurel Run were able to gain more governmental support in combating the Laurel Run mine fire than the people of Centralia were in stopping the Centralia mine fire. [5]

In the 21st century

The Earth Conservancy considered harnessing the geothermal energy of the mine fire. [6]

In 2013, Michael Corgan, a businessman from Wilkes-Barre Township was granted permission to strip mine 40 acres of land on top of the Laurel Run mine fire, on the condition that the strip mining operations remained at least 120 feet (37 m) above the fire. Strip mining on top of a mine fire had not previously been done, although Corgan had attempted to start a strip mine in the area in 1992. [7]

The setting of the novel Whispers from the Ashes is based on the community of Laurel Run in the early 1960s, when the residents were forced to evacuate. [8]

The Laurel Run mine fire may burn for another century. [9]

Geology

The geographical setting of the Laurel Run mine fire has been compared to that of the Centralia mine fire. The Laurel Run mine fire was located on the southern spur of the Wilkes-Barre syncline. It is part of the ridge and valley geographical province. The coal beds that are on fire are the Ross bed, the Top Red Ash bed, and the Bottom Red Ash bed. The coal beds dip 10 or 15 degrees to the north. The Llewellyn Formation is situated on top of the Red Ash bed and the Pottsville Conglomerate is situated below it. [1]

Due to the geographical features of the area, the mine fire is only able to spread to the northeast, northwest, and southwest. [1]

In some areas in the vicinity of the fire, the ground has cracked open. However, the surface temperature is not as hot as the Centralia mine fire. [1] The mine fire is 200 feet (60 m) to 300 feet (90 m) underground and burns at a temperature of around 1,000 °F (540 °C). [2]

See also

Related Research Articles

<span class="mw-page-title-main">Coal</span> Combustible sedimentary rock composed primarily of carbon

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 a type of fossil fuel, 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.

<span class="mw-page-title-main">Centralia, Pennsylvania</span> Ghost town in Pennsylvania, United States

Centralia is a borough and near-ghost town in Columbia County, Pennsylvania, United States. It is part of Northeastern Pennsylvania. Its population has declined from 1,000 in 1980 to five residents in 2020 because a coal mine fire has been burning beneath the borough since 1962. Centralia, part of the Bloomsburg–Berwick metropolitan area, is the least-populated municipality in Pennsylvania. It is completely surrounded by Conyngham Township.

<span class="mw-page-title-main">Anthracite</span> Hard, compact variety of coal

Anthracite, also known as hard coal and black coal, is a hard, compact variety of coal that has a submetallic lustre. 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.

<span class="mw-page-title-main">Wilkes-Barre Township, Pennsylvania</span> First class township with home rule in Pennsylvania, United States

Wilkes-Barre Township is a township with home rule status in Luzerne County, Pennsylvania, United States. It is adjacent to the city of Wilkes-Barre. The population of the township was 3,219 at the 2020 census.

<span class="mw-page-title-main">Coal-seam fire</span> Underground smouldering of a coal deposit

A coal-seam fire is a burning of an outcrop or underground coal seam. Most coal-seam fires exhibit smouldering combustion, particularly underground coal-seam fires, because of limited atmospheric oxygen availability. Coal-seam fire instances on Earth date back several million years. Due to thermal insulation and the avoidance of rain/snow extinguishment by the crust, underground coal-seam fires are the most persistent fires on Earth and can burn for thousands of years, like Burning Mountain in Australia. Coal-seam fires can be ignited by self-heating of low-temperature oxidation, lightning, wildfires and even arson. Coal-seam fires have been slowly shaping the lithosphere and changing atmosphere, but this pace has become faster and more extensive in modern times, triggered by mining.

<span class="mw-page-title-main">Burning Mountain</span> Common name for Mount Wingen, a hill near Wingen, New South Wales, Australia

Burning Mountain, the common name for Mount Wingen, is a hill near Wingen, New South Wales, Australia, approximately 224 km (139 mi) north of Sydney just off the New England Highway. It takes its name from a smouldering coal seam running underground through the sandstone. Burning Mountain is contained within the Burning Mountain Nature Reserve, which is administered by the NSW National Parks and Wildlife Service (NPWS).

<span class="mw-page-title-main">Centralia mine fire</span> Long-burning coal-seam fire in Pennsylvania

The Centralia mine fire is a coal-seam fire that has been burning in the labyrinth of abandoned coal mines underneath the borough of Centralia, Pennsylvania, United States, since at least May 27, 1962. Its original cause and start date are still a matter of debate. It is burning at depths of up to 300 ft (90 m) over an 8 mi (13 km) stretch of 3,700 acres (15 km2). At its current rate, it could continue to burn for over 250 years. Due to the fire, in the 1980s Centralia was mostly abandoned. There were 1,500 residents at the time the fire is believed to have started, but as of 2017 it has a population of 5 and most of the buildings have been demolished.

<span class="mw-page-title-main">Linn Run State Park</span> State park in Westmoreland County, Pennsylvania

Linn Run State Park is a Pennsylvania state park on 612 acres (248 ha) in Cook and Ligonier Townships, Westmoreland County, Pennsylvania in the United States. The park borders Forbes State Forest. Two smaller streams, Grove Run and Rock Run, join in Linn Run State Park to form Linn Run which has a waterfall, Adams Falls, which can be seen at the park. This state park is just off Pennsylvania Route 381 near the small town of Rector.

<span class="mw-page-title-main">Mahanoy Creek</span> Creek in Pennsylvania

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.

<span class="mw-page-title-main">Health and environmental impact of the coal industry</span>

The health and environmental impact of the coal industry includes issues such as land use, waste management, water and air pollution, caused by the coal mining, processing and the use of its products. In addition to atmospheric pollution, coal burning produces hundreds of millions of tons of solid waste products annually, including fly ash, bottom ash, and flue-gas desulfurization sludge, that contain mercury, uranium, thorium, arsenic, and other heavy metals. Coal is the largest contributor to the human-made increase of carbon dioxide in Earth's atmosphere.

<span class="mw-page-title-main">Centralia Power Plant</span>

Centralia Big Hanaford power plant is a coal-fired power plant supplemented with natural-gas-fired units. It is located east of Centralia, Washington, United States in Lewis County. It is the only commercial coal-fired power plant in the State of Washington.

<span class="mw-page-title-main">Pittsburgh coal seam</span>

The Pittsburgh Coal Seam is the thickest and most extensive coal bed in the Appalachian Basin; hence, it is the most economically important coal bed in the eastern United States. The Upper Pennsylvanian Pittsburgh coal bed of the Monongahela Group is extensive and continuous, extending over 11,000 mi2 through 53 counties. It extends from Allegany County, Maryland to Belmont County, Ohio and from Allegheny County, Pennsylvania southwest to Putnam County, West Virginia.

Tangascootack Creek is a tributary of the West Branch Susquehanna River in Clinton County, Pennsylvania in the United States. Tangascootack Creek stretches for 11.4 miles (18.3 km) through Bald Eagle, Beech Creek and Colebrook Townships. Its watershed covers 36.5 square miles. Among its tributaries are North Fork Tangascootack Creek and Muddy Run, and there is also a swamp called Bear Swamp near the headwaters. Coal mining, including strip mining, was common in the watershed throughout the 1800s and 1900s. The creek experiences acid mine drainage, much of which comes from Muddy Run.

<span class="mw-page-title-main">Solomon Creek</span> River of the Susquehanna River, Pennsylvania

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.

The Carbondale mine fire was a mine fire in the West Side neighborhood of Carbondale, Lackawanna County, Pennsylvania in the United States. The fire, which started in 1946 and was eventually contained by the 1970s, caused at least two fatalities and millions of dollars of property damage.

<span class="mw-page-title-main">McCauley Mountain (Pennsylvania)</span> Mountain in the state of Pennsylvania

McCauley Mountain is a mountain in Columbia County, Pennsylvania, in the United States. Its official elevation is 1,571 feet (479 m) above sea level. The mountain is a synclinal mountain. Main rock formations on and near it include the Mauch Chunk Formation and the Pottsville Formation. There are also coal deposits on it. The coal deposits were discovered in 1826 and mining of them began in the 1850s. However, coal mining on the east side of the mountain proved to be a commercial failure. There are a number of ponds on the mountain, some of which were created during the mining. However, others are natural vernal pools. Some of the ponds are surrounded by hemlocks and deciduous trees. Major streams near the mountain include Scotch Run, Beaver Run, and Catawissa Creek. The mountain is named after Alexander McCauley, who settled there in 1774.

Black Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 2.6 miles (4.2 km) long and flows through Conyngham Township. The creek's watershed has an area of 3.85 square miles (10.0 km2). It is designated as a Coldwater Fishery and a Migratory Fishery. The creek is ephemeral and loses its flow to underground mines. Varying concentrations of many alkali metals, alkaline earth metals, and transition metals occur in water in the creek's watershed. The watershed typically experiences relatively mild temperatures. It is mainly accessible via U.S. Route 11, Pennsylvania Route 239, and a local road.

<span class="mw-page-title-main">Environmental issues in Appalachia</span>

Environmental issues in Appalachia, a cultural region in the Eastern United States, include long term and ongoing environmental impact from human activity, and specific incidents of environmental harm such as environmental disasters related to mining. A mountainous area with significant coal deposits, many environmental issues in the region are related to coal and gas extraction. Some extraction practices, particularly surface mining, have met significant resistance locally and at times have received international attention.

<span class="mw-page-title-main">Assumption of the Blessed Virgin Mary Ukrainian Catholic Church (Centralia)</span>

The Assumption of the Blessed Virgin Mary Ukrainian Catholic Church is a Ukrainian Catholic church in the town of Centralia, Pennsylvania. The church is the last remaining church in Centralia, which was largely abandoned after a mine fire rendered much of the town unsafe.

<span class="mw-page-title-main">Coal refuse</span> Waste from coal mining

Coal refuse is the material left over from coal mining, usually as tailings piles or spoil tips. For every tonne of hard coal generated by mining, 400 kilograms of waste material remains, which includes some lost coal that is partially economically recoverable. Coal refuse is distinct from the byproducts of burning coal, such as fly ash.

References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 Glenn B. Stracher, ed. (January 1, 2007), Geology of Coal Fires: Case Studies from Around the World, ISBN   9780813741185 , retrieved January 30, 2014
  2. 1 2 3 4 5 6 7 8 9 Abandoned Mine Research, Inc. (2005), Laurel Run Mine Fire , retrieved January 30, 2014
  3. 1 2 "PAFireLocationTable" (PDF). Pennsylvania Department of Environmental Protection. 2020-10-01. Retrieved 2021-02-06.
  4. David DeKok (April 1, 2000), Unseen Danger: A Tragedy of People, Government, and the Centralia Mine Fire, ISBN   9780595092703 , retrieved January 30, 2014
  5. Melissa A. Nolter; Daniel H. Vice; Harold Aurand Jr. (March 7, 2007), Comparison of Pennsylvania anthracite mine fires: Centralia and Laurel Run, Geological Society of America , retrieved January 30, 2014
  6. Joseph Calamia (June 24, 2010), Slow Burn, Seed magazine, archived from the original on June 30, 2010, retrieved January 30, 2014{{citation}}: CS1 maint: unfit URL (link)
  7. Rory Sweeney (February 14, 2013), Potential strip mining a concern, Times Leader, archived from the original on February 21, 2014, retrieved January 30, 2014
  8. Bernadine Elick (February 10, 2011), Book recounts tragedy of Laurel Run mine fire, The Citizens' Voice , retrieved January 30, 2014
  9. Reclamation , retrieved January 30, 2014

41°13′26″N75°51′28″W / 41.22389°N 75.85778°W / 41.22389; -75.85778