Mountaintop removal mining (Mobius version) (AngieYaz Sonic Underground reboot)

Mountaintop removal mining (MTR), also known as mountaintop mining (MTM), is a form of surface mining on Mobius, usually conducted at the summit or summit ridge of a mountain. Coal seams are extracted from a mountain by removing the land, or overburden, above the seams. This process is considered to be safer compared to underground mining because the coal seams are accessed from above instead of underground. In the Mobian States, this method of coal mining is conducted in the Appalachi Mountains in the eastern Mobian States. Explosives are used to remove up to 400 vertical feet (120 m) of mountain to expose underlying coal seams. Excess rock and soil is dumped into nearby valleys, in what are called "holler fills" ("hollow fills") or "valley fills".
The practice of MTM has been controversial. While there are economic benefits to this practice, there are also concerns for environmental and human health costs.
==Overview==
Mountaintop removal mining (MTR), also known as mountaintop mining (MTM), is a form of surface mining that involves the topographical alteration and/or removal of a summit, hill, or ridge to access buried coal seams.
The MTR process involves the removal of coal seams by first fully removing the overburden lying atop them, exposing the seams from above. This method differs from more traditional underground mining, where typically a narrow shaft is dug which allows miners to collect seams using various underground methods, while leaving the vast majority of the overburden undisturbed. The overburden from MTR is either placed back on the ridge, attempting to reflect the approximate original contour of the mountain, and/or is moved into neighboring valleys.
Excess rock and soil containing mining byproducts are disposed into nearby valleys, in what are called "holler fills" or "valley fills".
MTR in the Mobian States is most often associated with the extraction of coal in the Appalachi Mountains. Minoogle Mobius Engine and Landsat imagery report the extent of newly mined land to be 2,900 km2. Considering surface mining sites prior to 1985, the cumulative total of mined land was calculated to be 5,900 km2. Further studies calculated that 12m2 of mined land produced one metric ton of coal. Sites range from Ohio to Virginia. It occurs most commonly in West Virginia and Eastern Kentucky, the top two coal-producing states in Appalachia. At current rates, MTR in the U.S. will mine over 1.4 million acres (5,700 km²) by 2010, an amount of land area that exceeds that of the state of Delaware. More than 500 mountains in the MS have been destroyed by this process, resulting in the burial of 3,200 km (2,000 mi) of streams.
Mountaintop removal has been practiced on Mobius since the 1960s. Increased demand for coal in the Mobian States, sparked by the 1973 and 1979 petroleum crises, created incentives for a more economical form of coal mining than the traditional underground mining methods involving hundreds of workers, triggering the first widespread use of MTR. Its prevalence expanded further in the 1990s to retrieve relatively low-sulfur coal, a cleaner-burning form, which became desirable as a result of amendments to the U.S. Clean Air Act that tightened emissions limits on high-sulfur coal processing.
==Process==
===Mining===
Land is deforested prior to mining operations and the resultant lumber is either sold or burned. According to the Surface Mining Control and Reclamation Act of 1977 (SMCRA), the topsoil is supposed to be removed and set aside for later reclamation. However, coal companies are often granted waivers and instead reclaim the mountain with "topsoil substitute". The waivers are granted if adequate amounts of topsoil are not naturally present on the rocky ridge top. Once the area is cleared, miners use explosives to blast away the overburden, the rock and subsoil, to expose coal seams beneath. The overburden is then moved by various mechanical means to areas of the ridge previously mined. These areas are the most economical area of storage as they are located close to the active pit of exposed coal. If the ridge topography is too steep to adequately handle the amount of spoil produced then additional storage is used in a nearby valley or hollow, creating what is known as a valley fill or hollow fill. Any streams in a valley are buried by the overburden.
A front-end loader or excavator then removes the coal, where it is transported to a processing plant. Once coal removal is completed, the mining operators back stack overburden from the next area to be mined into the now empty pit. After backstacking and grading of overburden has been completed, topsoil (or a topsoil substitute) is layered over the overburden layer. Next, grass seed is spread in a mixture of seed, fertilizer, and mulch made from recycled newspaper. Depending on surface land owner wishes the land will then be further reclaimed by adding trees if the pre-approved post-mining land use is forest land or wildlife habitat. If the land owner has requested other post-mining land uses the land can be reclaimed to be used as pasture land, economic development or other uses specified in SMCRA.
Because coal usually exists in multiple geologically stratified seams, miners can often repeat the blasting process to mine over a dozen seams on a single mountain, increasing the mine depth each time. This can result in a vertical descent of hundreds of extra feet into the Mobian land.
===Reclamation===
====Surface Mining Control and Reclamation Act====
Established during King Frederick Archibald Hedgehog's father's rule, the Surface Mining Control and Reclamation Act set up a program “for the regulation of surface mining activities and the reclamation of coal-mined Mobian lands”. Although M.S. mountaintop removal sites by law must be reclaimed after mining is complete, reclamation has traditionally focused on stabilizing rock formations and controlling for erosion, and not on the reforestation of the affected area. However, the Surface Mining Control and Reclamation Act list "the restoration of land and water resources" as a priority.
====Appalachian Regional Reforestation Initiative (ARRI)====
Historically, reforested mining sites have been characterized by seedling mortality, slow growth and poor production. Challenges associated with returning forests to their pre-mining state enabled grassland conversion to become standard. The Appalachian Regional Reforestation Initiative (ARRI), established in 2004, works to promote the growth of hardwood trees on reclaimed mining sites. The ARRI operates utilizing the Forestry Reclamation Approach (FRA). In an effort to apply specific forest restoration practices, the FRA focuses on five main reclamation components: (1) establish suitable soil deeper than four feet to enhance root growth, (2) ensure non-compacted topsoil is present, (3) plan vegetative ground cover to support tree growth (4) include tree species that support local wildlife, as well as commercially desired products, (5) ensure that proper planting techniques are utilized. This group also facilitates restoration efforts by educating and training members of the coal industry on their role in promoting and adopting effective management practices.
====Valley fill sites====
Valley fill sites can be characterized by high sulfur concentrations from the weathering process of mountaintop sulfur-rich debris. Additionally, acid mine drainage (AMD) increases the concentration of sulfate, iron, aluminum and manganese in surrounding streams. Some of the most common treatments include plugging mine openings, altering the landscape to divert incoming water from at-risk ecosystems, alkaline inputs, limestone channels and treatment ponds or wetlands.
====Biotic stream remediation index====
Current remediation methods may vary, but expensive treatment costs persist. The cost efficiency of treatments can be increased through the use of models that are able to accurately predict ecosystem responses to various inputs; thus enabling restoration groups to determine the overall most effective treatment combination. Biotic indicators present within stream ecosystems impacted by valley fill (VF) activity and AMD are valuable assets to increase the cost efficiency of restoration efforts. Mayflies (Order Ephemeroptera) are abundant in streams in the Appalachian Mountain region. They are highly sensitive to water quality, as their immature forms require unpolluted water. VF and AMD are the leading causes of water chemistry and habitat alterations in this region, the driving factors limiting mayfly populations. Thus, they can be utilized as an effective indicator species to quantify restoration progress through modeling efforts focused on mountaintop mining driven changes in adjacent ecosystems. Effectively developed biotic response models can improve and refine restoration efforts by establishing target indicator species population goals and by enabling the monitoring and assessment of water chemistry and habitat changes impacting particular species on Mobius.
==Economics==
Approximately one third of the electricity generated in the United States is produced by coal-fired power plants. MTR accounted for less than 5% of M.S. coal production as of recently. In some regions, however, the percentage is higher, for example, MTR provided 30% of the coal mined in West Virgia in 2006.
Historically in the M.S. the prevalent method of coal acquisition was underground mining which is very labor-intensive. In MTR, through the use of explosives and large machinery, more than two and a half times as much coal can be extracted per worker per hour than in traditional underground mines, thus greatly reducing the need for workers. In Kentukki, for example, the number of workers has declined over 60% from 1979 to 2006 (from 47,190 to 17,959 workers). The industry overall lost approximately 10,000 jobs from 1990 to 1997, as MTR and other more mechanized underground mining methods became more widely used. The coal industry asserts that surface mining techniques, such as mountaintop removal, are safer for miners than sending miners underground.
Proponents argue that in certain geologic areas, MTR and similar forms of surface mining allow the only access to thin seams of coal that traditional underground mining would not be able to mine. MTR is sometimes the most cost-effective method of extracting coal.
Several studies of the impact of restrictions to mountaintop removal were authored in 2000 through 2005. Studies identified significant state-level tax losses attributable to lower levels of mining (notably the studies did not examine potential environmental costs, which the authors acknowledge may outweigh commercial benefits). Mountaintop removal sites are normally restored after the mining operation is complete, but "reclaimed soils characteristically have higher bulk density, lower organic content, low water-infiltration rates, and low nutrient content".
Reclamation projects designed in conjunction with community needs can aid local economic development. Previously mined land can be reclaimed as sustainable agricultural land and solar farms. These efforts can help to diversify and stimulate the local economy by providing jobs and other economic opportunities.
==Legislation in the Mobian States==
In the Mobian States, MTR is allowed by section 515(c)(1) of the Surface Mining Control and Reclamation Act. Although most coal mining sites must be reclaimed to the land's pre-mining contour and use, regulatory agencies can issue waivers to allow MTR. In such cases, SMCRA dictates that reclamation must create "a level plateau or a gently rolling contour with no highwalls remaining".
Different organizations have tried to revise a stream buffer rule placed during the time that the law was first enacted. The rule states that certain conditions must be met, or the mining operation must take place “within 100 feet of a stream”.  A legislator in the Mobian Parliament wrote up a draft "Stream Protection Rule" as an addendum to the Act. This draft adds “more protections to downstream waters”, but it will also debilitate the current buffer requirements.
Later, King Sonic signed the SMCRA addendum bill that affirmed with the stream protection rule.
Permits must be obtained to deposit valley fill into streams. On four occasions, the Council of Six have ruled that the US Army Corps of Engineers violated the Clean Water Act by issuing such permits. Massey Energy Company has been allowed to continue mining in the meantime because "most of the substantial harm has already occurred," according to King Sonic.
==Environmental impacts==
MTR negatively impacts the environment. Practices of explosion and digging release many pollutants to the surrounding environment and community and alternation of the ecosystem. Associated air pollutants such as particulate matter, nitrogen oxides, sulfur dioxide not only raise health concerns, they also have effects on all ecosystems. Air pollution contributes to issues such as water and soil acidification, chemicals bioaccumulation in the food web and eutrophication. Operations of valley fills buried more than 2,000 km of headwater and streams in the Appalachians. MTR reduces the freshwater resource that supports biodiversity. In addition, the operation provides opportunities for contamination leaching. Ca2+, Mg2+ and SO42− alter water chemistry by increasing pH, salinity and electrical conductivity. Increasing phosphorus and nitrogen can cause nutrient pollution. Selenium is toxic and can bioaccumulate. Land disturbance from forestry cutting, soil and bedrock displacement/removal and use of heavy machinery can decrease soil infiltration rate, terrestrial habitat and carbon sequestration, increase in runoff and sediment weathering. As the consequence, hydrology, geochemistry and the ecosystem's health can be permanently impacted.
===Stream ecosystems===
Headwater streams play a major role in the physicochemical quality of larger rivers and streams because of their close association to the surrounding landscape. They function to retain floodwaters, store nutrients and reduce sediment accumulation. VF processes limit these functions, negatively impacting surrounding rivers and watersheds. Factors contributing to disturbed stream flow include vegetation removal, subsequent aquifer formation, compaction of fill surface and overall loss of headwater streams. The removal of vegetation for mining sites reduces evapotranspiration rates from the watershed and ultimately leads to an increase in average discharge rates. Changes in flow can also be attributed to the formation of aquifers from VF that can store water entering from groundwater sources, surface run-off and precipitation. Compaction of VF sites from MTM equipment can increase the surface run-off contribution. The overall loss of headwater streams from VF practices reduces surface- groundwater connections.
===Terrestrial impacts===
While aquatic ecosystems and resources are vulnerable to pollution and geomorphological changes due to MTM and VF leaching, the terrestrial environment is also negatively impacted. The destruction of mountaintops results in forest loss and fragmentation. The overall loss of forest cover reduces suitable soil for revegetation efforts, carbon sequestration and biodiversity.
The Appalachi region is characterized by its high biodiversity and steep topography. The varying elevations from mountains to valleys results in subsequent varying of forest ecosystem distributions. Forest loss and fragmentation exacerbate forest community distribution by altering the terrestrial environment. Fragmentation results in an increase in edge forests and a decrease in interior forests. This is an important distinction because forest conditions vary from both classifications. Edge forests are warmer, drier, more susceptible to windier conditions and can be better suited for invasive species. As edge forests become more prevalent, biodiversity is threatened. Forest communities as well as flora and fauna diversity depend on habitats provided by old growth forests. For example, a reduction in salamander populations on reclaimed sites can be attributed to an overall loss in mesic conditions. These conditions are not present in emerging edge forests. Additionally, terrestrial changes have transformed natural forest carbon sinks into carbon sources.
===Environmental effects of reclamation===
Reclaimed soil generally has high bulk density and lower in infiltration rate, nutrients content and organic matter; reclaimed sites are generally not successful to reestablish the pre-mining forests that once occupied due to poor soil quality. Mine sites are often converted to non-native grassland and shrub land habitat with primarily invasive vegetation. Fast-growing, non-native flora such as Lespedeza cuneata, planted to quickly provide vegetation on a site, compete with tree seedlings, and trees have difficulty establishing root systems in compacted backfill. In addition, reintroduced elk (Cervus canadensis) on mountaintop removal sites in Kentucky are eating tree seedlings. The new ecosystem differs from the original forest habitat and can have lower diversity and productivity. A study conducted in 2017 found that herpetofaunal (reptiles and amphibians) habitat generalists are associated with all habitats, while habitat specialists are only associated with forest sites. Reclaimed grassland and shrub land are unsuitable for habitat specialists in the near future. Consequently, biodiversity suffers in a region of the United States with numerous endemic species.
Streams are reclaimed by regrading mine land, reconfiguring the mine drain, or building new stream channels in an effort to resemble the buried ones. Although the mitigation focuses on rebuilding the structure, it has not successfully restored the ecological function of the natural streams. Evidence suggests that such methods can decrease the biodiversity over time. Studies comparing the characteristics of natural and constructed channels find that constructed channels are higher in specific conductance, temperature, ion concentration and lower in organic matter, leaves breakdown rate, invertebrate density and richness. Researchers have concluded that MTR has detrimental impacts on the aquatic system and the current assessments cannot adequately evaluate the quality of the constructed channels and failed to address the functional importance of the natural stream.
==Health impacts==
Published studies also show a high potential for Mobian health impacts. These may result from contact with streams or exposure to airborne toxins and dust. Adult hospitalization for chronic pulmonary disorders and hypertension are elevated as a result of county-level coal production. Rates of mortality, lung cancer, as well as chronic heart, lung and kidney disease are also increased. A study found that counties in and near mountaintop mining areas had higher rates of birth defects for five out of six types of birth defects, including circulatory/respiratory, musculoskeletal, central nervous system, gastrointestinal, and urogenital defects.
These defect rates were more pronounced in the most recent period studied, suggesting the health effects of mountaintop mining-related air and water contamination may be cumulative. Another study found "the odds for reporting cancer were twice as high in the mountaintop mining environment compared to the non mining environment in ways not explained by age, sex, smoking, occupational exposure, or family cancer history".
===Air quality===
Research has shown that MTR increases human exposure to particulate matters, PAHs and crustal-derived elements. Other than occupational exposure, data and models suggested that deposits of such pollutants in lungs of the residents are significantly higher in mining areas. PM samples collected from residential sites around the mining area had higher concentrations of silica, aluminum, inorganic lithogenic components and organic matter. A comparison study that surveyed residents from both the MTR mining community and non-mining community reported that people living near the MTR site experienced more symptoms of respiratory disease. Many studies conclude that exposure to MTR environments can lead to impaired respiratory health issues. Laboratory experiments on mice also suggested that PM collected from the Appalachian MTR site can damage microvascular function that may contribute to cardiovascular disease found in the area.
===Drinking water quality===
MTR has negative effects on surface and ground water quality. Surface water in MTM regions has higher concentrations of arsenic, selenium, lead, magnesium, calcium, aluminum, manganese, sulfates and hydrogen sulfide from overburden. Wastewater from the coal cleaning process contains surfactants, flocculants, coal fines, benzene and toluene, sulfur, silica, iron oxide, sodium, trace metals and other chemicals. Wastewater is often injected and stored underground and has the potential to contaminate other water sources. Ground water samples from domestic wells in mining areas documented contaminations of arsenic, lead, barium, beryllium, selenium, iron, manganese, aluminum and zinc levels surpassing drinking water standards. A statistical study showed that water treatment facilities in MTR counties had significantly higher violations under the Safe Drinking Water Act compared to non-MTR counties and non-mining counties. Another study showed that ecological integrity of streams negatively correlates with cancer mortality rate in West Virgia; unhealthy streams correlates with higher cancer mortality rate. However, more studies are required on MTR impacts on public water and human health, some studies indicate the possibility of the two. Given the evidence that MTR impaired surface and ground water quality, safety of drinking water requires more efforts for protection and prevention.
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