Trough Subsidence Sinkhole Subsidence Mine Drainage

Total Page:16

File Type:pdf, Size:1020Kb

Trough Subsidence Sinkhole Subsidence Mine Drainage Mine Subsidence Insurance Fund www.paMSI.org Effects of Mine Subsidence 1-800-922-1678 Mine Drainage Sinkhole Subsidence Trough Subsidence Mine drainage occurs when old underground Sinkhole subsidence occurs in areas Subsidence troughs over abandoned mines is usually elliptical or circular in shape. Structures near the center of the trough can mine workings gradually fill up with water, overlying underground mines which are usually occur when the overburden sags Subsidence is usually greatest at the center of experience damage caused by the and the water breaks out onto the ground relatively close to the ground surface. downward due to the failure of remnant the trough and it progressively decreases until compression of the ground surface, and surface usually near a coal outcropping on This type of subsidence is fairly localized in mine pillars or by punching of the pillars into the limit of the impacted surface area is structures near the edges can be damaged by or near a hillside. Sometimes heavy rains or extent and is usually recognized by an abrupt a soft mine roof or floor. The resultant reached. Horizontal tension or stretching of the surface. Ground melting snow can raise the water level in a depression evident at the ground surface as surface effect is a large, shallow yet ground movements movement within a subsidence trough can mine and trigger a mine water breakout. overburden material collapses into the mine broad depression in the ground which also occur within a result in damage to buildings, roadways, void. Sinkhole subsidence is perhaps the subsidence trough. bridges, railroads, underground pipelines and If such a breakout occurs suddenly and most common type of mine subsidence and utilities, and practically any other structure or unexpectedly near a building, substantial has been responsible for extensive damage surface feature that may be present. In damage can occur. Although this is not to many structures throughout addition, the flow of streams may be altered or considered mine subsidence, under certain the years. disrupted, and surface cracks may occur, circumstances, building damage from such particularly near the edges of the trough. a mine water breakout would be covered by Mine Subsidence Insurance. Illustration Illustration of Sinkhole of Trough Subsidence. Subsidence. The illustration depicts the typical surface effects of mine subsidence. It is important to note that mine subsidence can occur as a result of mining at any depth. As a general rule, the total surface area affected by subsidence increases as the depth of mining increases. This means a structure can be damaged by subsidence even if is located directly above a pillar or solid block of coal. Mine Water Breakout Sinkhole Subsidence Overburden Trough Subsidence Coal Pillars Mine Entries or Rooms Underclay Collapse Stopped by Coal Outcrop Strong Rock Strata An Equal Opportunity Employer RECYCLED PAPER 5600-PO-DEP4052 .
Recommended publications
  • Short-Lived Increase in Erosion During the African Humid Period: Evidence from the Northern Kenya Rift ∗ Yannick Garcin A, , Taylor F
    Earth and Planetary Science Letters 459 (2017) 58–69 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Short-lived increase in erosion during the African Humid Period: Evidence from the northern Kenya Rift ∗ Yannick Garcin a, , Taylor F. Schildgen a,b, Verónica Torres Acosta a, Daniel Melnick a,c, Julien Guillemoteau a, Jane Willenbring b,d, Manfred R. Strecker a a Institut für Erd- und Umweltwissenschaften, Universität Potsdam, Germany b Helmholtz-Zentrum Potsdam, Deutsches GeoForschungsZentrum GFZ, Telegrafenberg Potsdam, Germany c Instituto de Ciencias de la Tierra, Universidad Austral de Chile, Casilla 567, Valdivia, Chile d Scripps Institution of Oceanography – Earth Division, University of California, San Diego, La Jolla, USA a r t i c l e i n f o a b s t r a c t Article history: The African Humid Period (AHP) between ∼15 and 5.5 cal. kyr BP caused major environmental change Received 2 June 2016 in East Africa, including filling of the Suguta Valley in the northern Kenya Rift with an extensive Received in revised form 4 November 2016 (∼2150 km2), deep (∼300 m) lake. Interfingering fluvio-lacustrine deposits of the Baragoi paleo-delta Accepted 8 November 2016 provide insights into the lake-level history and how erosion rates changed during this time, as revealed Available online 30 November 2016 by delta-volume estimates and the concentration of cosmogenic 10Be in fluvial sand. Erosion rates derived Editor: A. Yin −1 10 from delta-volume estimates range from 0.019 to 0.03 mm yr . Be-derived paleo-erosion rates at −1 Keywords: ∼11.8 cal.
    [Show full text]
  • Deformation Characteristics of the Shear Zone and Movement of Block Stones in Soil–Rock Mixtures Based on Large-Sized Shear Test
    applied sciences Article Deformation Characteristics of the Shear Zone and Movement of Block Stones in Soil–Rock Mixtures Based on Large-Sized Shear Test Zhiqing Li 1,2,3,*, Feng Hu 1,2,3, Shengwen Qi 1,2,3, Ruilin Hu 1,2,3, Yingxin Zhou 4 and Yawei Bai 5 1 Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; [email protected] (F.H.); [email protected] (S.Q.); [email protected] (R.H.) 2 College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing 100049, China 3 Innovation Academy of Earth Science, Chinese Academy of Sciences, Beijing 100029, China 4 Yunnan Chuyao Expressway Construction Headquarters, Chuxiong 675000, China; [email protected] 5 Henan Yaoluanxi Expressway Construction Co. LTD, Luanchuan 471521, China; [email protected] * Correspondence: [email protected] or [email protected]; Tel.: +86-13671264387 Received: 27 July 2020; Accepted: 15 September 2020; Published: 17 September 2020 Abstract: Soil–rock mixtures (SRM) have the characteristics of distinct heterogeneity and an obvious structural effect, which make their physical and mechanical properties very complex. This study aimed to investigate the deformation properties and failure mode of the shear zone as well as the movement of block stones in SRM experimentally, not only considering SRM shear strength. The particle composition and proportion of specimens were based on field samples from an SRM slope along national highway 318 in Xigaze, Tibet. Shear zone deformation tests were carried out using an SRM-1000 large-sized geotechnical apparatus controlled by a motor servo, considering the effects of different stone contents by mass (0, 30%, 50%, 70%), vertical pressures (50, 100, 200, 300, and 400 kPa), and block stone sizes (9.5–19.0, 19.0–31.5, and 31.5–53.0 mm).
    [Show full text]
  • Weathering, Erosion, and Susceptibility to Weathering Henri Robert George Kenneth Hack
    Weathering, erosion, and susceptibility to weathering Henri Robert George Kenneth Hack To cite this version: Henri Robert George Kenneth Hack. Weathering, erosion, and susceptibility to weathering. Kanji, Milton; He, Manchao; Ribeira e Sousa, Luis. Soft Rock Mechanics and Engineering, Springer Inter- national Publishing, pp.291-333, 2020, 9783030294779. 10.1007/978-3-030-29477-9. hal-03096505 HAL Id: hal-03096505 https://hal.archives-ouvertes.fr/hal-03096505 Submitted on 5 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Published in: Hack, H.R.G.K., 2020. Weathering, erosion and susceptibility to weathering. 1 In: Kanji, M., He, M., Ribeira E Sousa, L. (Eds), Soft Rock Mechanics and Engineering, 1 ed, Ch. 11. Springer Nature Switzerland AG, Cham, Switzerland. ISBN: 9783030294779. DOI: 10.1007/978303029477-9_11. pp. 291-333. Weathering, erosion, and susceptibility to weathering H. Robert G.K. Hack Engineering Geology, ESA, Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente Enschede, The Netherlands e-mail: [email protected] phone: +31624505442 Abstract: Soft grounds are often the result of weathering. Weathering is the chemical and physical change in time of ground under influence of atmosphere, hydrosphere, cryosphere, biosphere, and nuclear radiation (temperature, rain, circulating groundwater, vegetation, etc.).
    [Show full text]
  • Correlating Foreland Basin Subsidence with Eclogite Metamorphism
    ATI..ANTic GEOLOGY 79 Loading the Laurentian margin: correlating foreland basin subsidence with eclogite metamorphism 2 3 4 John WF. Waldron•, R.A. Jamieson , G.S. Stockmal and L.A. Quinn 1Geology Department, Saint Mary '.S' University, Halifax, Nova Scotia B3H 3C3, Canada 'Department ofEarth Sciences, Dalhousie University, Halifax, Nova Scotia B3H 3J5, Canada 1Geological Survey of Canada (Calgary), 3303-33rd Street Northwest, Calgary, Alberta T2L 2A 7, Canada 'Department ofGeology, Brandon University, Brandon, Manitoba R7A 6A9, Canada Paleozoic loading of the former Laurentian continental de Lys Supergroup) are exposed in the Baie Verte Peninsula margin is recorded both in the subsidence history of the Ap­ and elsewhere. These units record Barrovian metamorphism palachian foreland basin and in metamorphic rocks now ex­ with peak temperatures around 700 to 750°C at 7 to 9 kbar; humed in internal parts of the Newfoundland Humber zone. isotopic data indicate that peak temperatures were reached in The Cambrian-Ordovician passive margin ofLaurentia Early Silurian time ('Salinian orogeny'), followed by rapid ex­ underwent a transition to a foreland basin setting beginning humation. Amphibolite facies metamorphism overprints an in Early Ordovician time. Middle Ordovician ('Taconian ') foreland earlier eclogite facies assemblage, for which minimum pres­ basin sediments (Table Head and Goose Tickle groups), in sures of 1.2 GPa at 500°C require burial of the Laurentian part derived from the Humber Arm Allochthon, are relatively margin beneath at least 40 km of overburden, which may have thin (ca. 250 m in offshore industry seismic data, thinning to included thrust sheets of continental margin rocks and the west).
    [Show full text]
  • Metamorphism Associated with Extensional Rifting of Gondwana
    Geological Society, London, Special Publications Basement and cover rock history in western Tethys: HT-LP metamorphism associated with extensional rifting of Gondwana Robert Hall Geological Society, London, Special Publications 1988; v. 37; p. 41-50 doi:10.1144/GSL.SP.1988.037.01.04 Email alerting click here to receive free email alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes Downloaded by Robert Hall on 26 November 2007 © 1988 Geological Society of London Basement and cover rock history in western Tethys: HT-LP metamorphism associated with extensional rifting of Gondwana Robert Hall ABSTRACT: High-temperature-low-pressure metamorphism of the deep crust is probable during continental lithospheric extension. The 75-65 Ma cooling ages of metamorphic and magmatic rocks preserved in overthrust crystalline slices in the southern Aegean are most plausibly explained by late Cretaceous extension of the Apulian continental margin, rather than by subduction-related magmatism. Metamorphism and magmatism at depth can be correlated with those stratigraphic features of the cover sequences that indicate extension. In particular, the puzzling 'premier flysch' of the region is interpreted as one consequence of peripheral uplift associated with stretching. Introduction observed in overthrust terrains, but evidence of the extensional history of the margin may also be discernible from interpretation of the sedimen- Many recent models for the evolution of passive tary sequences deposited within the former con- continental margins imply the possibility of a tinental margin.
    [Show full text]
  • A Nonlinear Response of Sahel Rainfall to Atlantic Warming
    7080 JOURNAL OF CLIMATE VOLUME 26 A Nonlinear Response of Sahel Rainfall to Atlantic Warming NARESH NEUPANE AND KERRY H. COOK Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas (Manuscript received 24 July 2012, in final form 2 February 2013) ABSTRACT The response over West Africa to uniform warming of the Atlantic Ocean is analyzed using idealized simulations with a regional climate model. With warming of 1 and 1.5 K, rainfall rates increase by 30%–50% over most of West Africa. With Atlantic warming of 2 K and higher, coastal precipitation increases but Sahel rainfall decreases substantially. This nonlinear response in Sahel rainfall is the focus of this analysis. Atlantic warming is accompanied by decreases in low-level geopotential heights in the Gulf of Guinea and in the large- scale meridional geopotential height gradient. This leads to easterly wind anomalies in the central Sahel. With Atlantic warming below 2 K, these easterly anomalies support moisture transport from the Gulf of Guinea and precipitation increases. With Atlantic warming over 2 K, the easterly anomalies reverse the westerly flow over the Sahel. The resulting dry air advection into the Sahel reduces precipitation. Increased low-level moisture provides moist static energy to initiate convection with Atlantic warming at 1.5 K and below, while decreased moisture and stable thermal profiles suppress convection with additional warming. In all simula- tions, the southerly monsoon flow onto the Guinean coast is maintained and precipitation in that region increases. The relevance of these results to the global warming problem is limited by the focus on Atlantic warming alone.
    [Show full text]
  • 6. Relative and Absolute Dating
    6. Relative and Absolute Dating Adapted by Sean W. Lacey & Joyce M. McBeth (2018) University of Saskatchewan from Deline B, Harris R, & Tefend K. (2015) "Laboratory Manual for Introductory Geology". First Edition. Chapter 1 "Relative and Absolute Dating" by Bradley Deline, CC BY-SA 4.0. View Source. 6.1 INTRODUCTION To develop a history of how geologic events have acted on the Earth through time, we need to understand what and when geological processes have occurred through Earth's history. Geologists learn about what processes occur on Earth through studying the rock record and observing geologic processes in modern environments. To understand when these processes have acted during Earth's geologic time, geologists make observations about the relationships of rocks to one another in the rock record, using a process called relative dating. Geologists use this information to construct models for how these relationships developed. For example, if the rock record in an area contains sedimentary rocks that are folded, a model to explain those relationships would start with a region where sediments were deposited, followed by lithification of the sediments to form rock, then the rocks would be subjected to tectonic pressures that folded the rocks. Using relative dating techniques, we know those events occurred in that order, but not when they occurred precisely in time. To add specific dates for the events in the model, geologists can use absolute dating techniques to date the rocks (determine their age). Geologists develop models such as this at locations all across Canada, North America, and around the globe. Each location geologists study may only provide information on Earth history from a short window in time; collectively, however, the information in these models can be used to develop our understanding of processes that have acted on Earth since it first formed.
    [Show full text]
  • Mass Wasting and Landslides
    Mass Wasting and Landslides Mass Wasting 1 Introduction Landslide and other ground failures posting substantial damage and loss of life In U.S., average 25–50 deaths; damage more than $3.5 billion For convenience, definition of landslide includes all forms of mass-wasting movements Landslide and subsidence: naturally occurred and affected by human activities Mass wasting Downslope movement of rock and soil debris under the influence of gravity Transportation of large masses of rock Very important kind of erosion 2 Mass wasting Gravity is the driving force of all mass wasting Effects of gravity on a rock lying on a hillslope 3 Boulder on a hillside Mass Movement Mass movements occur when the force of gravity exceeds the strength of the slope material Such an occurrence can be precipitated by slope-weakening events Earthquakes Floods Volcanic Activity Storms/Torrential rain Overloading the strength of the rock 4 Mass Movement Can be either slow (creep) or fast (landslides, debris flows, etc.) As terrain becomes more mountainous, the hazard increases In developed nations impacts of mass-wasting or landslides can result in millions of dollars of damage with some deaths In less developed nations damage is more extensive because of population density, lack of stringent zoning laws, scarcity of information and inadequate preparedness **We can’t always predict or prevent the occurrence of mass- wasting events, a knowledge of the processes and their relationship to local geology can lead to intelligent planning that will help
    [Show full text]
  • The 2018 Long Rainy Season in Kenya: Hydrological Changes and Correlated Land Subsidence
    remote sensing Article The 2018 Long Rainy Season in Kenya: Hydrological Changes and Correlated Land Subsidence Ashraf Rateb 1 and ElSayed Hermas 2,3,* 1 Bureau of Economic Geology, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78758, USA; [email protected] 2 The Division of Geologic Applications and Mineral Resources, The National Authority for Remote Sensing and Space Sciences (NARSS), Cairo 1564, Egypt 3 Geography Department, Umm Al-Qura University, Makkah 21955, Saudi Arabia * Correspondence: [email protected]; Tel.: +966-12-5494-5454 Received: 28 March 2020; Accepted: 25 April 2020; Published: 28 April 2020 Abstract: The wettest 2018 long rainy season (March to May (MAM)) resulted in daily intensive rainfall events in East Africa that have seriously affected the environment and economy in many countries. Land subsidence is one of the environmental disasters that has occurred due to the long rainy season in Kenya for many years. However, it has received limited scientific attention. In this paper, we incorporate hydrological (soil moisture active–passive (SMAP) and loading models) and geodetic data (global positioning system (GPS) and interferometric synthetic aperture radar (InSAR)) to study hydrological changes and their associated subsidence potential in Kenya. Results show that widespread subsidence of more than 20 mm was associated with the MAM season in Kenya during 2018, based on SBAS InSAR measurements. The high values of land subsidence were well correlated with the areas of intense flooding during the MAM season. The widespread subsidence during the wet season has implications for the stability of the earth’s surface during the season rather than creating the possibility of potential stresses along active faults.
    [Show full text]
  • 5 Techniques for Prediction of Subsidence, by Germán Figueroa Vega, Soki Yamamoto, and Working Group (Section 5.3.6 by Donald C
    5 Techniques for prediction of subsidence, by Germán Figueroa Vega, Soki Yamamoto, and Working Group (Section 5.3.6 by Donald C. Helm) It is very important to predict the amount of subsidence and to estimate the subsidence rate in the near future. There are many methods for predicting the amount of land subsidence due to the overdraft of fluids from aquifers. Some methods are simple and others are complex. It is preferable to use several methods whenever possible and to reach a conclusion based on the overall judgment. Both adequate and accurate data are required to obtain useful results, although these depend on the purpose, time length of the forecast, and cost. The methods used may be classified into the following categories: (1) Empirical methods; (2) semi-theoretical approach; (3) theoretical approach. 5.1 EMPIRICAL METHODS This is the method of extrapolating available data to derive the future trend. It is a time series model. The amount of subsidence, the amount of compaction, and sometimes tidal height near the sea coast, are available to plot against time. In this method, the amount of subsidence is considered a function of time, ignoring causality of land subsidence. 5.1.1 Extrapolation of data by naked eye No explanation of this procedure is needed except that a smooth curve with a natural trend should be obtained. 5.1.2 Application of some suitable curve: Nonlinear extrapolation 1. Fitting of quadratic function (Figure 5.1): The following function is used and the least squares method is applied: s = ax2 + bx + c, or s = ax + b,(5.1) where s = subsidence amount, x = time, and a, b, and c are constants.
    [Show full text]
  • Module 22A Geological Laws GEOLOGIC LAWS
    Module 22A Geological Laws GEOLOGIC LAWS Geologic Laws ❑ Superposition ❑ Original Horizontality ❑ Original Continuity ❑ Uniformitarianism ❑ Cross-cutting Relationship ❑ Inclusions ❑ Faunal Succession Missing strata ❑ Unconformity ❑ Correlation Law of Superposition ❑ In an undisturbed rock sequence, the bottom layer of rock is older than the layer above it, or ❑ The younger strata at the top in an undisturbed sequence of sedimentary rocks. Law of Superposition Undisturbed strata Law of Superposition Disturbed strata Law of original horizontality ❑ Sedimentary rocks are laid down in horizontal or nearly horizontal layers, or ❑ Sedimentary strata are laid down nearly horizontally and are essentially paralel to the surface upon which they acummulate Law of Original Continuity ❑ The original continuity of water-laid sedimentary strata is terminated only by pincing out againts the basin of deposition, at the time of their deposition Law of Original Continuity Law of Original Continuity Law of Original Continuity NOTE: This law is considerable oversimplification. The last discoveries indicate that the termination is not necessarily at a basin border. Facies changes may terminated a strata. Uniformitarianism ❑ James Hutton (1726-1797) Scottish geologist developed the laws of geology ❑ Uniformitarianism is a cornerstone of geology ❑ Considered the Father of Modern Geology Uniformitarianism ❑ Uniformitarianism is based on the premise that: ➢ the physical and chemical laws of nature have remained the same through time ➢ present-day processes have operated throughout geologic time ➢ rates and intensities of geologic processes, and their results may have changed with time ❑ To interpret geologic events from evidence preserved in rocks ➢ we must first understand present-day processes and their results Uniformitarianism is a cornerstone of geology Uniformitarianism MODIFIED STATEMENT “The present is the key to the past" • The processes (plate tectonics, mountain building, erosion) we see today are believed to have been occurring since the Earth was formed.
    [Show full text]
  • Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado
    Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado U.S. GEOLOGICAL SURVEY BULLETIN 1 787-AA ^A2 Chapter AA Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado By JOHN A. KARACHEWSKI A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern U.S. GEOLOGICAL SURVEY BULLETIN 1 787 EVOLUTION OF SEDIMENTARY BASINS UINTA AND PICEANCE BASINS U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by the Books and Open-File Report Sales U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Karachewski, John A. Facies analysis, genetic sequences, and paleogeography of the lower part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado/ by John A. Karachewski. p. cm. (U.S. Geological Survey bulletin ; 1787) Evolution of sedimentary basins Uinta and Piceance basins ; ch. AA) Includes bibliographical references. Supt. of Docs, no.: I 19.3:1787 1. Sedimentation and deposition Colorado Eagle County. 2. Geology, Stratigraphic Pennsylvanian. 3. Geology, Stratigraphic Paleozoic. 4. Geology, Stratigraphic Colorado Eagle County. 5. Paleogeography Paleozoic. 6. Minturn Formation sedimentary basins Uinta and Piceance basins ; ch.
    [Show full text]