US Geological Survey Karst Interest Group Proceedings, Fayetteville
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Introduction to Virginia's Karst
Introduction to Virginia’s Karst A presentation of The Virginia Department of Conservation and Recreation’s Karst Program & Project Underground Karst - A landscape developed in limestone, dolomite, marble, or other soluble rocks and characterized by subsurface drainage systems, sinking or losing streams, sinkholes, springs, and caves. Cross-section diagram by David Culver, American University. Karst topography covers much of the Valley and Ridge Province in the western third of the state. Aerial photo of karst landscape in Russell County. Smaller karst areas also occur in the Cumberland Plateau, Piedmont, and Coastal Plain provinces. At least 29 counties support karst terrane in western Virginia. In western Virginia, karst occurs along slopes and in valleys between mountain ridges. There are few surface streams in these limestone valleys as runoff from mountain slopes disappears into the subsurface upon contact with the karst bedrock. Water flows underground, emerging at springs on the valley floor. Thin soils over fractured, cavernous limestone allow precipitation to enter the subsurface directly and rapidly, with a minimal amount of natural filtration. The purer the limestone, the less soil develops on the bedrock, leaving bare pinnacles exposed at the ground surface. Rock pinnacles may also occur where land use practices result in massive soil loss. Precipitation mixing with carbon dioxide becomes acidic as it passes through soil. Through geologic time slightly acidic water dissolves and enlarges the bedrock fractures, forming caves and other voids in the bedrock. Water follows the path of least resistance, so it moves through voids in rock layers, fractures, and boundaries between soluble and insoluble bedrock. -
Living with Karst Booklet and Poster
Publishing Partners AGI gratefully acknowledges the following organizations’ support for the Living with Karst booklet and poster. To order, contact AGI at www.agiweb.org or (703) 379-2480. National Speleological Society (with support from the National Speleological Foundation and the Richmond Area Speleological Society) American Cave Conservation Association (with support from the Charles Stewart Mott Foundation and a Section 319(h) Nonpoint Source Grant from the U.S. Environmental Protection Agency through the Kentucky Division of Water) Illinois Basin Consortium (Illinois, Indiana and Kentucky State Geological Surveys) National Park Service U.S. Bureau of Land Management USDA Forest Service U.S. Fish and Wildlife Service U.S. Geological Survey AGI Environmental Awareness Series, 4 A Fragile Foundation George Veni Harvey DuChene With a Foreword by Nicholas C. Crawford Philip E. LaMoreaux Christopher G. Groves George N. Huppert Ernst H. Kastning Rick Olson Betty J. Wheeler American Geological Institute in cooperation with National Speleological Society and American Cave Conservation Association, Illinois Basin Consortium National Park Service, U.S. Bureau of Land Management, USDA Forest Service U.S. Fish and Wildlife Service, U.S. Geological Survey ABOUT THE AUTHORS George Veni is a hydrogeologist and the owner of George Veni and Associates in San Antonio, TX. He has studied karst internationally for 25 years, serves as an adjunct professor at The University of Ernst H. Kastning is a professor of geology at Texas and Western Kentucky University, and chairs Radford University in Radford, VA. As a hydrogeolo- the Texas Speleological Survey and the National gist and geomorphologist, he has been actively Speleological Society’s Section of Cave Geology studying karst processes and cavern development for and Geography over 30 years in geographically diverse settings with an emphasis on structural control of groundwater Harvey R. -
Chihuahua Norte
CHIHUAHUA NORTE ENGLISH VERSION Metropolitan Mission San Ignacio Cathedral. de Loyola, Cusárare. Chihuahua Other highlights include the Gov- Creel O ernment Palace, which also houses RE The state capital, founded in the Hidalgo Museum; the Munici- Designated a “magical town” by the inosa– 1709, has numerous attractions. pal Palace; the Museum of the Mexican Tourism Ministry, it was first P Visit its religious monuments, Mexican Revolution, also known founded in 1907 as a train stop. It is DO ES R A such as: the Metropolitan Cathe- as Villa’s House or Quinta Luz; the regarded as the gateway to the in- C O RE Juárez House Museum of Loyalty M / RI dral; the Church of Santa Rita, digenous Tarahumara zone and to T the city’s patron saint; the Church to the Republic; the Quinta Ga- the famed Copper Canyon. Visit the inosa– of San Francisco, one of the city’s meros University Culture Center, P Tarahumara Culture Folk Art Mu- PHOTO: © CP PHOTO: a neoclassical style building with DO ES oldest, and the Church of El Sa- R seum and the Church of Cristo Rey. A grado Corazón de Jesús. Rococo and Art Nouveau details, C Nearby is the town of Cusárare and M / RI T from there Cusárare Falls and the Urique Madera Mission and Museum of San Igna- cio de Loyola. One of the oldest towns in the Tara- It is home to Peñitas Dam, La Man- PHOTO: © CP PHOTO: humara region. Buy local folk art and ga Ranch as well as the Campo O Cerocahui sample tesqüino (corn beer). -
Chemical Engineering at UCSB 2020 Newsletter a LETTER from the CHAIR Dear Friends, All Is Normally a Wonderful Time of Anticipation in the Department
Chemical Engineering at UCSB 2020 Newsletter A LETTER FROM THE CHAIR Dear Friends, all is normally a wonderful time of anticipation in the department. Research is in high gear while we have had Fjust enough time to wish one graduating class well in their future careers and begin to look forward to and plan for the arrival of a new generation of undergraduate and graduate students. The view from Engineering II is normally spectacular and May Gray and June Gloom make way for blue skies and white water below the cliffs. For all of us, 2020 has been a year of unprecedented and at times unsettling change, but the anticipatory feeling of Fall is the same. We are starting to see the opportunities amidst the challenges and renew our commitment to rising above the storm for the betterment of our society. I cannot say enough about the remarkable ways in which our faculty, staff, and students have been a bright light this year. As we made an abrupt shift to remote teaching and shut down of experimental research laboratories, creative, innovative solutions emerged from every corner. A core group of faculty taught a series of crash courses in online teaching in early March just before an abrupt shift to remote instruction at the end of winter quarter. We held similar trainings for spring quarter TAs, who later helped us discover that online submission and grading of work is remarkably easier than the usual way. The faculty have now spent this summer realizing that the ability to slow us down and replay us (via recorded lectures) led to greater learning for some students while the loss of personal connection was hard on all of us. -
Review on the Formation and Geochemistry of the Mega Crystals of Naica, México
EGU2020-20593 https://doi.org/10.5194/egusphere-egu2020-20593 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Review on the formation and geochemistry of the mega crystals of Naica, México. Ana Laura Gutiérrez Gutiérrez, Maria de Jesus Puy y Alquiza, and Pooja Kshirsagar Universidad de Guanajuato, Division de Ingenierias, Departamento de Ingenierías en Minas, Metalurgia y Geología., Guanajuato, México ([email protected])) In the state of Chihuahua, Mexico, a mine located in Naica is one of the most important Pb and Zn deposits in the world. The region manifests several caves with varities of gypsum crystals (Ca4 H2O) known as selenite (the largest in the world so far, specimens up to eleven meters in length and one meter in thickness). The present abstract discusses the formation mechanism of these gigantic crystals. The review is based on the interpretations made by early workers (which includes one doctorate thesis and two Bulletins). The interpretations were made on 19 samples of anhydrites that were collected at a depth of -345 meters. At this depth the early workers also found microscopically alternating dark dolomite and light bands of anhydrite. The dolomite-anhydrite association is generally associated with mineral recrystallization events. With the geological review carried out, two sources of sulfates were identified: one is La Virgen Formation and the second in the stratiform anhydrite of the Aurora Formation. Formation of hydrothermal anhydrite during the last stage of mineralization has been attributed to the formation of selenite mega crystals due to its dissolution. -
Naica Mine M E X I
Cave of the Crystals grade 5 Revise / Sketch NEW ARIZONA MEXICO magine yourself one thousand feet underground, drilling a new tunnel in an old zinc and lead mine. I TEXAS Suddenly your drill bursts through the MEXICO rock wall. What you see takes your CHIHUAHUA breath away. Huge crystals fill a cave SONORA from end to end, floor to ceiling. They Chihuahua shimmer like moonlight. But before you can explore the cave, you are Naica Mine hit with air as hot as a blast from a furnace. Two mineworkers, Juan and Pedro Sanchez, discovered this amazing “Cave of the Crystals” in 2000 at the Naica Mine in the state of Chihuahua, The Cave of the Crystals is located in Mexico. They didn’t stay long, for the intenseSue heat Carlson 609 971 6828 the desert of northern drove them away. Mexico. The mine owners put an iron door at the mouth of the cave. Scientists came to study the cave, but because of the heat, they could stay inside for only a few minutes at a time. 28 5_RNLESE865836_U6SA27.indd 28 5/10/2012 6:28:25 AM Inside Mexico’s Cave of the Crystals Cave of the Crystals grade 5 Revise / Sketch Scientists found the crystals were made of selenite gypsum, a translucent, light-colored mineral. The cave had just the NEW right combination of minerals, water, and ARIZONA MEXICO temperature to grow the crystals. The cave had once been filled with water, and heat from the earth’s core kept the water at TEXAS MEXICO about 136 degrees Fahrenheit. -
Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
minerals Review Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico Iván Jalil Antón Carreño-Márquez 1 , Isaí Castillo-Sandoval 2, Bernardo Enrique Pérez-Cázares 3, Luis Edmundo Fuentes-Cobas 2 , Hilda Esperanza Esparza-Ponce 2 , Esperanza Menéndez-Méndez 4, María Elena Fuentes-Montero 3 and María Elena Montero-Cabrera 2,* 1 Department of Engineering, Universidad La Salle Chihuahua, Chihuahua 31625, Mexico; [email protected] 2 Department of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, Mexico; [email protected] (I.C.-S.); [email protected] (L.E.F.-C.); [email protected] (H.E.E.-P.) 3 Department of Computational Chemistry, Universidad Autónoma de Chihuahua, Chihuahua 31125, Mexico; [email protected] (B.E.P.-C.); [email protected] (M.E.F.-M.) 4 Department Physicochemical Assays, Instituto Eduardo Torroja de Ciencias de la Construcción, 28033 Madrid, Spain; [email protected] * Correspondence: [email protected] Abstract: Calcium sulfate (CaSO4) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO4·2H2O), bassanite (CaSO4·0.5H2O), soluble Citation: Carreño-Márquez, I.J.A.; anhydrite, and insoluble anhydrite (CaSO4), being the key difference the hydration state of the Castillo-Sandoval, I.; Pérez-Cázares, sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate B.E.; Fuentes-Cobas, L.E.; Esparza- thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow Ponce, H.E.; Menéndez-Méndez, E.; up to 11–12 m long. -
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology By Charles J. Taylor and Earl A. Greene Chapter 3 of Field Techniques for Estimating Water Fluxes Between Surface Water and Ground Water Edited by Donald O. Rosenberry and James W. LaBaugh Techniques and Methods 4–D2 U.S. Department of the Interior U.S. Geological Survey Contents Introduction...................................................................................................................................................75 Hydrogeologic Characteristics of Karst ..........................................................................................77 Conduits and Springs .........................................................................................................................77 Karst Recharge....................................................................................................................................80 Karst Drainage Basins .......................................................................................................................81 Hydrogeologic Characterization ...............................................................................................................82 Area of the Karst Drainage Basin ....................................................................................................82 Allogenic Recharge and Conduit Carrying Capacity ....................................................................83 Matrix and Fracture System Hydraulic Conductivity ....................................................................83 -
Platy Galena from the Viburnum Trend, Southeast Missouri
Missouri University of Science and Technology Scholars' Mine Geosciences and Geological and Petroleum Geosciences and Geological and Petroleum Engineering Faculty Research & Creative Works Engineering 01 Mar 2018 Platy Galena from the Viburnum Trend, Southeast Missouri: Character, Mine Distribution, Paragenetic Position, Trace Element Content, Nature of Twinning, and Conditions of Formation Richard D. Hagni Missouri University of Science and Technology, [email protected] Follow this and additional works at: https://scholarsmine.mst.edu/geosci_geo_peteng_facwork Part of the Geology Commons Recommended Citation R. D. Hagni, "Platy Galena from the Viburnum Trend, Southeast Missouri: Character, Mine Distribution, Paragenetic Position, Trace Element Content, Nature of Twinning, and Conditions of Formation," Minerals, vol. 8, no. 3, MDPI, Mar 2018. The definitive version is available at https://doi.org/10.3390/min8030093 This work is licensed under a Creative Commons Attribution 4.0 License. This Article - Journal is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in Geosciences and Geological and Petroleum Engineering Faculty Research & Creative Works by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. minerals Article Platy Galena from the Viburnum Trend, Southeast Missouri: Character, Mine Distribution, Paragenetic Position, Trace Element Content, Nature of Twinning, and Conditions of Formation Richard D. Hagni Department of Geological Sciences and Geological and Petroleum Engineering, Missouri University of Science and Technology, Rolla, MO 65401, USA; [email protected] Received: 15 December 2017; Accepted: 23 February 2018; Published: 2 March 2018 Abstract: The Viburnum Trend of southeast Missouri is one of the world’s largest producers of lead. -
GPS/Tachymetry) and GIS
Ecological Assessment of Springs and Spring Brooks in the Swiss National Park: Combining Fieldwork with Geodesy (GPS/Tachymetry) and GIS Diploma Thesis by Michael Döring Written at the Swiss Federal Institute for Environmental Science and Technology (EAWAG) Supervised by Dr. Urs Uehlinger PD Dr. Christopher T. Robinson (EAWAG, Switzerland) Diploma Professor: Prof. Dr. Thomas Schmitt (Ruhr Universität Bochum, Germany) Table of contents Table of contents I SUMMARY......................................................................................................................1 II ZUSAMMENFASSUNG ................................................................................................3 1 INTRODUCTION...........................................................................................................5 1.1 HISTORY .......................................................................................................................5 1.2 STUDIES ON SPRINGS.....................................................................................................5 1.3 ECOLOGY OF SPRINGS ...................................................................................................6 1.4 OBJECTIVES OF THE STUDY ...........................................................................................8 2 DESCRIPTION OF THE STUDY AREA ....................................................................9 2.1 GEOGRAPHICAL SITUATION ..........................................................................................9 2.2 SWISS NATIONAL -
Drainage Structures and Transit-Time Distributions in Conduit-Dominated
Drainage structures and transit-time distributions in conduit-dominated and fissured karst aquifer systems Zur Erlangung des akademischen Grades einer DOKTORIN DER NATURWISSENSCHAFTEN von der Fakultät für Bauingenieur-, Geo- und Umweltwissenschaften des Karlsruher Instituts für Technologie (KIT) genehmigte DISSERTATION von Dipl.-Geol. Ute Lauber aus Dachau Tag der mündlichen Prüfung: 21.11.2014 Referent: Prof. Dr. Nico Goldscheider Korreferent: Prof. Dr. Tim Bechtel Karlsruhe 2014 Abstract Abstract Abstract Karst aquifers are widely distributed across the world and are important groundwater resources. Solutionally-enlarged conduits embedded in fissured rock matrix result in a highly heterogene- ous underground drainage pattern that makes karst aquifers difficult to characterize. To ensure sustainable protection and management of karst water resources, hydrogeologic knowledge of karst systems is required. However, the quantitative characterization of groundwater flow in karst systems remains a major challenge. Specific investigating techniques and approaches are needed to account for the complexity of drainage. This thesis emphasizes the identification of drainage structures and the quantification of related transit-time distributions and hydraulic pa- rameters. To account for the strong heterogeneities of different types of catchment areas, three diverse karst aquifer systems are investigated: a conduit-dominated karst system, a fissured karst system and an aquifer system that comprises a karst and a porous-media (alluvial/rockfall) aquifer. For a detailed hydrogeologic assessment of the different catchment areas, adapted methods applied include a combination of artificial tracer tests, natural tracer analysis, and dis- charge analysis. The first two parts of this thesis describe a conduit-dominated karst system, the catchment area of the Blautopf (Swabian Alb, Germany). -
Are the Naica Giant Crystals Deteriorating Because of Human Action? M
PROCEEDINGS PAPER Are the Naica giant crystals deteriorating because of human action? M. E. Montero-Cabrera ,1,a) I. J. A. Carreño-Márquez,1 I. Castillo-Sandoval,1 B. Pérez-Cázares,2 L. E. Fuentes-Cobas,1 H. E. Esparza-Ponce,1 E. Menéndez-Méndez,3 M. E. Fuentes-Montero,2 H. Castillo-Michel,4 D. Eichert,5 R. Loredo-Portales,6 J. Canche-Tello,1 M. Y. Luna-Porres,1 G. González-Sánchez,1 D. Burciaga-Valencia,1 C. Caraveo-Castro,1 G. Gómez-Méndez,2 L. Muñoz-Castellanos,2 and I. Reyes-Cortes2 1Centro de Investigación en Materiales Avanzados (CIMAV), Chihuahua 31136, Mexico 2Universidad Autónoma de Chihuahua, Chihuahua 31125, Mexico 3Instituto Eduardo Torroja de Ciencias de la Construcción, Madrid 28033, Spain 4European Synchrotron Radiation Facility, Grenoble Cedex 9 38043, France 5Elettra Sincrotrone Trieste S.C.p.A., AREA Science Park, Basovizza (Trieste) 34149, Italy 6Universidad Nacional Autónoma de México, Hermosillo 83000, Mexico (Received 11 November 2019; accepted 14 April 2020) The giant gypsum crystals of Naica cave have fascinated scientists since their discovery in 2000. Human activity has changed the microclimate inside the cave, making scientists wonder about the potential environmental impact on the crystals. Over the last 9 years, we have studied approximately 70 samples. This paper reports on the detailed chemical–structural characterization of the impurities present at the surface of these crystals and the experimental simulations of their potential deterioration patterns. Selected samples were studied by petrography, optical and electronic microscopy, and lab- oratory X-ray diffraction. 2D grazing incidence X-ray diffraction, X-ray μ-fluorescence, and X-ray μ-absorption near-edge structure were used to identify the impurities and their associated phases.