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Karst Features — Where and What Are They?
Karst Features — Where and What are They? This story was made with Esri's Story Map Journal. Read the interactive version on the web at https://arcg.is/jCmza. Iowa Geological and Water Survey Bureau completed a detailed mapping project of bedrock geologic units, key subsurface horizons, and surficial karst features in the Iowa portion of the Upper Iowa River Watershed in 2011. In the report, they note that “One of the primary goals of the study was to gain more thorough understanding of relationships between bedrock geology and karst features within the watershed.” Black River Falls photo courtesy of Larry Reis. Sinkholes Esri, HERE, Garmin, FAO, USGS, NGA, EPA, NPS According to the GIS data from the Iowa DNR, the UIR Watershed has 6,649 known sinkholes in the Iowa portion of the watershed. Although this number is very precise, sinkhole development is actually an active process in the UIR Watershed so the actual number of sinkholes changes over time as some are filled in through natural or human processes and others are formed. One of the most numerous karst features found in the UIR Watershed, sinkholes are formed when specific types of underlying bedrock are gradually dissolved, creating voids in the subsurface. When soils and other materials above these voids can no longer bridge the gap created in the bedrock, a collapse occurs. Photo Courtesy of USGS Sinkholes vary in size and shape and can and do occur in any type of land use in the UIR Watershed, from row crop to forest, and even in roads. According to the Iowa Geologic Survey, sinkholes are often connected to underground bedrock fractures and conduits, from minor fissures to enlarged caverns, which allow for rapid movement of water from sinkholes vertically and laterally through the subsurface. -
Pleistocene Panthera Leo Spelaea
Quaternaire, 22, (2), 2011, p. 105-127 PLEISTOCENE PANTHERA LEO SPELAEA (GOLDFUSS 1810) REMAINS FROM THE BALVE CAVE (NW GERMANY) – A CAVE BEAR, HYENA DEN AND MIDDLE PALAEOLITHIC HUMAN CAVE – AND REVIEW OF THE SAUERLAND KARST LION CAVE SITES n Cajus G. DIEDRICH 1 ABSTRACT Pleistocene remains of Panthera leo spelaea (Goldfuss 1810) from Balve Cave (Sauerland Karst, NW-Germany), one of the most famous Middle Palaeolithic Neandertalian cave sites in Europe, and also a hyena and cave bear den, belong to the most im- portant felid sites of the Sauerland Karst. The stratigraphy, macrofaunal assemblages and Palaeolithic stone artefacts range from the final Saalian (late Middle Pleistocene, Acheulean) over the Middle Palaeolithic (Micoquian/Mousterian), and to the final Palaeolithic (Magdalénien) of the Weichselian (Upper Pleistocene). Most lion bones from Balve Cave can be identified as early to middle Upper Pleistocene in age. From this cave, a relatively large amount of hyena remains, and many chewed, and punctured herbivorous and carnivorous bones, especially those of woolly rhinoceros, indicate periodic den use of Crocuta crocuta spelaea. In addition to those of the Balve Cave, nearly all lion remains in the Sauerland Karst caves were found in hyena den bone assemblages, except those described here material from the Keppler Cave cave bear den. Late Pleistocene spotted hyenas imported most probably Panthera leo spelaea body parts, or scavenged on lion carcasses in caves, a suggestion which is supported by comparisons with other cave sites in the Sauerland Karst. The complex taphonomic situation of lion remains in hyena den bone assemblages and cave bear dens seem to have resulted from antagonistic hyena-lion conflicts and cave bear hunting by lions in caves, in which all cases lions may sometimes have been killed and finally consumed by hyenas. -
Late Pleistocene Panthera Leo Spelaea (Goldfuss, 1810) Skeletons
Late Pleistocene Panthera leo spelaea (Goldfuss, 1810) skeletons from the Czech Republic (central Europe); their pathological cranial features and injuries resulting from intraspecific fights, conflicts with hyenas, and attacks on cave bears CAJUS G. DIEDRICH The world’s first mounted “skeletons” of the Late Pleistocene Panthera leo spelaea (Goldfuss, 1810) from the Sloup Cave hyena and cave bear den in the Moravian Karst (Czech Republic, central Europe) are compilations that have used bones from several different individuals. These skeletons are described and compared with the most complete known skeleton in Europe from a single individual, a lioness skeleton from the hyena den site at the Srbsko Chlum-Komín Cave in the Bohemian Karst (Czech Republic). Pathological features such as rib fractures and brain-case damage in these specimens, and also in other skulls from the Zoolithen Cave (Germany) that were used for comparison, are indicative of intraspecific fights, fights with Ice Age spotted hyenas, and possibly also of fights with cave bears. In contrast, other skulls from the Perick and Zoolithen caves in Germany and the Urșilor Cave in Romania exhibit post mortem damage in the form of bites and fractures probably caused either by hyena scavenging or by lion cannibalism. In the Srbsko Chlum-Komín Cave a young and brain-damaged lioness appears to have died (or possibly been killed by hyenas) within the hyena prey-storage den. In the cave bear dominated bone-rich Sloup and Zoolithen caves of central Europe it appears that lions may have actively hunted cave bears, mainly during their hibernation. Bears may have occasionally injured or even killed predating lions, but in contrast to hyenas, the bears were herbivorous and so did not feed on the lion car- casses. -
Research Article Extinctions of Late Ice Age Cave Bears As a Result of Climate/Habitat Change and Large Carnivore Lion/Hyena/Wolf Predation Stress in Europe
Hindawi Publishing Corporation ISRN Zoology Volume 2013, Article ID 138319, 25 pages http://dx.doi.org/10.1155/2013/138319 Research Article Extinctions of Late Ice Age Cave Bears as a Result of Climate/Habitat Change and Large Carnivore Lion/Hyena/Wolf Predation Stress in Europe Cajus G. Diedrich Paleologic, Private Research Institute, Petra Bezruce 96, CZ-26751 Zdice, Czech Republic Correspondence should be addressed to Cajus G. Diedrich; [email protected] Received 16 September 2012; Accepted 5 October 2012 Academic Editors: L. Kaczmarek and C.-F. Weng Copyright © 2013 Cajus G. Diedrich. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Predation onto cave bears (especially cubs) took place mainly by lion Panthera leo spelaea (Goldfuss),asnocturnalhuntersdeep in the dark caves in hibernation areas. Several cave bear vertebral columns in Sophie’s Cave have large carnivore bite damages. Different cave bear bones are chewed or punctured. Those lets reconstruct carcass decomposition and feeding technique caused only/mainlybyIceAgespottedhyenasCrocuta crocuta spelaea, which are the only of all three predators that crushed finally the long bones. Both large top predators left large tooth puncture marks on the inner side of cave bear vertebral columns, presumably a result of feeding first on their intestines/inner organs. Cave bear hibernation areas, also demonstrated in the Sophie’s Cave, were far from the cave entrances, carefully chosen for protection against the large predators. The predation stress must have increased on the last and larger cave bear populations of U. -
I Subsurface Waste Disposal by Means of Wells a Selective Annotated Bibliography
I Subsurface Waste Disposal By Means of Wells A Selective Annotated Bibliography By DONALD R. RIMA, EDITH B. CHASE, and BEVERLY M. MYERS GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2020 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS G. B. MORTON, Secretary GEOLOGICAL SURVEY W. A. Radlinski, Acting Director Library of Congress catalog-card No. 77-179486 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.50 (paper cover) Stock Number 2401-1229 FOREWORD Subsurface waste disposal or injection is looked upon by many waste managers as an economically attractive alternative to providing the sometimes costly surface treatment that would otherwise be required by modern pollution-control law. The impetus for subsurface injection is the apparent success of the petroleum industry over the past several decades in the use of injection wells to dispose of large quantities of oil-field brines. This experience coupled with the oversimplification and glowing generalities with which the injection capabilities of the subsurface have been described in the technical and commercial literature have led to a growing acceptance of deep wells as a means of "getting rid of" the ever-increasing quantities of wastes. As the volume and diversity of wastes entering the subsurface continues to grow, the risk of serious damage to the environment is certain to increase. Admittedly, injecting liquid wastes deep beneath the land surface is a potential means for alleviating some forms of surface pollution. But in view of the wide range in the character and concentrations of wastes from our industrialized society and the equally diverse geologic and hydrologic con ditions to be found in the subsurface, injection cannot be accepted as a universal panacea to resolve all variants of the waste-disposal problem. -
Groundwater Issues in the Paleozoic Plateau a Taste of Karst, a Modicum of Geology, and a Whole Lot of Scenery
GGroundwaterroundwater IssuesIssues inin tthehe PaleozoicPaleozoic PlateauPlateau A Taste of Karst, a Modicum of Geology, and a Whole Lot of Scenery Iowa Groundwater Association Field Trip Guidebook No. 1 Iowa Geological and Water Survey Guidebook Series No. 27 Dunning Spring, near Decorah in Winneshiek County, Iowa September 29, 2008 In Conjunction with the 53rd Annual Midwest Ground Water Conference Grand River Center, Dubuque, Iowa, September 30 – October 2, 2008 Groundwater Issues in the Paleozoic Plateau A Taste of Karst, a Modicum of Geology, and a Whole Lot of Scenery Iowa Groundwater Association Field Trip Guidebook No. 1 Iowa Geological and Water Survey Guidebook Series No. 27 In Conjunction with the 53rd Annual Midwest Ground Water Conference Grand River Center, Dubuque, Iowa, September 30 – October 2, 2008 With contributions by M.K. Anderson Robert McKay Iowa DNR-Water Supply Engineering Iowa DNR-Geological and Water Survey Bruce Blair Jeff Myrom Iowa DNR-Forestry Iowa DNR-Solid Waste Michael Bounk Eric O’Brien Iowa DNR-Geological and Water Survey Iowa DNR-Geological and Water Survey Karen Osterkamp Lora Friest Iowa DNR-Fisheries Northeast Iowa Resource Conservation and Development Jean C. Prior Iowa DNR-Geological and Water Survey James Hedges Luther College James Ranum Natural Resources Conservation Service John Hogeman Winneshiek County Landfi ll Operator Robert Rowden Iowa DNR-Geological and Water Survey Claire Hruby Iowa DNR-Geographic Information Systems Joe Sanfi lippo Iowa DNR-Manchester Field Offi ce Bill Kalishek Gary Siegwarth Iowa DNR-Fisheries Iowa DNR-Fisheries George E. Knudson Mary Skopec Luther College Iowa DNR-Geological and Water Survey Bob Libra Stephanie Surine Iowa DNR-Geological and Water Survey Iowa DNR-Geological and Water Survey Huaibao Liu Paul VanDorpe Iowa DNR-Geological and Water Survey Iowa DNR-Geological and Water Survey Iowa Department of Natural Resources Richard Leopold, Director September 2008 CONTENTS INTRODUCTION . -
53. Jahrestagung in Herne
Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age Hugo Obermaier - Gesellschaft für Erforschung des Eiszeitalters und der Steinzeit e.V. 53. Jahrestagung in Herne 26. – 30. April 2011 in Kooperation mit dem Bibliographische Information der Deutschen Nationalbibliothek: Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliographie, detail- lierte bibliographische Angaben sind im Internet über http://dnb.d-nb.de abrufbar. Für den Inhalt der Seiten sind die Autoren selbst verantwortlich. © 2011 Hugo Obermaier – Gesellschaft für Erforschung des Eiszeitalters und der Steinzeit e.V. c/o Institut für Ur- und Frühgeschichte der Universität Erlangen-Nürnberg Kochstr. 4/18 D-91054 Erlangen Alle Rechte vorbehalten. Jegliche Vervielfältigung einschließlich fotomechanischer und digitalisierter Wieder- gabe nur mit ausdrücklicher Genehmigung der Herausgeber und des Verlages. Redaktion, Satz & Layout: Leif Steguweit (Schriftführer der HOG); Frontcover: Trittsiegel eines Höhlenlöwen aus Bottrop, ca. 35.000 Jahre alt (Zeichnung nach W. von Koenigswald 1995) Stadtwappen von Herne (Quelle: Wikimedia) Druck: PrintCom oHG, Erlangen-Tennenlohe ISBN: 978-3-933474-75-9 Inhalt (Content) Programmübersicht (Brief program) 5 Programm (Meeting program) 6 Kurzfassungen der Vorträge und Poster (Abstracts of Reports and Posters) 13 Exkursionsbeiträge (Excursion´s Guide) 54 An outline of the geology and geomorphology of the Twente region 55 Das sauerländische Höhlenland im südlichen Westfalen (Einführung) 71 Blätterhöhle bei Hagen (J. Orschiedt) 75 Feldhofhöhle bei Balve im Hönnetal (M. Baales) 77 Balver Höhle – größter Höhlenraum des Hönnetals (M. Baales) 79 Die letzten Rentierjäger im Sauerland: Der „Hohle Stein“ bei Kallenhardt (M. 83 Baales) Bericht zur 52. Tagung der Gesellschaft in Leipzig 87 Teilnehmerliste (List of Participants) 95 Weitere Informationen: http://www.uf.uni-erlangen.de/obermaier/obermaier.html Programm der 53. -
Pleistocene Cave Hyenas in the Iberian Peninsula: New Insights from Los Aprendices Cave (Moncayo, Zaragoza)
Palaeontologia Electronica palaeo-electronica.org Pleistocene cave hyenas in the Iberian Peninsula: New insights from Los Aprendices cave (Moncayo, Zaragoza) Víctor Sauqué, Raquel Rabal-Garcés, Joan Madurell-Malaperia, Mario Gisbert, Samuel Zamora, Trinidad de Torres, José Eugenio Ortiz, and Gloria Cuenca-Bescós ABSTRACT A new Pleistocene paleontological site, Los Aprendices, located in the northwest- ern part of the Iberian Peninsula in the area of the Moncayo (Zaragoza) is presented. The layer with fossil remains has been dated by amino acid racemization to 143.8 ± 38.9 ka (earliest Late Pleistocene or latest Middle Pleistocene). Five mammal species have been identified in the assemblage: Crocuta spelaea (Goldfuss, 1823) Capra pyre- naica (Schinz, 1838), Lagomorpha indet, Arvicolidae indet and Galemys pyrenaicus (Geoffroy, 1811). The remains of C. spelaea represent a mostly complete skeleton in anatomical semi-connection. The hyena specimen represents the most complete skel- eton ever recovered in Iberia and one of the most complete remains in Europe. It has been compared anatomically and biometrically with both European cave hyenas and extant spotted hyenas. In addition, a taphonomic study has been carried out in order to understand the origin and preservation of these exceptional remains. The results sug- gest rapid burial with few scavenging modifications putatively produced by a medium sized carnivore. A review of the Pleistocene Iberian record of Crocuta spp. has been carried out, enabling us to establish one of the earliest records of C. spelaea in the recently discovered Los Aprendices cave, and also showing that the most extensive geographical distribution of this species occurred during the Late Pleistocene (MIS4- 2). -
55Th Legislature - State of New Mexico - First Session, 2021
1 HOUSE MEMORIAL 12 2 55TH LEGISLATURE - STATE OF NEW MEXICO - FIRST SESSION, 2021 3 INTRODUCED BY 4 Cathrynn N. Brown and Gail Armstrong 5 6 7 8 9 10 A MEMORIAL 11 REQUESTING THE GOVERNOR TO ISSUE A PROCLAMATION RECOGNIZING 12 2021 AS THE "INTERNATIONAL YEAR OF CAVES AND KARST". 13 14 WHEREAS, caves and related landforms like sinkholes, 15 springs and sinking streams, collectively known as karst, 16 present some of the world's most dramatic landscapes; and 17 WHEREAS, caves and karst have diverse economic, ecologic, 18 scientific and cultural impacts around New Mexico, the United ] = delete = ] 19 States and the world; and 20 WHEREAS, Carlsbad Caverns national park alone has an 21 economic benefit of about thirty-four million dollars 22 ($34,000,000) each year for New Mexico; and 23 WHEREAS, other New Mexico cave tourist destinations 24 include Bottomless Lakes state park, Santa Rosa blue hole, the underscored material = new = material underscored material [bracketed 25 ice cave and Bandera volcano and El Malpais national monument; .219712.1 1 and 2 WHEREAS, the country's first underground wilderness was 3 established in New Mexico to protect the spectacular 4 Lechuguilla cave; and 5 WHEREAS, the country's first underground national 6 conservation area was established in New Mexico to protect the 7 equally amazing Fort Stanton-Snowy River Cave national 8 conservation area; and 9 WHEREAS, the primary water supplies for roughly fifteen 10 percent of New Mexico are karst aquifers, especially supporting 11 the communities in the southeast -
Beneath the Forest" Is a Biannual Newsletter Published by the Forest Service of the U.S
Volume 6, Issue 2 Fall 2013 “Beneath the Forest" is a biannual newsletter published by the Forest Service of the U.S. Department of Agriculture. Edited by Johanna L. Kovarik, Minerals and Geology Management Centralized National Operations Inside this Issue…and more Page Sandy Glacier Cave Project: Mt. Hood, Oregon 3 MOU between the National Cave and Karst Research Institute and the Forest Service 8 C-23: New Discoveries in an Old Cave 10 Battle for Bats: New White-Nose Syndrome video available 16 Beneath the Forest 1 Editor’s Notes: CAVE AND KARST CALENDAR OF EVENTS I am pleased to present our 11th issue of Beneath the Forest, the U.S. Forest Service cave and karst ------------------------------------------------------------------------------- newsletter, published twice a year in the spring and in the fall. We welcome contributions from stakeholders and volunteers as well as forest employees. Karst Interest Group Meeting Tuesday April 28 - 30 2014 Our next issue will be the spring issue in May of 2014. Carlsbad, New Mexico Articles for the Spring 2014 issue are due on April 1st, 2014, in order for the issue to be out in May 2014. Please encourage resource managers, cavers, karst scientists, and —————————————————— other speleological enthusiasts who do work on your for- est to submit articles for the next exciting issue! International Workshop on Ice Caves Cover art: The Entrance of Snow Dragon Glacier Cave on Mt. Hood at sunset. Image: Brent MacGregor Photography August 17 - 22 2014 Idaho Falls, Idaho Contributors and Entities represented -
Structural and Lithological Influences on the Tony Grove Alpine Karst
Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-2016 Structural and Lithological Influences on the onyT Grove Alpine Karst System, Bear River Range, North-Central Utah Kirsten Bahr Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Geology Commons Recommended Citation Bahr, Kirsten, "Structural and Lithological Influences on the onyT Grove Alpine Karst System, Bear River Range, North-Central Utah" (2016). All Graduate Theses and Dissertations. 5015. https://digitalcommons.usu.edu/etd/5015 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. STRUCTURAL AND LITHOLOGICAL INFLUENCES ON THE TONY GROVE ALPINE KARST SYSTEM, BEAR RIVER RANGE, NORTH-CENTRAL UTAH by Kirsten Bahr A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geology Approved: ______________________________ ______________________________ W. David Liddell, Ph.D. Robert Q. Oaks, Jr, Ph.D. Major Professor Committee Member ______________________________ ______________________________ Thomas E. Lachmar, Ph.D. Mark R. McLellan, Ph.D. Committee Member Vice President for Research and Dean of the School of Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 2016 ii Copyright © Kirsten Bahr 2016 All Rights Reserved iii ABSTRACT Structural and Lithological Influences on the Tony Grove Alpine Karst System, Bear River Range, North-Central Utah by Kirsten Bahr, Master of Science Utah State University, 2016 Major Professor: Dr. W. -
Terminology Used in Caving
Cave and Karst Terminology by J. N. Jennings with additions by others Copyright © Australian Speleological Federation. This document may be freely copied provided that this copyright notice remains with the document. Copyright Notices and References First published in ASF Newsletter 83 (1979) Replaces list in Speleo Handbook (1968) As published in Australian Karst Index 1985 Amended by Max Meth and Arthur Clarke Additions by Rauleigh Webb 1995, 1996. Abbreviations and Conventions Abb. = abbreviation Syn. = synonym (word with same meaning) Cf. = confer (compare) with the following term which is not identical but related to it. (n.) = noun (v.) = verb A word in brackets in the left-hand column is commonly used in conjunction with the preceding word without altering the meaning. Square brackets enclose statements not part of the definition but for special reasons included in the list. ABNEY LEVEL A type of clinometer with a bubble tube used in cave survey to determine vertical angles. ACTIVE CAVE A cave which has a stream flowing in it. Cf. live cave. ADAPTATION An inherited characteristic of an organism in structure, function or behaviour which makes it better able to survive and reproduce in a particular environment. Lengthening of appendages, loss of pigment and modification of eyes are considered adaptations to the dark zone of caves. ACETYLENE An inflammable hydrocarbon gas, C2H2, produced by water reacting with calcium carbide. When burnt, yields carbon dioxide as well as light. AGGRESSIVE Referring to water which is still capable of dissolving more limestone, other karst rock, or speleothems. ACCIDENTAL (n.) An animal accidentally living in a cave.