World Heritage Caves and Karst: a Thematic Study
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Reviews of the Genera Schaefferia Absolon, 1900, Deuteraphorura
TAR Terrestrial Arthropod Reviews 5 (2012) 35–85 brill.nl/tar Reviews of the genera Schaefferia Absolon, 1900, Deuteraphorura Absolon, 1901, Plutomurus Yosii, 1956 and the Anurida Laboulbène, 1865 species group without eyes, with the description of four new species of cave springtails (Collembola) from Krubera-Voronya cave, Arabika Massif, Abkhazia Rafael Jordana1, Enrique Baquero1*, Sofía Reboleira2 and Alberto Sendra3 1Department of Zoology and Ecology, University of Navarra, 31080 Pamplona, Spain e-mails: [email protected]; [email protected] *Corresponding author. 2Department of Biology, Universidade de Aveiro and CESAM Campus Universitário de Santiago, 3810-193 Aveiro, Portugal e-mail: [email protected] 3Museu Valencià d’Història Natural (Fundación Entomológica Torres Sala) Paseo de la Pechina 15. 46008 Valencia, Spain e-mail: [email protected] Received on November 4, 2011. Accepted on November 21, 2011 Summary Krubera-Voronya cave and other deep systems in Arabika Massif are being explored during many speleological expeditions. A recent Ibero-Russian exploration expedition (summer of 2010) took place in this cave with the aim of providing a study of the biocenosis of the deepest known cave in the world. Four new species of Collembola were found at different depths: Schaefferia profundissima n. sp., Anurida stereoodorata n. sp., Deuteraphorura kruberaensis n. sp., and Plutomurus ortobalaganensis n. sp., the last one at -1980 m deep. The identification and description of the new species have required the careful study of all congeneric species, implying a revision of each genus. As a result of this work tables and keys to all significant characters for each species are presented. -
Caving: Safety Activity Checkpoints
Caving: Safety Activity Checkpoints Caving—also called “spelunking” (speh-LUNK-ing) is an exciting, hands-on way to learn about speleology (spee-lee-AH- luh-gee), the study of caves, in addition to paleontology (pay-lee-en-TAH-luh-gee), the study of life from past geologic periods by examining plant and animal fossils. As a sport, caving is similar to rock climbing, and often involves using ropes to crawl and climb through cavern nooks and crannies. These checkpoints do not apply to groups taking trips to tourist or commercial caves, which often include safety features such as paths, electric lights, and stairways. Girl Scout Daisies and Brownies do not participate in caving. Know where to go caving. Connect with your Girl Scout council for site suggestions. Also, the National Speleological Society provides an online search tool for U.S. caving clubs, and the National Park Service provides information about National Park caves. Include girls with disabilities. Communicate with girls with disabilities and/or their caregivers to assess any needs and accommodations. Learn more about the resources and information that the National Center on Accessibility and the National Center of Physical Activities and Disabilities provide to people with disabilities. Caving Gear Basic Gear Sturdy boots with ankle protection (hiking boots for dry areas; rubber boots or wellies for wet caves) Warm, rubber gloves (to keep hands warm and protect against cuts and abrasions) Nonperishable, high-energy foods such as fruits and nuts Water Specialized Gear -
Atlas of American Orthodox Christian Monasteries
Atlas of American Orthodox Christian Monasteries Atlas of Whether used as a scholarly introduction into Eastern Christian monasticism or researcher’s directory or a travel guide, Alexei Krindatch brings together a fascinating collection of articles, facts, and statistics to comprehensively describe Orthodox Christian Monasteries in the United States. The careful examina- Atlas of American Orthodox tion of the key features of Orthodox monasteries provides solid academic frame for this book. With enticing verbal and photographic renderings, twenty-three Orthodox monastic communities scattered throughout the United States are brought to life for the reader. This is an essential book for anyone seeking to sample, explore or just better understand Orthodox Christian monastic life. Christian Monasteries Scott Thumma, Ph.D. Director Hartford Institute for Religion Research A truly delightful insight into Orthodox monasticism in the United States. The chapters on the history and tradition of Orthodox monasticism are carefully written to provide the reader with a solid theological understanding. They are then followed by a very human and personal description of the individual US Orthodox monasteries. A good resource for scholars, but also an excellent ‘tour guide’ for those seeking a more personal and intimate experience of monasticism. Thomas Gaunt, S.J., Ph.D. Executive Director Center for Applied Research in the Apostolate (CARA) This is a fascinating and comprehensive guide to a small but important sector of American religious life. Whether you want to know about the history and theology of Orthodox monasticism or you just want to know what to expect if you visit, the stories, maps, and directories here are invaluable. -
By Jocelyn Cranefield
Expository Text by Jocelyn Cranefield PAIRED READ Why Bat Flies at Night STRATEGIES & SKILLS Comprehension Content Standards Strategy: Ask and Answer Science Questions Life Science Skill: Cause and Effect Vocabulary adaptations, agile, caches, dormant, forage, frigid, hibernate, insulate Word Count: 1,434** Photography Credit: MICHAEL NICHOLS/National Geographic Creative **The total word count is based on words in the running text and headings only. Numerals and words in captions, labels, diagrams, charts, and sidebars are not included. mheducation.com/prek-12 Copyright © 2014 McGraw-Hill Education All rights reserved. No part of this publication may be reproduced or distributed in any form or by any means, or stored in a database or retrieval system, without the prior written consent of McGraw-Hill Education, including, but not limited to, network storage or transmission, or broadcast for distance learning. Send all inquiries to: McGraw-Hill Education Two Penn Plaza New York, New York 10121 ISBN: 978-0-02-119233-5 MHID: 0-02-119233-2 Printed in the United States of America. 11 12 13 14 15 QVS 22 21 20 19 18 E Genre Expository Text Essential Question How are living things adapted to their environment? by Jocelyn Cranefield Introduction ................................ 2 Chapter 1 From the Entrance to the Twilight Zone ..... 4 Chapter 2 Dark and Surprising Places ................. 10 Conclusion.................................. 16 Respond to Reading ........................ 18 PAIRED READ Why Bat Flies at Night ........... 19 Glossary ................................... 22 Index ...................................... 23 Focus on Science ................. 24 Introduction Caves are found all over the world. They often go a long way in from the entrance and go deep below Earth’s surface. -
Tentative Lists Submitted by States Parties As of 15 April 2021, in Conformity with the Operational Guidelines
World Heritage 44 COM WHC/21/44.COM/8A Paris, 4 June 2021 Original: English UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION CONVENTION CONCERNING THE PROTECTION OF THE WORLD CULTURAL AND NATURAL HERITAGE WORLD HERITAGE COMMITTEE Extended forty-fourth session Fuzhou (China) / Online meeting 16 – 31 July 2021 Item 8 of the Provisional Agenda: Establishment of the World Heritage List and of the List of World Heritage in Danger 8A. Tentative Lists submitted by States Parties as of 15 April 2021, in conformity with the Operational Guidelines SUMMARY This document presents the Tentative Lists of all States Parties submitted in conformity with the Operational Guidelines as of 15 April 2021. • Annex 1 presents a full list of States Parties indicating the date of the most recent Tentative List submission. • Annex 2 presents new Tentative Lists (or additions to Tentative Lists) submitted by States Parties since 16 April 2019. • Annex 3 presents a list of all sites included in the Tentative Lists of the States Parties to the Convention, in alphabetical order. Draft Decision: 44 COM 8A, see point II I. EXAMINATION OF TENTATIVE LISTS 1. The World Heritage Convention provides that each State Party to the Convention shall submit to the World Heritage Committee an inventory of the cultural and natural sites situated within its territory, which it considers suitable for inscription on the World Heritage List, and which it intends to nominate during the following five to ten years. Over the years, the Committee has repeatedly confirmed the importance of these Lists, also known as Tentative Lists, for planning purposes, comparative analyses of nominations and for facilitating the undertaking of global and thematic studies. -
NSS Conservation and Preservation Policies ( .Pdf )
Part 2-Conservation, Management, Ethics: NSS Conservation and Preservation Policies 253 Section C-Improving Caver Ethics NSS Conservation and Preservation Policies NSS Cave Conservation Policy The National Speleological Society believes: Caves have unique scientific, recreational, and scenic values. These values are endangered by both carelessness and intentional vandalism. These values, once gone, cannot be recovered. The responsibility for protecting caves must be assumed by those who study and enjoy them. Accordingly, the intention of the Society is to work for the preservation of caves with a realistic policy supported by effective programs for: Encouraging self-discipline among cavers. Education and research concerning the causes and prevention of cave damage. Special projects, including cooperation with other groups similarly dedicated to the conservation of natural areas. Specifically: All contents of a cave-formations, life, and loose deposits-are significant for their enjoyment and interpretation. Caving parties should leave a cave as they find it. Cavers should provide means for the removal of waste. Cavers should limit marking to a few, small, removable signs as needed for surveys. Cavers should especially exercise extreme care not to accidentally break or soil formations, disturb life forms, or unnecessarily increase the number of disfiguring paths through an area. Scientific collection is professional, selective, al)d minimal. The collecting of mineral or biological material for display purposes-including previ- ously broken or dead specimens-is never justified, as it encourages others to collect and destroy the interest of the cave. The Society encourages projects such as: Establishing cave preserves. Placing entrance gates where appropriate. Opposing the sale of speleothems. -
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. -
Casleguard Cave 2005
Castleguard Cave 2005 First ascent of the 200-foot aven Text by Marek Vokáˇc Photos by Christian Rushfeldt, Bjørn Myrvold, Jørn Halvorsen, Marek Vokáˇc First edition October 27, 2006 Copyright notice: Overall copyright © 2006 Marek Vokáˇc. Photographers retain their copy- right © to individual images as specified in photo credits/captions. Permission is generally granted for individual, non-commercial use of this report, provided due credit is given. Parks Canada is additionally granted permission for other non-commercial use and distribution. Author contact: Marek Vokáˇc Thorleifs Allé 5c 0489 Oslo Norway email: [email protected] Telephone: +47 934 92 857 Cover photo: Marek Vokáˇcclimbing the aven, by Christian Rushfeldt (CC05-064) Dedicated to all whose generous support made this trip possible, and a success: my wife and children; the team; their families; and our colleagues and employers Introduction Castleguard Cave lies in the heart of the Rocky Mountains, close to the Saskatchewan Glacier. To get to the cave from Calgary, one drives the beautiful Icefields Parkway, past Lake Louise and Banff, preferably staying at the Saksatchewan Crossing hotel. Getting to the cave entrance is a full-day ski trip. The cave itself was known early in the 1900’s, and was visited by tourists with horses and mules. The biggest attraction were the sudden floods coming out of the entrance, where the dry opening would change into a roaring river in a few seconds. Modern cave exploration started in 1967, during the summer. The explorers were caught by a sudden rise in the water and trapped inside the first drop. After 18 hours the water level dropped enough for them to get out; soon after that, the waters rose again and ran for weeks. -
Museum of Natural History & Science Interpretation Guide for the Cavern
Museum of Natural History & Science Interpretation Guide for The Cavern A cave is a naturally occurring hole in the ground large enough to be explored by humans. Caves can be found on every continent in the world. Caves, along with the objects found within them, are extremely fragile and take millions of years to form. They are home to unique organisms—many of which are still unknown to science; they are archaeological sites that preserve our cultural heritage; and geologic laboratories that demonstrate how water can both dissolve and deposit rock. Caves are a vital and non-renewable resource that must be conserved and protected. The Cavern is a recreation of a Kentucky limestone dissolution cave. It is the largest artificial cave in the United States—and some say the world—containing 535 feet of passage in an area 44 feet wide, 24 feet high and 64 feet long. Parts of the cave were modeled after two caves in Kentucky: Teamers Cave in Rockcastle County and Dyches Bridge Cave in Pulaski County. By modeling our cavern after these two caves, our dissolution cave has a realistic appearance. A dissolution cave is by far the most common type of cave. They can be found throughout the world if the right conditions present themselves. The formation of a dissolution cave requires four basic elements: rock, water, carbon dioxide and time. • Rock, especially carbonate rocks, such as limestone, is the first ingredient. These types of rocks were formed hundreds of millions of years ago. It is in the seas surrounding the continents that limestone is formed. -
Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada
Arctic and Alpine Research ISSN: 0004-0851 (Print) 2325-5153 (Online) Journal homepage: https://www.tandfonline.com/loi/uaar19 Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada T. C. Atkinson To cite this article: T. C. Atkinson (1983) Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada, Arctic and Alpine Research, 15:4, 523-536 To link to this article: https://doi.org/10.1080/00040851.1983.12004379 Copyright 1983 Regents of the University of Colorado Published online: 01 Jun 2018. Submit your article to this journal Article views: 64 View related articles Citing articles: 4 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=uaar20 Arctic and Alpine Research, Vol. 15, No.4, 1983, pp. 523-536 GROWTH MECHANISMS OF SPELEOTHEMS IN CASTLEGUARD CAVE, COLUMBIA ICEFIELDS, ALBERTA, CANADA* T. C. ATKINSON School ofEnvironmental Sciences, University ofEast Anglia, Norwich NR4 7TJ, England, U.K. ABSTRACT In spite of its location beneath high alpine terrain and active glaciers, Castleguard Cave contains many actively growing calcite'speleothems. Four hypotheses as to their growth mechanism were tested against field data on water chemistry, temperatures, CO 2 content of cave air, and evaporation rates. The hypotheses were (1) that a biogenic source of high PC02 is unlikely, so calcite deposition by CO 2 degassing would require a nonbiogenic source; (2) warming of water after entering the cave, or in passage through the rocks above it might cause calcite supersaturation; (3) calcite might be deposited because of evaporation of seep age; and (4) waters dissolving several Ca-bearing minerals might precipitate calcite as the least soluble by the common-ion effect. -
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada Derek Ford, PGeo., PhD, FRSC. Emeritus Professor of Geography and Earth Sciences, McMaster University [email protected] For: Environment and Natural Resources, Government of the Northwest Territories August 2009 (i) Executive Summary The Goal of this Report is to Produce Maps of the Known and Potential Karst Landform Sites in the Northwest Territories (NWT) Karst landforms are those created by the dissolution of comparatively soluble rocks and the routing of the water (from rain or snowmelt) underground via caves rather than at the surface in river channels. The principal karst rocks are salt (so soluble that it is scarcely seen at the surface in the NWT), gypsum and anhydrite (solubility around 2500 mg/l of water), and limestone and dolomite (solubility around 250 -350 mg/l). All of these rock types are common and widespread amongst the sedimentary strata in the NWT. Surface karst landforms include: a) karren, which are spreads of individually small solution pits, shafts, and runnels that, collectively, may cover many hectares (limestone pavements); b) sinkholes of solutional, collapse, or other origin that can be tens to hundreds of metres in diameter and proportionally as deep. Sinkholes are considered the diagnostic karst landform worldwide; c) larger topographically closed depressions that may flood or drain seasonally, poljes if flat-floored, otherwise turloughs; d) extensive dry valleys and gorges, dry because their formative waters have been captured underground. All water sinking underground via karst landforms of all sizes drain quickly in comparison with all other types of groundwater because they are able to flow through solutionally enlarged conduits, termed caves where they are of enterable size.