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Karst Geology
National Park Service Mammoth Cave U.S. Department of the Interior Mammoth Cave National Park Karst Geology Look Beneath Beneath the surface of South Central Kentucky lies a world characterized by miles of dark, seemingly endless passageways. The geological processes which formed this world referred to as Mammoth Cave began hundreds of millions of years ago and continue today. The Ancient World 350 million years ago the North American continent About 280 million years ago the sea level started to was located much closer to the equator. A shallow fall exposing the layers of limestone and sandstone. sea covered most of the southeastern United States, Additional tectonic forces caused the earth’s crust and its warm water supported a dense population of to slowly rise causing cracks to form in and between tiny organisms whose shells were made of calcium the limestone and sandstone formations. As the up- carbonate (CaCO3). As these creatures died, their lift continued, rivers developed which over millions shells accumulated by the billions on the sea fl oor. of years have created the sandstone-capped plateau In addition, calcium carbonate can precipitate from above the Green River and the low, almost fl at lime- the water itself. The build-up of material continued stone plain which extends southeast of I-65. for 70 million years accumulating seven hundred feet of limestone and shale followed by sixty feet of sandstone that was deposited over much of the area by a large river system fl owing into the sea from the north. “Acid Rain” Rain water, acidifi ed by carbon dioxide in the soil water, they enlarged faster. -
Canyons & Caves
CANYONS & CAVES A Newsletter from the Resource Management Offices Carlsbad Caverns National Park Issue No. 10 Fall 1998 HISTORIC ITEMS – Items of a historical nature continue to be moved around in Lower Cave and Slaughter Canyon Cave. Preserving America’s Natural and When items are moved, they are taken out of Cultural Heritage for future generations! context and information concerning their placement is lost. Moving an item also impacts the item and the cave floor. Please DO NOT move any historic item found in any cave. WELCOME to Steven Bekedam, a new SCA for Surface Edited by Dale L. Pate Resources. Steven EOD’s Oct. 1. TABLE OF CONTENTS WHAT’S HAPPENING IN SURFACE RESOURCES • Mountain Lion Transects begin again in October. The Resource News 1 dates for the transects are in the Calendar of Events. The Mystery of the Scattered Pearls 2 Contact David Roemer, ext. 373, if you’d like to Identifying Wetlands at Rattlesnake Springs 3 participate. Barite “Stalactites” in Lechuguilla 3 • The week of October 5 begins the field work to delineate Banner-tailed Kangaroo Rat 4 the active and historic wetlands boundaries at Rattlesnake Black-tailed Rattlesnake 4 Springs (see write up) Helictites and Subaqueous Helictites 5 • Renée Beymer and Diane Dobos-Bubno will attend two And the Times, They are a Change’n 5 back-to-back conferences in Albuquerque this November: Yes, We Have Algae 6 one focuses on vegetation management and one on Calendar of Events 8 riparian habitat and water use issues. RESOURCE NEWS CAVE RESOURCES VOLUNTEERS – Adios and thanks to Gosia Roemer and Jed Holmes for all the hard work they did SPRING AND SUMMER WEATHER – Hot and dry this summer. -
Journal of Cave and Karst Studies
September 2019 Volume 81, Number 3 JOURNAL OF ISSN 1090-6924 A Publication of the National CAVE AND KARST Speleological Society STUDIES DEDICATED TO THE ADVANCEMENT OF SCIENCE, EDUCATION, EXPLORATION, AND CONSERVATION Published By BOARD OF EDITORS The National Speleological Society Anthropology George Crothers http://caves.org/pub/journal University of Kentucky Lexington, KY Office [email protected] 6001 Pulaski Pike NW Huntsville, AL 35810 USA Conservation-Life Sciences Julian J. Lewis & Salisa L. Lewis Tel:256-852-1300 Lewis & Associates, LLC. [email protected] Borden, IN [email protected] Editor-in-Chief Earth Sciences Benjamin Schwartz Malcolm S. Field Texas State University National Center of Environmental San Marcos, TX Assessment (8623P) [email protected] Office of Research and Development U.S. Environmental Protection Agency Leslie A. North 1200 Pennsylvania Avenue NW Western Kentucky University Bowling Green, KY Washington, DC 20460-0001 [email protected] 703-347-8601 Voice 703-347-8692 Fax [email protected] Mario Parise University Aldo Moro Production Editor Bari, Italy [email protected] Scott A. Engel Knoxville, TN Carol Wicks 225-281-3914 Louisiana State University [email protected] Baton Rouge, LA [email protected] Journal Copy Editor Exploration Linda Starr Paul Burger Albuquerque, NM National Park Service Eagle River, Alaska [email protected] Microbiology Kathleen H. Lavoie State University of New York Plattsburgh, NY [email protected] Paleontology Greg McDonald National Park Service Fort Collins, CO The Journal of Cave and Karst Studies , ISSN 1090-6924, CPM [email protected] Number #40065056, is a multi-disciplinary, refereed journal pub- lished four times a year by the National Speleological Society. -
Geologic Resources Inventory Report, Wind Cave National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Wind Cave National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/087 THIS PAGE: Calcite Rafts record former water levels at the Deep End a remote pool discovered in January 2009. ON THE COVER: On the Candlelight Tour Route in Wind Cave boxwork protrudes from the ceiling in the Council Chamber. NPS Photos: cover photo by Dan Austin, inside photo by Even Blackstock Wind Cave National Park Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/087 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 March 2009 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. -
From Cave to Cave
FROM CAVE TO CAVE Nature, culture, hospitality. For the trip of a lifetime exploring the wonderful cave network of the Adriatic region. Hidden treasures waiting to be discovered. 1 FROM CAVE TO Far from the surface, a world apart. CAVE Deep underground, shrouded in darkness, mysterious places wait to be discovered. A real adventure leading to the exploration of amazing caves, approaching the beauties of the underground world with the support of experienced and passionate local guides. INDEX A broad choice of cave tours along the countries facing the Adriatic Sea. Tour packages ...........p.4 Different countries, different languages, Create your own different caves all linked together by a European international tour! .... p.18 Project: the Interreg ADRION — Adriaticaves. A unique opportunity to take an “underground” journey that will open you up to amazing geological formations and life-forms incredibly adapted to live in these dark environments. A real caving experience will allow you to discover these extremely fragile environments 1 Cavallone Cave Hrvatska and their importance using a respectful 2 Praje Cave 3 Serbia Onferno Cave Bosnia and and sustainable approach. 6 Herzegovina 5 8 4 Tanaccia Cave 4 7 A plunge into the cave world you will never forget. 3 5 Re Tiberio Cave Italy Montenegro 6 Cerovac Cave 9 10 7 2 Bijambare Cave 1 8 Kadjenica Cave Albania 9 Lipa Cave 10 Shpella e Kaurit, caves of Shkoder Region 2 3 ENTE PARCO NAZIONALE DELLA MAJELLA Via Occidentale, 6 66016 Guardiagrele – Italy [email protected] www.parcomajella.it MAJELLA NATIONAL PARK - ITALY Mountains in the Majella National Park are mainly made of limestone, witnessing a fasci- nating geological history started at least 140 million years ago in an environment like the present-day Bahamas Sea. -
Geology of Caves Geology of Caves by W
U.S. Department of the Interior / U.S. Geological Survey Geology of Caves Geology of Caves by W. E. Davies and I. M. Morgan A cave is a natural opening in the ground extending beyond the zone of light and large enough to permit the entry of man. Occurring in a wide variety of rock types and caused by widely differing geological proc esses, caves range in size from single small rooms to intercorinecting passages many miles long. The scientific study of caves is called speleology (from the Greek words spelaion for cave and logos for study). It is a composite science based on geology, hydrology, biology, and archaeology, and thus holds special interest for earth scientists of the U.S. Geological Survey. Caves have been natural attractions since prehistoric times. Prolific evidence of early man's interest has been discovered in caves scattered throughout the world. Fragments of skeletons of some of the earliest manlike creatures (Australopithecines) have been discovered in cave deposits in South Africa, and the first evidence of primitive Neander thal Man was found in a cave in the Meander Valley of Germany. Cro-Magnon Man created his remarkable murals on the walls of caves in southern France and northern Spain where he took refuge more than 10,000 years ago during the chill of the ice age. Interest in caves has not dwindled. Although firm figures for cave visitors are not available, in 1974 about 1.5 million people toured Mammoth Cave in Kentucky, and more than 670,000 visited Carlsbad Caverns in New Mexico, two of the most famous caves in the United States. -
Cavern Geology Lesson Plan 1
Thank you to the Sierra Nevada Recreation Corporation: Moaning Cavern, Black Chasm Cavern and California Cavern for permission to use their classroom lesson plan material. Cavern Geology Lesson 1: What is a Cavern? OBJECTIVE Students will learn to identify the different types of caves. BACKGROUND INFORMATION Cave or Cavern? Is there a difference between a cave and a cavern? This is a frequently asked question, and many people use the terms interchangeably. However, there is a difference. A cave is any cavity in the ground that is large enough that some portion of it will not receive direct sunlight. There are many types of caves (discussed in this lesson plan). A cavern is a specific type of cave, naturally formed in soluble rock with the ability to grow speleothems. So, although a cavern can accurately be called a cave (since it is a type of cave), all caves cannot be called caverns. Caves Caves can be classified into two main categories known as primary and secondary. This classification is based on their origin. Primary caves are developed as the host rock is solidifying. Examples of primary caves include lava tubes and coral caves (descriptions follow). Secondary caves are carved out of the host rock after it has been deposited or consolidated. Most caves fall in the secondary category. However, some primary caves may later be enlarged by the forces associated with secondary cave development. Listed here are the main types of caves, and how they are formed: Coral Caves When colonies of coral in shallow water expand and unite, they form lacy or bulbous walls around an open area. -
Chapter 4: Water and Cave Sculptures
Chapter 4: Water and Cave Sculptures Jenny and Carlos felt refreshed from their lunch another bat colony, but no small shapes were hidden break in the Bateteria. They scrambled up a pile of between the rocks. Some of the stalactites looked like loose slippery boulders. At the top, an entrance took soda straws. They were white and hollow, and water them into another cave room. dripped down from their tips. Jenny moved the flashlight beam about the room. “We should call these soda straw stalactites,” she said “Look!” she said. Instead of boulders, this room was to Carlos. Bat agreed. That’s exactly what the cave crowded with those pointy-shaped stone tree stumps explorers call them. that looked like soft ice cream. Only this room was “Bat, what do you mean the stalactites ‘grow’?” asked like a forest of the strange rocks. “It’s like a museum Carlos, looking at a big stalagmite in front of him. of weird sculptures.” “These are rocks, not plants.” Icicle-shaped rocks hung from the ceiling. On the They grow, but they’re not alive like a plant or animal. cave walls, the rocks rippled and draped like curtains. They get bigger really slowly. In fact, that stalagmite Here and there flower-like crystals grew, while others in front of you probably took ten thousand years to get stuck out like strange spirals of funnel cake you buy at that big. Just a teeny bit every year. the fair. “It’s magic,” Carlos said. “I’ve never seen anything like this.” “How do they grow if they’re not alive?” Carlos wondered. -
Karst Landscape and Caves of Southeast Alaska a Resource for Teachers the Karst LANDSCAPE and Caves Of
Table of contents PART 1: Karst Landscapes and Caves Overview and fundamentals . 4 Illustrated record of life forms . 5 Geology . 6 Hydrology . 11 Physical Geography . 13 Cave Biology . 15 Paleontology and Archaeology . 21 Safety in the Caves . 28 Conservation in the Caves . 31 Map of El Capitan Cave . 36 Bibliography . 37 Glossary . 39 Map of Karst Areas in Southeast Alaska . 44 Educational Activities . 46-67 PART 2: Paleontology El Capitan Management Acknowledgments Plan . 68-116 Geological Time Scale . 118 for the First Edition Map of fossils finds Many people made indispensable contributions to this guide . in the region . 119 Scientists Jim Baichtal, John Autrey and Terry Fifield of U.S.D.A. Forest Top 12 Fossils of Service contributed text and reviewed material . Southeast Robert Wangerin and Risa Carlson wrote significant portions of the text, as did Marcel LaPerriere and Connie LaPerriere . Alaska . 120-131 Ward Serrill provided photographs of scenes inside and outside the caves . Skip Fabry and Robert Price contributed to the activities section . Robert Wetherell provided information about protection of El Capitan Cave . Valerie Steward and Jan Bush contributed to the text and Stephen Roguski to the glossary . The Klawock Parent-Teacher-Student Association aided the original educational project . 2 U.S.D.A. Forest Service Tongass National Forest IntroductIon This resource guide was prepared for middle- Project Underground is also a good school and secondary-school teachers as a source of information on caves and karst source of information and ideas about the caves landscapes . Their contacts: and karst lands of Southeast Alaska . We include Project Underground in the binder a map depicting the karst lands and 8 Radford St . -
Δ13c of Cave Speleothems Located in Kentucky And
δ13 C OF CAVE SPELEOTHEMS LOCATED IN KENTUCKY AND OHIO, U.S.A.: IMPLICATION FOR PALEOVEGETATION AND PALEOCLIMATE STUDIES Brett Alan Miller A Thesis Submitted to the Graduate College Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May 2008 Committee: Dr. Joe Elkins, Advisor Dr. John Farver Dr. Jeff Snyder ii ABSTRACT Joe T. Elkins, Advisor Calcium carbonate δ13C values of actively growing/actively dripping speleothems have been evaluated for comparison to the range predicted for modern vegetation. Some geochemical 13 models suggest that speleothem calcium carbonate δ C values from caves under C3 surface 13 vegetation should exhibit δ C values predicted for C3 vegetation; however, several field studies have shown that this relationship is unreliable. In this research, δ13C values were measured on speleothem, soil and bedrock samples in various caves in Ohio and Kentucky. These caves include: Crooked Creek Ice Cave, Floyd Mullins Cave, Great Salt Peter Cave, Hard Baker Cave, and Pine Hill Cave located in Rockcastle Co., KY; Seneca Caverns and Perry’s Cave in Seneca and Erie Counties, Ohio respectively. Soil organic matter δ13C values closely matched the range 13 for C3 vegetation with three samples demonstrating slight enrichment. Speleothem δ C values were not consistent with the published predicted values. The modern speleothems collected at the various caves indicate a large δ13C variability ranging from -11.34‰ to -2.96‰ VPDB. The percentage of measured speleothem δ13C values not agreeing with published predictions ranges from 20% to 80% depending on which predicted values are used. -
Bulletin of the Geological Society of Greece
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Documentation Centre - EKT journals Bulletin of the Geological Society of Greece Vol. 47, 2013 Contribution to the evolution of the Perama Cave (Ioannina, NW Greece). Ifandi E. University of Patras, Department of Geology, Section of Earth Materials, 265 00, Patras, Greece Tsikouras B. 1University of Patras, Department of Geology, Section of Earth Materials, 265 00, Patras, Greece & University of Brunei Darussalam, Department of Petroleum Geoscience, Jalan Tungku Link, Gadong BE1410, Bandar Seri Begawan, Brunei Darussalam Hatzipanagiotou K. University of Patras, Department of Geology, Section of Earth Materials, 265 00, Patras, Greece https://doi.org/10.12681/bgsg.10939 Copyright © 2016 E. Ifandi, B. Tsikouras, K. Hatzipanagiotou To cite this article: Ifandi, E., Tsikouras, B., & Hatzipanagiotou, K. (2013). Contribution to the evolution of the Perama Cave (Ioannina, NW Greece).. Bulletin of the Geological Society of Greece, 47(1), 255-263. doi:https://doi.org/10.12681/bgsg.10939 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 07/06/2020 15:18:32 | Bulletin of the Geological Society of Greece, vol. XLVII 2013 Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τομ. XLVII , 2013 Proceedings of the 13th International Congress, Chania, Sept. Πρακτικά 13ου Διεθνούς Συνεδρίου, Χανιά, Σεπτ. 2013 2013 CONTRIBUTION TO THE EVOLUTION OF THE PERAMA CAVE (IOANNINA, NW GREECE) Ifandi E.1, Tsikouras B.1,2 and Hatzipanagiotou K.1 1University of Patras, -
Cave and Karst Program Geologic Resources Division National Park Service National Park Service U.S
Cave and Karst Program Geologic Resources Division National Park Service National Park Service U.S. Department of the Interior P.O. Box 25287 Denver, CO 80225 Stalactite www2.nature.nps.gov/grd/geology/caves/ Geologic Resources Division Caves are some of the most fragile and easily Cave And Karst Program damaged environments on earth. When you visit caves remember the motto of the National Speleological Society: “Take only pictures, kill nothing but time, and leave nothing behind.” A desert Pallid bat catches its food using echo-location in the dark of night. Lighting for photo by Stalagmite Dr. Scott Altenbach. Soda Straw The following is a partial list of National Park Service units that contain cave and karst areas. For more information about units that contain caves go to www.nps.gov Carlsbad Caverns Mammoth Cave National Park National Park Carlsbad, NM Mammoth Cave, KY (505) 785-2232 (270) 758-2328 Craters of the Moon Oregon Caves National Monument National Monument Arco, ID Cave Junction, OR (208) 527-3257 (541) 592-2100 Great Basin Russell Cave National Park National Monument Baker, NV Bridgeport, AL Column (775) 234-7331 (205) 495-2672 Jewel Cave Timpanogos Cave National Monument National Monument Custer, SD American Fork, UT (605) 673-2288 (801) 756-5239 Cave and karst areas are a rich source of yet-to-be- discovered knowledge of the world around us. The Lava Beds Wind Cave National Park Service Cave and Karst Program National Monument National Park Flowstone Tulelake, CA Hot Springs, SD emphasizes stewardship, responsibility, science, Floors (530) 667-2282 (605) 745-4600 cooperation, coordination, and education.