January 2010 Issue
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 -
Grade 11 Informational Mini-Assessment Stalagmite Trio This Grade 11 Mini-Assessment Is Based on Two Texts and an Accompanying Video About Cave Formations
Grade 11 Informational Mini-Assessment Stalagmite Trio This grade 11 mini-assessment is based on two texts and an accompanying video about cave formations. The subject matter, as well as the stimuli, allow for the testing of the Common Core State Standards (CCSS) for Literacy in Science and Technical Subjects and the Reading Standards for Informational Texts. The texts are worthy of students’ time to read, and the video adds a multimedia component to make the task a more complete and authentic representation of research. The texts meet the expectations for text complexity at grade 11. Assessments aligned to the CCSS will employ quality, complex texts such as these, and some assessments will include multimedia stimuli as demonstrated by this mini-assessment. Questions aligned to the CCSS should be worthy of students’ time to answer and therefore do not focus on minor points of the texts. Several standards may be addressed within the same question because complex texts tend to yield rich assessment questions that call for deep analysis. In this mini-assessment there are twelve questions that address the Reading Standards below. There is also one constructed response item that addresses Reading, Writing, and Language standards. We encourage educators to give students the time that they need to read closely and write to sources. Please note that this mini- assessment is likely to take at least two class periods. Note for teachers of English Language Learners (ELLs): This assessment is designed to measure students’ ability to read and write in English. Therefore, educators will not see the level of scaffolding typically used in instructional materials to support ELLs—these would interfere with the ability to understand their mastery of these skills. -
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: an Annotated Bibliography by R
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: An Annotated Bibliography by R. Lee Hadden Topographic Engineering Center November 2005 US Army Corps of Engineers 7701 Telegraph Road Alexandria, VA 22315-3864 Adits, Caves, Karizi-Qanats, and Tunnels In Afghanistan Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing this collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE 30-11- 2. REPORT TYPE Bibliography 3. DATES COVERED 1830-2005 2005 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER “Adits, Caves, Karizi-Qanats and Tunnels 5b. GRANT NUMBER In Afghanistan: An Annotated Bibliography” 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER HADDEN, Robert Lee 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT US Army Corps of Engineers 7701 Telegraph Road Topographic Alexandria, VA 22315- Engineering Center 3864 9.ATTN SPONSORING CEERD / MONITORINGTO I AGENCY NAME(S) AND ADDRESS(ES) 10. -
Abseil: Descent of a Rope. Active Cave / Streamway: Cave Passage with a Flowing Stream
Caving terms (more detailed) Abseil: Descent of a rope. Active cave / streamway: Cave passage with a flowing stream. Aven: A vertical shaft as seen from below. Bed: Horizontal band of limestone. Bedding plane: Weakness or gap between beds. Belay: A fixed point to attach rope. Also describes the act of controlling a rope attached to another caver to prevent a fall. Boulder choke: Fallen rocks obscuring a passage. Calcite: A form of calcium carbonate that is the main mineral from which cave formations are made. Cavern: A very large cave chamber. Crawl: A cave passage with a low roof that necessitates crawling. Curtain: A sheet-shaped stalactite. Decorations: Another term for cave formations. Duck: Place where the cave roof almost reaches a water surface. Flowstone: Calcite formations resembling a frozen waterfall. Formations: Features such as stalactites and stalagmites formed by the deposition of calcite. Also called speleothems. Helictites: Stalactites that grow in convoluted shapes Jumar: A device used to ascend a rope. Also termed an ascender. Karst: A descriptive term for typical limestone landscapes. Pitch: A vertical shaft requiring a ladder or rope to descend. Pothole: A vertical cave. Rift: A cave passage formed at a fault. Shakehole: A surface depression resulting from the collapse of soil and rock. underneath. May indicate the presence of a cave beneath. Shaft: A vertical cave pitch. A shaft that opens to the ground surface is also called a pothole. Sink / Swallow hole / Swallet: Where surface water enters the ground. Speleothem: Another term for a cave formation such as a stalactite. SRT: Abbreviation for Single Rope Technique where a caver uses a rope to access vertical pitches in a cave rather than a wire ladder. -
Underwater Speleology Journal of the Cave Diving Section of the National Speleological Society
Underwater Speleology Journal of the Cave Diving Section of the National Speleological Society INSIDE THIS ISSUE: Possible Explanations For The Lack Of Formations In Underwater Caves In FLA The Challenge At Challenge Cave Diving Science Visit with A Cave: Cannonball Cow Springs Clean Up Volume 41 Number 1 January/February/March 2014 Underwater Speleology NSS-CDS Volume 41 Number 1 BOARD OF DIRECTORS January/February/March 2014 CHAIRMAN contents Joe Citelli (954) 646-5446 [email protected] Featured Articles VICE CHAIRMAN Tony Flaris (904) 210-4550 Possible Explanations For The Lack Of Formations In Underwater Caves In FLA [email protected] By Dr. Jason Gulley and Dr. Jason Polk............................................................................6 TREASURER The Challenge At Challenge Terri Simpson By Jim Wyatt.................................................................................................................8 (954) 275-9787 [email protected] Cave Diving Science SECRETARY By Peter Buzzacott..........................................................................................................10 TJ Muller Visit With A Cave: Cannonball [email protected] By Doug Rorex.................................................................................................................16 PROGRAM DIRECTORS Book Review: Classic Darksite Diving: Cave Diving Sites of Britain and Europe David Jones By Bill Mixon..............................................................................................................24 -
Exploration/Survey in Whigpistle Cave System Patricia Kambesis Cave Research Foundation, [email protected]
Western Kentucky University TopSCHOLAR® Mammoth Cave Research Symposia 10th Research Symposium 2013 Feb 15th, 10:45 AM The akM ing of a Connection: Exploration/Survey in Whigpistle Cave System Patricia Kambesis Cave Research Foundation, [email protected] Joel Despain Cave Research Foundation Chris Groves Hoff am n Environmental Research Institute, Western Kentucky University Follow this and additional works at: http://digitalcommons.wku.edu/mc_reserch_symp Part of the Animal Sciences Commons, Forest Sciences Commons, Geology Commons, Hydrology Commons, Other Earth Sciences Commons, and the Plant Sciences Commons Recommended Citation Patricia Kambesis, Joel Despain, and Chris Groves, "The akM ing of a Connection: Exploration/Survey in Whigpistle Cave System" (February 15, 2013). Mammoth Cave Research Symposia. Paper 8. http://digitalcommons.wku.edu/mc_reserch_symp/10th_Research_Symposium_2013/Day_two/8 This is brought to you for free and open access by TopSCHOLAR®. It has been accepted for inclusion in Mammoth Cave Research Symposia by an authorized administrator of TopSCHOLAR®. For more information, please contact [email protected]. The Making of a Connection – The Potential of a Mammoth Cave System-Whigpistle Cave Connection 1 1 2 Patricia Kambesis , Joel Despain , Chris Groves 1 Cave Research Foundation 2 Hoff man Environmental Research Institute, Western Kentucky University Abstract The current length of the Flint Ridge-Mammoth Cave System (to be called Mammoth Cave System for the rest of this paper) has been attained by a series of connections instigated by cave explorers/mappers of the Cave Research Foundation (CRF) and Central Kentucky Karst Coalition (CKKC). Between 1961 and 2011, connections have expanded the surveyed extent of the cave system to its current “offi cial” length of 390 miles (650 km). -
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. -
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. -
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. -
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico)
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico) by Stephen Alexander Daire A Thesis Presented to the Faculty of the USC Graduate School University of Southern California In Partial Fulfillment of the Requirements for the Degree Master of Science (Geographic Information Science and Technology) May 2019 Copyright © 2019 by Stephen Daire “History is just a 25,000-year dash from the trees to the starship; and while it’s going on its wild and woolly but it’s only like that, and then you’re in the starship.” – Terence McKenna. Table of Contents List of Figures ................................................................................................................................ iv List of Tables ................................................................................................................................. xi Acknowledgements ....................................................................................................................... xii List of Abbreviations ................................................................................................................... xiii Abstract ........................................................................................................................................ xvi Chapter 1 Planetary Sciences, Cave Survey, & Human Evolution................................................. 1 1.1. Topic & Area of Interest: Exploration & Survey ....................................................................12 -
Appendix 4-K Preliminary Assessment of Open Pit Slope Instability Due to the Mitchell Block Cave
APPENDIX 4-K PRELIMINARY ASSESSMENT OF OPEN PIT SLOPE INSTABILITY DUE TO THE MITCHELL BLOCK CAVE TM SEABRIDGE GOLD INC. KSM PRELIMINARY FEASIBILITY STUDY UPDATE PRELIMINARY ASSESSMENT OF OPEN PIT SLOPE INSTABILITY DUE TO THE MITCHELL BLOCK CAVE FINAL PROJECT NO: 0638-013-31 DISTRIBUTION: DATE: December 24, 2012 SEABRIDGE: 2 copies DOCUMENT NO: KSM12-26 BGC: 2 copies R.2.7.6 #500-1045 Howe Street Vancouver, B.C. Canada V6Z 2A9 Tel: 604.684.5900 Fax: 604.684.5909 December 24, 2012 Project No: 0638-013-31 Mr. T. Jim Smolik, Pre-Feasibility Study Manager Seabridge Gold Inc. 108 Front Street East Toronto, Ontario, M5A 1E1 Dear Mr. Smolik, Re: Preliminary Assessment of Open Pit Slope Instability due to the Mitchell Block Cave – FINAL Please find attached the above referenced report. Thank you for the opportunity to work on this interesting project. Should you have any questions or comments, please do not hesitate to contact the undersigned. Yours sincerely, BGC ENGINEERING INC. per: Derek Kinakin, M.Sc., P.Geo. (BC) Senior Engineering Geologist Seabridge Gold Inc., KSM Preliminary Feasibility Study Update December 24, 2012 Preliminary Assessment of Open Pit Slope Instability due to the Mitchell Block Cave FINAL Project No: 0638-013-31 EXECUTIVE SUMMARY The Mitchell Zone is the largest of the four exploration targets comprising Seabridge Gold Inc.’s KSM Project and is the only zone where a combination of open pit and block caving mining methods is proposed. The open pit will be mined with ultimate north and south wall heights reaching approximately 1,200 m. -
Airborne Microorganisms in Lascaux Cave (France) Pedro M
International Journal of Speleology 43 (3) 295-303 Tampa, FL (USA) September 2014 Available online at scholarcommons.usf.edu/ijs/ & www.ijs.speleo.it International Journal of Speleology Off icial Journal of Union Internationale de Spéléologie Airborne microorganisms in Lascaux Cave (France) Pedro M. Martin-Sanchez1, Valme Jurado1, Estefania Porca1, Fabiola Bastian2, Delphine Lacanette3, Claude Alabouvette2, and Cesareo Saiz-Jimenez1* 1Instituto de Recursos Naturales y Agrobiología de Sevilla, IRNAS-CSIC, Apartado 1052, 41080 Sevilla, Spain 2UMR INRA-Université de Bourgogne, Microbiologie du Sol et de l’Environnement, BP 86510, 21065 Dijon Cedex, France 3Université de Bordeaux, I2M, UMR 5295, 16 Avenue Pey-Berland, 33600 Pessac, France Abstract: Lascaux Cave in France contains valuable Palaeolithic paintings. The importance of the paintings, one of the finest examples of European rock art paintings, was recognized shortly after their discovery in 1940. In the 60’s of the past century the cave received a huge number of visitors and suffered a microbial crisis due to the impact of massive tourism and the previous adaptation works carried out to facilitate visits. In 1963, the cave was closed due to the damage produced by visitors’ breath, lighting and algal growth on the paintings. In 2001, an outbreak of the fungus Fusarium solani covered the walls and sediments. Later, black stains, produced by the growth of the fungus Ochroconis lascauxensis, appeared on the walls. In 2006, the extensive black stains constituted the third major microbial crisis. In an attempt to know the dispersion of microorganisms inside the cave, aerobiological and microclimate studies were carried out in two different seasons, when a climate system for preventing condensation of water vapor on the walls was active (September 2010) or inactive (February 2010).