DOCSLIB.ORG

Texas Caver Vol.26, No.3, 1981 CONTENTS

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

the Texas Caver Vol.26, No.3, 1981 CONTENTS Three Fingers Cave Mapping Report ....... 35 Three Fingers Cave Map ................ 37 Glacier Caves in Mex ico . ..... ........... 38 Robber Baron Clean-up ............... .. 39 Caving in the Global Village ............ 40 Bits & Pieces ........... .. .............. 41 Emergency Communication Invitation ...... 41 Coon Crap Cave Map ...................... 42 Trip Reports ...................... ..... 43 The Clay Choke Cave Map ................. 44 Texas Caver Word Hunt No . 3 ........... 48 Cover Photo: George Veni crawls through a narrow passage in Inner Space. Photo by James Jasek. Contents Page Photo: Steve Boehm crosses a deep crevasse on the way to the Volcano in Inner Space. James Jasek photo. Th e TEXAS CAVER is a bimonthly publication of the Texas Speleological Association (TSA}, an internal organization of the National Speleological Society (NSS) and is published by James Jas ek in Waco, Texas. (817) 776-172 7 SUBSCRIPTIONS are $5.00 per year. Persons subscribing after the first of the y ear will receive all back issues for that y ear. Single copies are available at $1.00 each, postpaid. Th e TEXAS CAVER openly invites contributors to submit: articles, reports, news, cartoons, cave maps, caving articles, and photographs (any size print black and white or color print) for publication in the TEXAS CAVER. Address all SUBSCRIPTIONS and EDITORIAL material to the editor: James Jasek, 1019 Melrose Dr., Waco , Texas 76710. (817) 776 -1 727 Wh en sending in a change of address, please include y our old address. Persons interested in EXCHANGES or FOREIGN subscriptions should direct correspondence to the editor. THREE FINGERS CAVE Mapping Report Duwain Whitis Near the bottom of a rugged canyon in During the course of the summer, Duwain he Guadalupe Mountains of New Mexico lies worked on the data reduction only to find hree Finger Cave. Since August of 1979 the that much of the survey needed to be ggie Speleological Society of Texas A&M re-done. The errors common to most surveys niversity has been involved in the survey had become so intwined that they were f this complex cave. Discovered in 1967 impossible to isolate. In August of 1979, y Bob Sarabia and Jim Peck of Carlsbad, the first week long expedition to the cave he cave has not yet been fully explored. was mounted. This trip concentrated on lthough much has been rumored about the resurveying the area between the Bell xtent of the cave, very little work was Room and the Temple of the Fiery Cave God. one previous to 1976. It was mentioned as This trip 'rediscovered' the Z survey area n addendum to several United States deep which appeared to be almost untravelled. ave lists as being about 500 feet deep. A large portion of the 'Mid Maze' was also o survey documented the depth, however. explored. This is a portion of the cave survey was began in 1968 by several where it is possible to get lost after emb ers of the Southwestern Region, but traveling fifty feet. Stories abound of ery little of the cave was surveyed and people who have been lost in the cave for o ma p was published. The survey extended hours. One pair of Aggies got lost in the . r om the bottom of the entrance drop, maze for an hour . hrough the Meador Pincher, and down the In November of 1979, the Aggies returned resent day Z survey. to the cave at Thanksgiving. Staying in I n 1976, the Cave Research Foundation the cave for 66 hours, they concentrated :.gan a new exploration of the cave. on adding much detail to the Bell Room 'n:ough 1979, they mapped the Bell Room, Map. The Bell Room is about 400 feet long h~ Temp le of the Fiery Cave God, and Three and 100 feet wide at the widest point. It .• ng er Hall. Some surveying was done in slopes sharply from south to north and has 1:e maze below the seventy foot chimney an elevation change of almost 200 feet. ·''· i.c h drops out of the Temple. Unknowingly, The Room is filled with cemented breakdown . :te CRF teams tied some of the old SWR which forms a ridge down the length of the ~~a t ion s thinking that the tie stations chamber. Tall columns are numerous, the •2re new ones set by the CRF. During this most notable being the 'Bell Canopy' after 2riod, very little data reduction was which the room is named. Numerous holes .. ·::.·r:f ormed. Errors which would have been exist in the breakdown in the northern a.s y to detect became immersed· in other half of the room. These lead to lower areas e :: rors . of the cave, but most visitors only see I n 19 79, Jim Goodbar, who then worked as the Bell Room. Another trip in March of o cave specialist for the Bureau of Land 1980 produced the survey of the North Room :anagement in Carlsbad, was sent a copy of and the Lower Complex. The North Room is , ie data. He was asked by the project a lower extension of the Bell Room, but is Clo r dinators, Alan and Carol Hill, to see separated by breakdown. Further down is ·na t he could do with the survey. In May, the Lower Complex, a series of three large two cavers from Texas A&M University drop­ rooms which exceed the Temple of the Fiery ped in on Jim to visit. Duwain Whitis and Cave God in size. This area contains much Ba rb Vinson had just come from the moun­ virgin passage. The Caca Rojo Room only tains after doing some tourista caving, had one set of footprints on a red clay and Barb wanted to see Jim, who she knew floor. f rom caving in Mexico and who had also In May, the CRF held their annual received his degree at A&M. As a result expedition to the cave. Unfortunately , of that visit and Duwain's inquiries about only seven persons appeared, two of whom the cave, Jim agreed to send the Aggies a were Aggies. Since Carol Pill's mineralogy copy of the survey notes. work in Cottonwood Cave took precedence, 35 very little was accompl ished except for a Tom Bemis CRF surface survey to the high end of the Bell Steve Boehm ASS Room where surface organic debris has John Brooks ASS washed into the cave . A small fissure lead­ Bob Buecher CRF ing to the surface probably exists but will Debbie Buecher CRF likely be too small to make digging worth- Steve Cole ASS while (another entrance is of question- Rod Crowder CRF able desirability). The surface points Bill Davies CRF are about 25 feet above the corresponding Heather Fannin ASS point in the cave. Richard Flukerson ASS The last surveying trip to the cave was Jim Goodbar CRF made in August, 1980. The Aggies returned Scott Harden ASS once again, but this trip was less Alan Hill CRF productive than others. Another route down Carol Hill CRF to the Lower Complex was mapped, and the Larry Hill CRF Bell Room was carefully checked for other Del Holman ASS possible leads, a few of which exist. The Tracy Johnson CRF remainder of that trip was spent beginning Ann Lawson ASS a new survey of Hell Below where 2000 feet Pete Lindsley CRF was surveyed. John McLean CRF Three Fingers is a very complex cave. The Denis McQuillar CRF survey now encompasses 8340 feet of Hendrick Stokvis ASS traverse with 16 loops, 14 of which are Kevin Sullivan ASS interconnected. Because of this, and Barb Vinson ASS/CRF because of the certain continuation of the Cal Welborn CRF maze nature of the cave, the data is now Duwain Whitis ASS/CRF being processed with the aid of the computer program 'Ellipse' . This has made the Three Fingers is located on public land, silhouette profile which accompanies this is gated, and requires a permit for leg2l article possible. The profile only represents access. If you should visit the cave, the surveyed portion of the r;we. Much more exercise care to leave the cave as you cave exists and literally hundreds of found it. Also, help to prevent the suney leads are waiting to be checked. The cave markers from being destroyed. These are certainly goes deeper. The Z survey smoke dotes labelled with orange surveyors extends under a large ridge to the south flagging which will be removed when they which may be permeated with passage. Air are no longer needed. flow is detectable in many areas of the cave indicating that other entrances may exist. The next planned trip to the cave will be the annual CRF trip in May. This expedition will concentrate on exploring the maze area below the Temple of the Fiery Cave God and above the Three Fingers Ha ll . Leads in the Lower Complex and the Z survey will also be pushed. Three Fingers is only one of many pote ntia lly large caves in the Guadalupe Mountains. Many of these caves are not surveyed or completely explored, although they have been visited for many years. Most of these caves are going to require a gr eat amo unt of work and patience to explore. Three Fingers is a prime example. The following persons have participated in the present survey of Three Fingers. An £ :.;o9L-40N .1><n1; a»oM ~'"~";) SYX"'!!_L O_J_ NOI..Ln"'loS indication of the sponsoring organizations is give n for the trips attended. Elbert Bassham CRF Dave Belski CRF 36 a. a. SURFACE SURVEY a. THREE FINGERS CAVE Profile: 285° view Eddy Co.
Recommended publications
  • Bibliography

    Bibliography

    Bibliography Many books were read and researched in the compilation of Binford, L. R, 1983, Working at Archaeology. Academic Press, The Encyclopedic Dictionary of Archaeology: New York. Binford, L. R, and Binford, S. R (eds.), 1968, New Perspectives in American Museum of Natural History, 1993, The First Humans. Archaeology. Aldine, Chicago. HarperSanFrancisco, San Francisco. Braidwood, R 1.,1960, Archaeologists and What They Do. Franklin American Museum of Natural History, 1993, People of the Stone Watts, New York. Age. HarperSanFrancisco, San Francisco. Branigan, Keith (ed.), 1982, The Atlas ofArchaeology. St. Martin's, American Museum of Natural History, 1994, New World and Pacific New York. Civilizations. HarperSanFrancisco, San Francisco. Bray, w., and Tump, D., 1972, Penguin Dictionary ofArchaeology. American Museum of Natural History, 1994, Old World Civiliza­ Penguin, New York. tions. HarperSanFrancisco, San Francisco. Brennan, L., 1973, Beginner's Guide to Archaeology. Stackpole Ashmore, w., and Sharer, R. J., 1988, Discovering Our Past: A Brief Books, Harrisburg, PA. Introduction to Archaeology. Mayfield, Mountain View, CA. Broderick, M., and Morton, A. A., 1924, A Concise Dictionary of Atkinson, R J. C., 1985, Field Archaeology, 2d ed. Hyperion, New Egyptian Archaeology. Ares Publishers, Chicago. York. Brothwell, D., 1963, Digging Up Bones: The Excavation, Treatment Bacon, E. (ed.), 1976, The Great Archaeologists. Bobbs-Merrill, and Study ofHuman Skeletal Remains. British Museum, London. New York. Brothwell, D., and Higgs, E. (eds.), 1969, Science in Archaeology, Bahn, P., 1993, Collins Dictionary of Archaeology. ABC-CLIO, 2d ed. Thames and Hudson, London. Santa Barbara, CA. Budge, E. A. Wallis, 1929, The Rosetta Stone. Dover, New York. Bahn, P.
  • Beneath the Forest" Is a Biannual Newsletter Published by the Forest Service of the U.S

    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

    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

    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.
  • 227504791.Pdf

    227504791.Pdf

    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Scholar Commons | University of South Florida Research University of South Florida Scholar Commons School of Geosciences Faculty and Staff Publications School of Geosciences 2014 Searching for Cold-Adapted Microorganisms in the Underground Glacier of Scarisoara Ice Cave, Romania Alexandra Maria Hillebrand-Voiculescu Emil Racovita Institute of Speleology, [email protected] Corina Itcus Institute of Biology Bucharest Ioan Ardelean Institute of Biology Bucharest Denisa Pascu Institute of Biology Bucharest Aurel Persoiu Stefan cel Mare University See next page for additional authors Follow this and additional works at: https://scholarcommons.usf.edu/geo_facpub Part of the Earth Sciences Commons Scholar Commons Citation Hillebrand-Voiculescu, Alexandra Maria; Itcus, Corina; Ardelean, Ioan; Pascu, Denisa; Persoiu, Aurel; Rusu, Andreea; Brad, Traian; Popa, Elena; Onac, Bogdan P.; and Purcarea, Christina, "Searching for Cold-Adapted Microorganisms in the Underground Glacier of Scarisoara Ice Cave, Romania" (2014). School of Geosciences Faculty and Staff Publications. 1893. https://scholarcommons.usf.edu/geo_facpub/1893 This Article is brought to you for free and open access by the School of Geosciences at Scholar Commons. It has been accepted for inclusion in School of Geosciences Faculty and Staff Publications by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Authors Alexandra Maria
  • Human Origin Sites and the World Heritage Convention in Eurasia

    Human Origin Sites and the World Heritage Convention in Eurasia

    World Heritage papers41 HEADWORLD HERITAGES 4 Human Origin Sites and the World Heritage Convention in Eurasia VOLUME I In support of UNESCO’s 70th Anniversary Celebrations United Nations [ Cultural Organization Human Origin Sites and the World Heritage Convention in Eurasia Nuria Sanz, Editor General Coordinator of HEADS Programme on Human Evolution HEADS 4 VOLUME I Published in 2015 by the United Nations Educational, Scientific and Cultural Organization, 7, place de Fontenoy, 75352 Paris 07 SP, France and the UNESCO Office in Mexico, Presidente Masaryk 526, Polanco, Miguel Hidalgo, 11550 Ciudad de Mexico, D.F., Mexico. © UNESCO 2015 ISBN 978-92-3-100107-9 This publication is available in Open Access under the Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) license (http://creativecommons.org/licenses/by-sa/3.0/igo/). By using the content of this publication, the users accept to be bound by the terms of use of the UNESCO Open Access Repository (http://www.unesco.org/open-access/terms-use-ccbysa-en). The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Cover Photos: Top: Hohle Fels excavation. © Harry Vetter bottom (from left to right): Petroglyphs from Sikachi-Alyan rock art site.
  • Glacier Caves: a Globally Threatened Subterranean Biome

    Glacier Caves: a Globally Threatened Subterranean Biome

    Francis G. Howarth. Glacier caves: a globally threatened subterranean biome. Journal of Cave and Karst Studies, v. 83, no. 2, p. 66-70. DOI:10.4311/2019LSC0132 GLACIER CAVES: A GLOBALLY THREATENED SUBTERRANEAN BIOME Francis G. Howarth1 Abstract Caves and cave-like voids are common features within and beneath glaciers. The physical environment is harsh and extreme, and often considered barren and devoid of life. However, accumulating evidence indicates that these caves may support a diverse invertebrate fauna with species endemic to each region. As glaciers continue to disappear at an alarming rate due to global warming, they take their largely unknown fauna with them. Thus, glacier caves may harbor one of the most endangered ecosystems globally, and yet their biodiversity is among the least studied or known. Faunal surveys and ecological studies are urgently needed before all examples are lost. INTRODUCTION Glacier caves are voids within and beneath glaciers that are formed mostly by surface meltwater sinking into the glacier through crevasses, moulins, and fissures (Piccini and Mecchia, 2013; Smart, 2003; Kováč, 2018; Gulley and Fountain, 2019). Glacier caves can be enlarged by geothermal melting (Kiver and Mumma, 1971; Giggenbach, 1976), as well as by pressure and friction at the contact between the ice and bedrock. These caves are created by natural phenomena during the life of the glacier and are common features in glaciers. They are best developed in montane gla- ciers in comparison to polar glaciers, largely because of the steeper gradient, greater flow rate, and seasonally warmer temperatures (Smart, 2003). The cave structure is dynamic; for example, changing shape and course as the glacier flows downslope; enlarging during warm periods; and collapsing and deforming under pressure.
  • THE SANDY GLACIER CAVE PROJECT: the STUDY of GLACIAL RECESSION from WITHIN Eduardo L

    THE SANDY GLACIER CAVE PROJECT: the STUDY of GLACIAL RECESSION from WITHIN Eduardo L

    THE SANDY GLACIER CAVE PROJECT: THE STUDY OF GLACIAL RECESSION FROM WITHIN Eduardo L. Cartaya Brent McGregor Deschutes National Forest Deschutes National Forest 63095 Deschutes Market Road 63095 Deschutes Market Road Bend, Oregon, 97701,USA, [email protected] Bend, Oregon 97701 USA, [email protected] Abstract in the form of a crevasse. After a short rappel, the three The Sandy Glacier Cave Project is a National realized they had found the titanic cave and completed Speleological Society (NSS) sponsored study on the a grade 5 survey of the upper section, which bored unique system of glacier caves located on the Sandy over 550 meters up the mountain under the hard, blue Glacier on the western flank of Mt Hood, Oregon. While glacier ice. They named the cave Snow Dragon, after a the study primarily targets the structure, layout and common analogy to avalanche dangers. Brent and Eddy ice volume change of the ever moving cave system by returned a few weeks later with wet suits to survey the conducting annual grade 5 surveys, numerous tangential wet lower section of the cave. It travels mostly through observations and trends have been recorded that are of firn, a highly compacted, pre-glacial, form of snow that great interest to the study of glacial recession, watershed melts off in large sections during late summer. The two hydrology, micro-biology and astro-biology, as well as discovered a rushing torrent of icy water entering the the study of organic specimens and remains being thawed system from an unexplored side tube. The volume of out of the ice mass by the expanding cave.
  • Sturtz Unr 0139M 13151.Pdf

    Sturtz Unr 0139M 13151.Pdf

    University of Nevada, Reno A Natural and Cultural History of Leonard Rockshelter, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Arts in Anthropology By Sara N. Sturtz Dr. Geoffrey Smith/Thesis Advisor May, 2020 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by entitled be accepted in partial fulfillment of the requirements for the degree of Advisor Committee Member Graduate School Representative David W. Zeh, Ph.D., Dean Graduate School i ABSTRACT Leonard Rockshelter (LRS) is located in Pershing County, Nevada. Robert Heizer excavated the site in 1950 and reported more than 2 m of stratified deposits from which he recovered a modest assemblage of perishable and lithic artifacts. Of interest to the University of Nevada Reno’s Great Basin Paleoindian Research Unit (GBPRU) was Heizer’s discovery of obsidian flakes in deposits dated to 11,199±570 14C BP (14,900- 11,610 cal BP). This possibility of a stratified Pleistocene occupation prompted the GBPRU to return to LRS in 2018 and 2019 for additional work, which produced few artifacts but a sizeable small mammal assemblage. In this thesis, I test two hypotheses: (1) the small mammal assemblage provides a paleoenvironmental record that demonstrates changing local conditions during the Terminal Pleistocene and Holocene; and (2) the shelter contains evidence of human occupation dating to the Terminal Pleistocene. My results demonstrate that the Early Holocene and initial Middle Holocene were more mesic than later periods. They also suggest that people did not occupy LRS until the Early Holocene, after which time they periodically returned to the site.
  • Geomorphological Context and Formation History of Cloggs Cave

    Geomorphological Context and Formation History of Cloggs Cave

    Geomorphological context and formation history of Cloggs Cave: What was the cave like when people inhabited it? Jean-Jacques Delannoy, Bruno David, Joanna Fresløv, Russell Mullett, Helen Green, Johan Berthet, Fiona Petchey, Lee Arnold, Rachel Wood, Matthew Mcdowell, et al. To cite this version: Jean-Jacques Delannoy, Bruno David, Joanna Fresløv, Russell Mullett, Helen Green, et al.. Geo- morphological context and formation history of Cloggs Cave: What was the cave like when peo- ple inhabited it?. Journal of Archaeological Science: Reports, Elsevier, 2020, 33, pp.102461. 10.1016/j.jasrep.2020.102461. halshs-03115566 HAL Id: halshs-03115566 https://halshs.archives-ouvertes.fr/halshs-03115566 Submitted on 22 Mar 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NoDerivatives| 4.0 International License Journal of Archaeological Science: Reports 33 (2020) 102461 Contents lists available at ScienceDirect Journal of Archaeological Science: Reports journal homepage: www.elsevier.com/locate/jasrep Geomorphological context and formation history of Cloggs Cave: What was T the cave like when people inhabited it? ⁎ ⁎ Jean-Jacques Delannoya,b, , Bruno Davidb,c, , Joanna Fresløvd, Russell Mullettd, GunaiKurnai Land and Waters Aboriginal Corporationd, Helen Greenb,e, Johan Bertheta, Fiona Petcheyb,f, Lee J.
  • Early and Middle Archaic Projectile Point Technologies in the Closed Basin Area of the San Luis Valley, Colorado

    Early and Middle Archaic Projectile Point Technologies in the Closed Basin Area of the San Luis Valley, Colorado

    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2001 Early and Middle Archaic projectile point technologies in the Closed Basin area of the San Luis Valley, Colorado Scott A. Des Planques The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Des Planques, Scott A., "Early and Middle Archaic projectile point technologies in the Closed Basin area of the San Luis Valley, Colorado" (2001). Graduate Student Theses, Dissertations, & Professional Papers. 2124. https://scholarworks.umt.edu/etd/2124 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Maureen and Mike MANSFIELD LIBRARY The University of Montana Permission is granted by the author to reproduce this material in its entirety, provided that this material is used for scholarly purposes and is properly cited in published works and reports. **Please check "Yes" or "No" and provide signature** Yes, I grant permission No, I do not grant permission Author's Signature; ^ P Date: 5Z£//ol ' Any copying for commercial purposes or financial gain may be undertaken only with the author's exphcit consent. MSThcsis\Mansfjeld Library Permission THE EARLY AND MIDDLE ARCHAIC PROJECTILE POINT TECHNOLOGIES IN THE CLOSED BASIN AREA OF THE SAN LUIS VALLEY, COLORADO by Scott A.
  • Roman Hapka, Co-Président Fontaine 12 CH-2022 Bevaix Switzerland E-Mail: Hapka@Vtx.Ch

    Roman Hapka, Co-Président Fontaine 12 CH-2022 Bevaix Switzerland E-Mail: [email protected]

    UIS-BULLETIN UNION INTERNATIONALE DE SPÉLÉOLOGIE 1997 43 No. 2 _______________________ EDITED IN JULY 1997 * EDITE EN JUILLET 1996 * AUSGEGEBEN IM JULI 1997 ASSEMBLY GENERAL - Agenda ASSEMBLÉE GÉNÉRALE - Ordre du jour GENERALVERSAMMLUNG - Tagesordnung La Chaux-de-Fonds, Switzerland, Europe High School First Session-Premiére Séance - Erste Sitzung August 10, 1997, 8.30 am 1. Opening of the Assembly General - Ouverture de l'Assemblée Générale - Eröffnung der Generalversammlung 2. Ascertainment of the number of voting delegates - Constattion du nombre des délégations votantes - Feststellung der Anzahl der stimmberechtigten Delegierten 3. Salutations and thanks - Salutations et remerciements - Begrüβungen und Danksagungen 4. Approval of Minutes of the UIS Assembly General from Beijing (1993) - Approbation formale du proces-verbal de l'Assemblée Générale de l'UIS de Beijing (1993) - Approbation des Protokolls der Generalversammlung der UIS in Beijing (1993) 5. Reports concerning activities of the UIS, Commissions, Working Groups and Committees - Rapport concernant les activités de l'UIS Commissions, des Groupes de Travail et des Committées - Bericht über die Tätigkeit der UIS, der Kommissionen, der Arbeitsgruppen und der Komitees 6. Election of two auditors - Elections de deux Commissires aux Comptes - Wahl zweiter Rechnungsprüfer 7. Election of a Commission for the elections of the new UIS Bureau - Election d'une Commissison des candidatures poure le prochain Bureau - Wahl einer Kommission für die Kandidaturen fur das nächste Büro 8. Presentation of candidate countries to organize the 13th International Congress of Speleology - Présentation des candidatures pour le 13me Congrs International de Spéléologie - Vorstellung der Bewerber fur den 13. Internationaler Kongreβ für Speläologie (2001) 9. Admission of new Member Countries of the UIS - Admission de nouveaux membres de l'UIS - Aufnahme neuer Mitglieder der UIS 10.