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Nancy Hultgren Remembers.Pdf
PART III: Carlsbad Caverns National Park, New Mexico The “main focus” of our five-day trip, in the early spring of 1952, was extended time to visit two locations—Carlsbad Caverns National Park, in the southeastern part of the State of New Mexico, and Ciudad Juarez, Mexico—across the International Border from El Paso, Texas, which lies in the far western tip of Texas. A beautiful morning awaited as we rose from our beds in the small motel in the town of Carlsbad, New Mexico. Out in the parking lot, in front of our room, the Hudson was covered with a thick layer of dust, accumulated during our long drive through Colorado and New Mexico. No rain in sight to help wash the car off, but my dad pulled into a Texaco Gas Station in town to refuel, and have the attendant check the oil and clean the windshields and side windows for us. (While living in Denver, Colorado, my dad often frequented a favorite Texaco Station on Colorado Blvd., not far from our first house on Birch Street.) In a friendly tone, and looking at our license plates, which read “Colorful Colorado,” the station attendant asked, “How far have you folks come? Headed for the Caverns I bet! Any time of year is a good time to go, ya’ know! Doesn’t matter what the temperature is on the outside today, cause deep in the Caverns the temperature is the same year round—56°.” Motel Stevens in Carlsbad, New Mexico. Curt Teich vintage linen postcard. Leaving Carlsbad and the Pecos River Valley behind, my dad pointed the Hudson southwest out of town on US Hwy. -
2015 Visitor Guide Park Information and Maps
National Park Service Wind Cave National Park U.S. Department of the Interior The official newspaper Annual 2015 Visitor Guide Park Information and Maps The Best of Both Worlds What Lies Below? From Tipis to Tours Back From the Brink Wind Cave National Park is host to Wind Cave is considered sacred and Many national parks are great places one of the longest and most complex culturally significant to many American to view wildlife. However, that has caves in the world. Currently over 143 Indians, and throughout the centuries, not always been the case. In the early miles of twisting passageways reside many tribes lived and traveled within 1900s, many animal populations neared under only 1.2 square miles of surface what would become Wind Cave extinction because of loss of habitat or area, creating a maze of tunnels deep National Park. Who first discovered hunting pressures. below the park's rolling hills. The cave Wind Cave is lost to time, but in 1881, is famous for a rare formation known Tom and Jesse Bingham rediscovered as boxwork. More boxwork is found in the cave when they were attracted Welcome to Wind Cave than all other caves in the to the entrance by whistling noises Wind Cave National Park! world combined. coming out of the cave. This national park is one of the oldest in Portions of Wind Cave are believed to In 1889, the South Dakota Mining the country. Established in 1903, it was the be over 300 million years old, making Company established a mining eighth national park created and the first set it one of the oldest known caves in the claim at Wind Cave and hired J.D. -
A Conservation Focused Inventory of Subterranean Invertebrates of the Southwest Illinois Karst
Julian J. Lewis, Philip Moss, Diane Tecic, and Matthew E. Nelson - A conservation focused inventory of subterranean invertebrates of the southwest Illinois Karst. Journal of Cave and Karst Studies, v. 65, n. 1, p. 9-21. A CONSERVATION FOCUSED INVENTORY OF SUBTERRANEAN INVERTEBRATES OF THE SOUTHWESTERN ILLINOIS KARST JULIAN J. LEWIS J. Lewis and Associates, Biological Consulting, 217 W. Carter Avenue, Clarksville, IN 47129 USA PHILIP MOSS Ozark Underground Laboratory, 1572 Aley Lane, Protem, MO 65733 USA DIANE TECIC Natural Heritage Regional Administrator, 4521 Alton Commerce Parkwary, Alton, IL 62025 USA MATTHEW E. NELSON formerly The Nature Conservancy; current 7401 Placer Run, Fort Wayne, IN 46815 USA In 1998-1999 The Nature Conservancy conducted a bioinventory of caves in Monroe and St. Clair coun- ties in southwestern Illinois. This karst area comprises a small section of the Ozark Plateau isolated from the Missouri Ozarks by the Mississippi River. In the 71 sites that were sampled, 41 species thought to be globally rare were found and were assigned state (S) and global (G) ranks of rarity for conservation use. The list includes 10 species considered to be new to science and 12 species previously unreported from Illinois. Twenty four taxa were classified as obligate subterranean species, including four endemic species: the pseudoscorpion Mundochthonius cavernicolus, the amphipod Gammarus acherondytes, the milliped Chaetaspis sp. (undescribed), and the dipluran Eumesocampa sp. (undescribed). Gammarus acherondytes, recently listed as an endangered species, was found in six previously unsampled caves. All sites were rank-ordered according to the number of global and state rare species. The greatest single site diversity was found in Fogelpole Cave with 18 global and 20 state rare species. -
Hotspots of Subterranean Biodiversity in Caves and Wells
...J Oklahoma State Univ. Interlibrary Loan Call#: pdf w Location: pdf a:: Journal Title: Journal of cave and karst studies ; <( the National Speleological Society bulletin. Volume: 62 Issue: 1 ARIEL MonthNear: 2000 MaxCost: $501FM Pages: 11-17 Scanned by: Article Title: DC Culver and B Sket; Hotspots of Subterranean Shipped by: Biodiversity in Caves and Wells Ariel: 128.194.84.50 Article Author: Fax: 979-458-2032 or Borrower: TXA Shipping Address: Patron: Bandel, Micaela TAMU Libraries - College Station .. TAE z 41 HOU I- ILL Number: 85855670 Lending ~ String: *OKS,COD,IXA,TXH,VA@ ""0 The work from which this copy was made did not include a formal copyright notice. Copyright law may protect this work. Uses may be al lowed with permission from the rights holder, or if the copyright on the work has expired, or if the use is "fair use" or if it is within another exemption. The user of this work is responsible for determining its lawful uses. David C. Culver and Boris Sket - Hotspots of Subterranean Biodiversity in Caves and Wells . .Journal of Cave and Karst Studies 62(1):11-17. HOTSPOTS OF SUBTERRANEAN BIODIVERSITY IN CAVES AND WELLS DAVID C. CULVER Department of Biology, American University, 4400 Massachusetts Ave., NW, Washington, DC 20016, USA, [email protected] BORIS SKET Department of Biology, Biotechnical Faculty, University of Ljubljana, PO. Box 2995, 1001 Ljubljana, SLOVENIA, [email protected] We documented 18 caves and two karst wells that have 20 or more stygobites and troglobites. Crustacea dominated the aquatic fauna. Taxonomic composition ofthe terrestrial fauna varied, but Arachnida and Insecta together usually dominated. -
Monitoring Methodology and Protocols for 20 Habitats, 20 Species and 20 Birds
1 Finnish Environment Institute SYKE, Finland Monitoring methodology and protocols for 20 habitats, 20 species and 20 birds Twinning Project MK 13 IPA EN 02 17 Strengthening the capacities for effective implementation of the acquis in the field of nature protection Report D 3.1. - 1. 7.11.2019 Funded by the European Union The Ministry of Environment and Physical Planning, Department of Nature, Republic of North Macedonia Metsähallitus (Parks and Wildlife Finland), Finland The State Service for Protected Areas (SSPA), Lithuania 2 This project is funded by the European Union This document has been produced with the financial support of the European Union. Its contents are the sole responsibility of the Twinning Project MK 13 IPA EN 02 17 and and do not necessarily reflect the views of the European Union 3 Table of Contents 1. Introduction .......................................................................................................................................................... 6 Summary 6 Overview 8 Establishment of Natura 2000 network and the process of site selection .............................................................. 9 Preparation of reference lists for the species and habitats ..................................................................................... 9 Needs for data .......................................................................................................................................................... 9 Protocols for the monitoring of birds .................................................................................................................... -
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 -
Podgrad, Sw Slovenia Speleogeneza in Sedimentaci
COBISS: 1.01 SPELEOGENESIS AND DEPOSITIONAL HISTORY OF PALEOKARST PHREATIC CAVES/CAVITIES; PODGRAD, SW SLOVENIA SPELEOGENEZA IN SEDIMENTACIJSKA ZGODOVINA PALEOKRAŠKIH JAM/VOTLIN PREŽETE CONE; PODGRAD, JZ SLOVENIJA Bojan OTONIČAR1,* Abstract UDC 551.44:551.35(497.434) Izvleček UDK 551.44:551.35(497.434) Bojan Otoničar: Speleogenesis and depositional history of Bojan Otoničar: Speleogeneza in sedimentacijska zgodovina paleokarst phreatic caves/cavities; Podgrad, SW Slovenia paleokraških jam/votlin prežete cone; Podgrad, JZ Slovenija The studied paleokarst corresponds to an uplifted peripheral Raziskovani paleokras se je oblikoval na dvignjeni periferni foreland bulge when Upper Cretaceous diagenetically imma- izboklini, ko so bili diagenetsko nezreli zgornje kredni kar- ture eogenetic carbonates were subaerially exposed, karstified bonati dvignjeni nad morsko gladino in zakraseli. Kasneje je and subsequently overlain by upper Paleocene/lower Eocene bil ta zakraseli del periferne izbokline ponovno potopljen pod palustrine limestone. morsko gladino, paleokraško površje pa prekrito z zgornje pale- Among the subsurface paleokarstic features, both vadose and ocenskimi do spodnje eocenskimi palustrinimi apnenci. phreatic forms occur. The phreatic caves/cavities include fea- Na raziskovanem območju se pojavljajo podpovršinske tures characteristic of the mixing zone speleogenesis at the paleokraške oblike značilne tako za prežeto kot neprežeto interface between freshwater (brackish water) lenses and the hidrogeološko cono. Kraške jame in manjše votlinice prežete underlying seawater. They were found in various positions cone kažejo značilnosti speleogeneze v območju mešanja with respect to the paleokarstic surface, the deepest being meteorne in morske vode. Pojavljajo se v različnih nivo- about 75 m below the surface. Three indistinct horizons of jih glede na paleokraško površje, najgloblje približno 75 cavities/caves and intermediate vugs were recognized. -
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. -
Institutions Contact Person Priority 1, Strategic Theme 1: Innovation As
Institutions Contact person e-mail Priority 1, Strategic theme 1: Innovation as key for economic development Municipality of Koper, Verdijeve 10, 6000 Koper, Slovenia Ivana Štrkalj [email protected] Municipality of Izola, Sončno nabrežje 8, 6310 Izola, Slovenia Boštjan Lavrič [email protected] Regional development agency of Northern Primorska, Trg Edvarda Kardelja 3, 5000 Nova Gorica, Slovenia Tomaž Vadjunec [email protected] Chamber of Craft and Small Business of Slovenia, Celovška 71, 1000 Ljubljana, Slovenia Bogdan Sovinc [email protected] Primorska Technology Park, mednarodni prehod 6, vrtojba, 5290 Šempeter pri Novi Gorici Tanja Kožuh [email protected] Tehniški šolski center Nova Gorica, Cankarjeva 10, 5000 Nova Gorica, Slovenia Rosana Pahor [email protected] GEA College, Kidričevo nabrežje 2, 6330 Piran Majda Gartner [email protected] Centre of Excellence BIPC (www.cobik.si) Mladen Dakič [email protected] Priority 2, Strategic theme 1: Improving marine, coastal and delta rivers environment by joint management Institute for Water of the Republic of Slovenia, Hajdrihova 28 c, 1000 Ljubljana, Slovenia Leon Gosar [email protected] Jožef Stefan Institute, Jamova cesta 39, 1000 Ljubljana, Slovenia Sonja Lojen [email protected] Municipality of Izola, Sončno nabrežje 8, 6310 Izola, Slovenia Boštjan Lavrič [email protected] Slovenian national building and civil engineering institute, Dimičeva 12, 1000 Ljubljana Karmen Fifer [email protected] Municipality of Koper, Verdijeve 10, 6000 Koper, Slovenia Ivana Štrkalj [email protected] Priority 2, Strategic theme 2: Protection from ballast water pollution A single potential partnership with Slovenian institutions is in a process of establishment where the Institute for Water of the Republic of Slovenia will assume a role of a Lead Beneficiary. -
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs
ORIGINAL RESEARCH published: 28 April 2016 doi: 10.3389/feart.2016.00049 Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs Tomaso R. R. Bontognali 1*, Ilenia M. D’Angeli 2*, Nicola Tisato 1, 3, Crisogono Vasconcelos 1, Stefano M. Bernasconi 1, Esteban R. G. Gonzales 4 and Jo De Waele 2, 5 1 Department of Earth Sciences, ETH Zurich, Zurich, Switzerland, 2 Department of Biological, Geological and Environmental Sciences, Bologna University, Bologna, Italy, 3 Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX, USA, 4 Comité Espeleológico de Matanzas, Sociedad Espeleológica de Cuba, Matanzas, Cuba, 5 Associazione di Esplorazioni Geografiche la Venta, Treviso, Italy Unusual speleothems resembling giant mushrooms occur in Cueva Grande de Santa Catalina, Cuba. Although these mineral buildups are considered a natural heritage, their composition and formation mechanism remain poorly understood. Here we characterize their morphology and mineralogy and present a model for their genesis. We propose that the mushrooms, which are mainly comprised of calcite and aragonite, formed during four Edited by: different phases within an evolving cave environment. The stipe of the mushroom is an Karim Benzerara, assemblage of three well-known speleothems: a stalagmite surrounded by calcite rafts Centre National de la Recherche Scientifique, France that were subsequently encrusted by cave clouds (mammillaries). More peculiar is the Reviewed by: cap of the mushroom, which is morphologically similar to cerebroid stromatolites and Jakob Zopfi, thrombolites of microbial origin occurring in marine environments. Scanning electron University of Basel, Switzerland microscopy (SEM) investigations of this last unit revealed the presence of fossilized Michal Gradzinski, Jagiellonian University, Poland extracellular polymeric substances (EPS)—the constituents of biofilms and microbial *Correspondence: mats. -
A Checklist and Annotated Bibliography of the Subterranean Aquatic Fauna of Texas
A CHECKLIST AND ANNOTATED BIBLIOGRAPHY OF THE SUBTERRANEAN AQUATIC FAUNA OF TEXAS JAMES R. REDDELL and ROBERT W. MITCHELL Texas Technological College WATER RESOURCES \ CENTER Lubbock, Texas WRC 69-6 INTERNATIONAL CENTER for ARID and August 1969 SEMI-ARID LAND STUDIES A CHECKLIST AND ANNOTATED BIBLIOGRAPHY OF THE SUBTERRANEAN AQUATIC FAUNA OF TEXAS James R. Reddell and Robert W. Mitchell Department of Biology Texas Tech University Lubbock, Texas INTRODUCTION In view of the ever-increasing interest in all studies relating to the water resources of Texas, we have found it timely to prepare this guide to the fauna and biological literature of our subterranean waters. The value of such a guide has already been demonstrated by Clark (1966) in his "Publications, Personnel, and Government Organizations Related to the Limnology, Aquatic Biology and Ichthyology of the Inland Waters of Texas". This publication dea ls primarily with inland surface waters, however, barely touching upon the now rather extensive literature which has accumulated on the biology of our subterranean waters. To state a n obvious fact, it is imperative that our underground waters receive the attention due them. They are one of our most important resources. Those subterranean waters for which biological data exi st are very un equally distributed in the state. The best known are those which are acces sible to collection and study via the entrances of caves. Even in cavernous regions there exist inaccessible deep aquifers which have yielded little in formation as yet. Biological data from the underground waters of non-cave rn ous areas are virtually non-existant. -
Mighty Caves and Karst –
MIGHTY CAVES AND KARST – NATURE´S HIDDEN GEM Tour Description From one jewel to another, for all the photo-hungry cyclers and nature lovers. Surrender yourself to this week long self guided cycling tour, blessed with true beauty, pristine nature, Karst landscape and it’s phenomena’s. Yes, biking in Slovenia sure is an amazing way to spend your holiday. While cycling in Karst you will be accomodated in two Hotels, in two beautiful Karst towns, from where interesting cycle day tours are designed for you. Starting point is in Postojna, the jewel in the Karst Region. Postojna is in many ways marked by its unique position, which had a significant influence on the town’s development as early as ancient times. The town lies on the Pivka River and because of the two world class attractions; Postojna Cave and Predjama Castle is visited by many tourists every year. Biking through Karst area and discovering it’s wonders such as the caves, Rakov Škocjan, intermittent lakes, sinking rivers, rocky surface and dolines, is a unique and special experience. The second location of this scenic cycle tour is Divača. Divača is today the biggest settlement and seat of the municipality. In the 16th century it was just a hamlet of sheep farmers, but with the development of transport running from the port of Trieste to the interior, it gained importance, expanded and developed. The importance of the railway is still evident today in the steam locomotive engine that now stands as a museum piece open to visitors at the railway station.