Descriptions of Virginia Caves
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In Search of the Indiana Lenape
IN SEARCH OF THE INDIANA LENAPE: A PREDICTIVE SUMMARY OF THE ARCHAEOLOGICAL IMPACT OF THE LENAPE LIVING ALONG THE WHITE RIVER IN INDIANA FROM 1790 - 1821 A THESIS SUBMITTED TO THE GRADUATE SCHOOL IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS BY JESSICA L. YANN DR. RONALD HICKS, CHAIR BALL STATE UNIVERSITY MUNCIE, INDIANA DECEMBER 2009 Table of Contents Figures and Tables ........................................................................................................................ iii Chapter 1: Introduction ................................................................................................................ 1 Research Goals ............................................................................................................................ 1 Background .................................................................................................................................. 2 Chapter 2: Theory and Methods ................................................................................................. 6 Explaining Contact and Its Material Remains ............................................................................. 6 Predicting the Intensity of Change and its Effects on Identity................................................... 14 Change and the Lenape .............................................................................................................. 16 Methods .................................................................................................................................... -
Description of the Estillville Sheet
DESCRIPTION OF THE ESTILLVILLE SHEET. GEOGRAPHY. ward across the States of Illinois and Indiana. course to the Ohio. South of Chattanooga the ment among the high points on Wallin Ridge, the Its eastern boundary is sharply defined by the streams flow directly to the Gulf of Mexico. even crest of Stone Mountain, and the summit of General relations. The territory represented Alleghany front and ..the Cumberland escarp Topography of the Appalachian province. The Powell Mountain west of Slemp Gap. Beyond by the Estillville atlas sheet is one-quarter of a ment. The rocks of this division are almost different divisions of the province vary much in Big Black Mountain, with its irregular crest, is square degree of the earth's surface, extending entirely of sedimentary origin, and remain very character of topography, as do also different por the even summit of Pine Mountain, planed down from latitude 36° 30' on the south to 37° on the nearly horizontal. The character of the surface, tions of the same division. This variation of top to the general height of the valley ridges. The north, and from longitude 82° 30' on the east to which is dependent on the character and attitude ographic forms is due to several conditions, which peneplain was originally very nearly horizontal, 83° on the west. Its average width is 27.7 miles, of the rocks, is that of a plateau more or less com either prevail at present or have prevailed in the but it has been tilted, so that now it varies in ele its length is 34.5 miles, and its area is 956.6 pletely worn down. -
Message from the New Chairman
Subcommission on Devonian Stratigraphy Newsletter No. 21 April, 2005 MESSAGE FROM THE NEW CHAIRMAN Dear SDS Members: This new Newsletter gives me the pleasant opportunity to thank you for your confidence which should allow me to lead our Devonian Subcommission successfully through the next four years until the next International Geological Congress in Norway. Ahmed El Hassani, as Vice-Chairman, and John Marshall, as our new Secretary, will assist and help me. As it has been our habit in the past, our outgoing chairman, Pierre Bultynck, has continued his duties until the end of the calendar year, and in the name of all the Subcommission, I like to express our warmest thanks to him for all his efforts, his enthusi- asm for our tasks, his patience with the often too slow progress of research, and for the humorous, well organized and skil- ful handling of our affairs, including our annual meetings. At the same time I like to thank all our outgoing Titular Members for their partly long-time service and I express my hope that they will continue their SDS work with the same interest and energy as Corresponding Members. The new ICS rules require a rather constant change of voting members and the change from TM to CM status should not necessarily be taken as an excuse to adopt the lifestyle of a “Devonian pensioner”. I see no reason why constantly active SDS members shouldn´t become TM again, at a later stage. On the other side, the rather strong exchange of voting members should bring in some fresh ideas and some shift towards modern stratigraphical tech- niques. -
5 Years on Ice Age Europe Network Celebrates – Page 5
network of heritage sites Magazine Issue 2 aPriL 2018 neanderthal rock art Latest research from spanish caves – page 6 Underground theatre British cave balances performances with conservation – page 16 Caves with ice age art get UnesCo Label germany’s swabian Jura awarded world heritage status – page 40 5 Years On ice age europe network celebrates – page 5 tewww.ice-age-europe.euLLING the STORY of iCe AGE PeoPLe in eUROPe anD eXPL ORING PLEISTOCene CULtURAL HERITAGE IntrOductIOn network of heritage sites welcome to the second edition of the ice age europe magazine! Ice Age europe Magazine – issue 2/2018 issn 25684353 after the successful launch last year we are happy to present editorial board the new issue, which is again brimming with exciting contri katrin hieke, gerdChristian weniger, nick Powe butions. the magazine showcases the many activities taking Publication editing place in research and conservation, exhibition, education and katrin hieke communication at each of the ice age europe member sites. Layout and design Brightsea Creative, exeter, Uk; in addition, we are pleased to present two special guest Beate tebartz grafik Design, Düsseldorf, germany contributions: the first by Paul Pettitt, University of Durham, cover photo gives a brief overview of a groundbreaking discovery, which fashionable little sapiens © fumane Cave proved in february 2018 that the neanderthals were the first Inside front cover photo cave artists before modern humans. the second by nuria sanz, water bird – hohle fels © urmu, director of UnesCo in Mexico and general coordi nator of the Photo: burkert ideenreich heaDs programme, reports on the new initiative for a serial transnational nomination of neanderthal sites as world heritage, for which this network laid the foundation. -
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. -
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. -
Survey Solutions for 3D Acquisition and Representation of Artificial And
applied sciences Article Survey Solutions for 3D Acquisition and Representation of Artificial and Natural Caves Daniele Giordan 1 , Danilo Godone 1,* , Marco Baldo 1, Marco Piras 2 , Nives Grasso 2 and Raffaella Zerbetto 3 1 Italian National Research Council, Research Institute for Geo-Hydrological Protection (CNR-IRPI), Strada delle Cacce 73, 10135 Torino, Italy; [email protected] (D.G.); [email protected] (M.B.) 2 Department of Environment, Land and Infrastructure Engineering (DIATI), Politecnico di Torino, Corso Duca Degli Abruzzi, 24, 10129 Torino, Italy; [email protected] (M.P.); [email protected] (N.G.) 3 Speleo Club Tanaro, Via Carrara, 12075 Garessio, Italy; [email protected] * Correspondence: [email protected] Abstract: A three-dimensional survey of natural caves is often a difficult task due to the roughness of the investigated area and the problems of accessibility. Traditional adopted techniques allow a simplified acquisition of the topography of caves characterized by an oversimplification of the geometry. Nowadays, the advent of LiDAR and Structure from Motion applications eased three- dimensional surveys in different environments. In this paper, we present a comparison between other three-dimensional survey systems, namely a Terrestrial Laser Scanner, a SLAM-based portable instrument, and a commercial photo camera, to test their possible deployment in natural caves survey. We presented a comparative test carried out in a tunnel stretch to calibrate the instrumentation on a benchmark site. The choice of the site is motivated by its regular geometry and easy accessibility. According to the result obtained in the calibration site, we presented a methodology, based on the Citation: Giordan, D.; Godone, D.; Structure from Motion approach that resulted in the best compromise among accuracy, feasibility, Baldo, M.; Piras, M.; Grasso, N.; and cost-effectiveness, that could be adopted for the three-dimensional survey of complex natural Zerbetto, R. -
Scenic Landforms of Virginia
Vol. 34 August 1988 No. 3 SCENIC LANDFORMS OF VIRGINIA Harry Webb . Virginia has a wide variety of scenic landforms, such State Highway, SR - State Road, GWNF.R(T) - George as mountains, waterfalls, gorges, islands, water and Washington National Forest Road (Trail), JNFR(T) - wind gaps, caves, valleys, hills, and cliffs. These land- Jefferson National Forest Road (Trail), BRPMP - Blue forms, some with interesting names such as Hanging Ridge Parkway mile post, and SNPMP - Shenandoah Rock, Devils Backbone, Striped Rock, and Lovers Leap, National Park mile post. range in elevation from Mt. Rogers at 5729 feet to As- This listing is primarily of those landforms named on sateague and Tangier islands near sea level. Two nat- topographic maps. It is hoped that the reader will advise ural lakes occur in Virginia, Mountain Lake in Giles the Division of other noteworthy landforms in the st& County and Lake Drummond in the City of Chesapeake. that are not mentioned. For those features on private Gaps through the mountains were important routes for land always obtain the owner's permission before vis- early settlers and positions for military movements dur- iting. Some particularly interesting features are de- ing the Civil War. Today, many gaps are still important scribed in more detail below. locations of roads and highways. For this report, landforms are listed alphabetically Dismal Swamp (see Chesapeake, City of) by county or city. Features along county lines are de- The Dismal Swamp, located in southeastern Virginia, scribed in only one county with references in other ap- is about 10 to 11 miles wide and 15 miles long, and propriate counties. -
1. Background-Regions Economic Development Situation
1. BACKGROUND-REGIONS ECONOMIC DEVELOPMENT SITUATION A. General Description of Area The Cumberland Plateau Planning District is in Southwest Virginia and encompasses the counties of Buchanan, Dickenson, Russell and Tazewell. The District borders West Virginia on the north and Kentucky on the northeast. Wise, Scott, Washington, Smyth and Bland Counties in Virginia form the boundaries on the west, south, and east. The District is 67 miles long and 40 miles wide and covers approximately 1,848 square miles. The District is divided into two physiographically distinct regions, both lying in the Appalachian Highlands. The counties of Buchanan and Dickenson, along with the northern portions of Russell and Tazewell Counties, lie in the Cumberland Plateau which is, in turn, a part of the Appalachian Plateau. This area has a uniformly mountainous surface characterized by many small streams separated by sharply rising ridges, steep slopes, and narrow valleys. The remaining region of the District, comprising the greater portion of Russell and Tazewell Counties, lies in the Valley and Ridge Province of the Appalachian Highlands. This belt, consisting of alternate valleys and ridges is bordered on the south by the Clinch Mountains and on the north by the Cumberland Plateau. Elevations vary from 845 feet above sea level where the Levisa Fork crosses into Kentucky to 4,705 feet atop Garden Mountain in the southeastern part of the District near the Bland County line. The most prominent physiographic features in the District are Clinch Mountain, Breaks of the Cumberland, Burkes Garden, Big A Mountain, and Pine Mountain. Cumberland Plateau PDC 2018 Profile Page 1 Comparatively smooth to moderately sloping uplands are found in places in the southern and southeastern portions of the District. -
Community Conservation Assessment for Cave Streams and Associated Rare Animal Species
Community Conservation Assessment for Cave Streams and Associated Rare Animal Species (photo by J. Lewis) USDA Forest Service, Eastern Region October 2002 Julian J. Lewis, Ph.D. J. Lewis & Associates, Biological Consulting 217 W. Carter Avenue Clarksville, IN 47129 [email protected] HOOSIER NATIONAL FOREST This Conservation Assessment was prepared to compile the published and unpublished information on cave stream habitats and associated rare animals species in the Hoosier National Forest. It does not represent a management decision by the U.S. Forest Service. Though the best scientific information available was used and subject experts were consulted in preparation of this document, it is expected that new information will arise. In the spirit of continuous learning and adaptive management, if you have information that will assist in conserving the subject community and associated taxa, please contact the Eastern Region of the Forest Service Threatened and Endangered Species Program at 310 Wisconsin Avenue, Milwaukee, Wisconsin 53203. Community Conservation Assessment for Cave Streams 2 and Associated Rare Animal Specie Table of Contents EXECUTIVE SUMMARY.....................................................................4 DESCRIPTION OF HABITAT AND COMMUNITY...........................4 ENVIRONMENTAL CONDITIONS .....................................................5 CURRENT COMMUNITY CONDITION, DISTRIBUTION AND ABUNDANCE ........................................................................................6 REGIONAL FORESTER -
Hotspots of Subterranean Biodiversity in Caves and Wells
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, P.O. 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 of the terrestrial fauna varied, but Arachnida and Insecta together usually dominated. Geographically, the sites were concentrated in the Dinaric Karst (6 caves). Sites tended to have high primary productivity or rich organic input from the surface, be large caves, or have permanent groundwater (phreatic water). Dokumentirala sva 18 jam in dva kraška vodnjaka, iz katerih je znanih 20 ali vec vrst troglobiontov in stigobiontov. V vodni favni preladujejo raki. Taksonomski sestav kopenske favne je raznolik, vendar pajkovci in zuzelke skupaj navadno prevladujejo. Najvec takšnih jam (šest) je v Dinarskem krasu. Nadpovprecno so zastopane jame z lastno primarno produkcijo ali bogatim vnosom hrane s površja, obsezne jame in jame, ki vkljucujejo tudi freatsko plast. Over the past few years, there has been a growing aware- terns at individual sites. Even though most subterranean bio- ness and concern with biodiversity worldwide. Books and diversity results from the accumulation of different species monographs with a focus on biodiversity have appeared (e.g., from nearby sites, there are some outstanding examples of high Wilson 1992; Master et al. -
Caves of Missouri
CAVES OF MISSOURI J HARLEN BRETZ Vol. XXXIX, Second Series E P LU M R I U BU N S U 1956 STATE OF MISSOURI Department of Business and Administration Division of GEOLOGICAL SURVEY AND WATER RESOURCES T. R. B, State Geologist Rolla, Missouri vii CONTENT Page Abstract 1 Introduction 1 Acknowledgments 5 Origin of Missouri's caves 6 Cave patterns 13 Solutional features 14 Phreatic solutional features 15 Vadose solutional features 17 Topographic relations of caves 23 Cave "formations" 28 Deposits made in air 30 Deposits made at air-water contact 34 Deposits made under water 36 Rate of growth of cave formations 37 Missouri caves with provision for visitors 39 Alley Spring and Cave 40 Big Spring and Cave 41 Bluff Dwellers' Cave 44 Bridal Cave 49 Cameron Cave 55 Cathedral Cave 62 Cave Spring Onyx Caverns 72 Cherokee Cave 74 Crystal Cave 81 Crystal Caverns 89 Doling City Park Cave 94 Fairy Cave 96 Fantastic Caverns 104 Fisher Cave 111 Hahatonka, caves in the vicinity of 123 River Cave 124 Counterfeiters' Cave 128 Robbers' Cave 128 Island Cave 130 Honey Branch Cave 133 Inca Cave 135 Jacob's Cave 139 Keener Cave 147 Mark Twain Cave 151 Marvel Cave 157 Meramec Caverns 166 Mount Shira Cave 185 Mushroom Cave 189 Old Spanish Cave 191 Onondaga Cave 197 Ozark Caverns 212 Ozark Wonder Cave 217 Pike's Peak Cave 222 Roaring River Spring and Cave 229 Round Spring Cavern 232 Sequiota Spring and Cave 248 viii Table of Contents Smittle Cave 250 Stark Caverns 256 Truitt's Cave 261 Wonder Cave 270 Undeveloped and wild caves of Missouri 275 Barry County 275 Ash Cave