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University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Eudo Citizenship Observatory
EUDO CITIZENSHIP OBSERVATORY COUNTRY REPORT: ICELAND Gudni Th. Jóhannesson, Gunnar Thór Pétursson, Thorbjörn Björnsson Revised and updated January 2013 http://eudo-citizenship.eu European University Institute, Florence Robert Schuman Centre for Advanced Studies EUDO Citizenship Observatory Report on Iceland Gudni Th. Jóhannesson,Gunnar Thór Pétursson, Thorbjörn Björnsson Revised and updated January 2013 EUDO Citizenship Observatory Robert Schuman Centre for Advanced Studies in collaboration with Edinburgh University Law School Country Report, RSCAS/EUDO-CIT-CR 2013/8 Badia Fiesolana, San Domenico di Fiesole (FI), Italy © Gudni Th. Jóhannesson,Gunnar Thór Pétursson, Thorbjörn Björnsson This text may be downloaded only for personal research purposes. Additional reproduction for other purposes, whether in hard copies or electronically, requires the consent of the authors. Requests should be addressed to [email protected] The views expressed in this publication cannot in any circumstances be regarded as the official position of the European Union Published in Italy European University Institute Badia Fiesolana I – 50014 San Domenico di Fiesole (FI) Italy www.eui.eu/RSCAS/Publications/ www.eui.eu cadmus.eui.eu Research for the EUDO Citizenship Observatory Country Reports has been jointly supported, at various times, by the European Commission grant agreements JLS/2007/IP/CA/009 EUCITAC and HOME/2010/EIFX/CA/1774 ACIT and by the British Academy Research Project CITMODES (both projects co-directed by the EUI and the University of Edinburgh). The financial support from these projects is gratefully acknowledged. For information about the project please visit the project website at http://eudo-citizenship.eu Iceland Gudni Th. Jóhannesson,Gunnar Thór Pétursson and Thorbjörn Björnsson 1 Introduction Historically, Iceland has been among the world’s most homogenous countries. -
Topography Along the Virginia-Kentucky Border
Preface: Topography along the Virginia-Kentucky border. It took a long time for the Appalachian Mountain range to attain its present appearance, but no one was counting. Outcrops found at the base of Pine Mountain are Devonian rock, dating back 400 million years. But the rocks picked off the ground around Lexington, Kentucky, are even older; this limestone is from the Cambrian period, about 600 million years old. It is the same type and age rock found near the bottom of the Grand Canyon in Colorado. Of course, a mountain range is not created in a year or two. It took them about 400 years to obtain their character, and the Appalachian range has a lot of character. Geologists tell us this range extends from Alabama into Canada, and separates the plains of the eastern seaboard from the low-lying valleys of the Ohio and Mississippi rivers. Some subdivide the Appalachians into the Piedmont Province, the Blue Ridge, the Valley and Ridge area, and the Appalachian plateau. We also learn that during the Paleozoic era, the site of this mountain range was nothing more than a shallow sea; but during this time, as sediments built up, and the bottom of the sea sank. The hinge line between the area sinking, and the area being uplifted seems to have shifted gradually westward. At the end of the Paleozoric era, the earth movement are said to have reversed, at which time the horizontal layers of the rock were uplifted and folded, and for the next 200 million years the land was eroded, which provided material to cover the surrounding areas, including the coastal plain. -
1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
Bureau of Reclamation Hoh River Geomorphic
Summary Report for Geomorphic Assessment of Hoh River in Washington State Hoh River Miles 17 to 40: Oxbow Canyon and Mount Tom Creek U.S. Department of the Interior Bureau of Reclamation Technical Service Center July 2004 Summary Report for Geomorphic Assessment of Hoh River in Washington State River Miles 17 to 40 between Oxbow Canyon and Mount Tom Creek Report Prepared by: Lucille A. Piety, Geomorphologist Seismotectonics & Geophysics Group, Technical Service Center Jennifer A. Bountry, P.E., Hydraulic Engineer Sedimentation & River Hydraulics Group, Technical Service Center Timothy J. Randle, P.E., Hydraulic Engineer Sedimentation & River Hydraulics Group, Technical Service Center Edward W. Lyon, Jr., Geologist Geology, Exploration, & Instrumentation Group Pacific Northwest Regional Office Report Peer Reviewed by: Ralph E. Klinger, Ph.D., Geomorphologist Flood Hydrology Group, Technical Service Center Richard A. Link, Regional Geologist Geology, Exploration, & Instrumentation Group Pacific Northwest Regional Office U.S. Department of the Interior Bureau of Reclamation Technical Service Center, Denver, Colorado UNITED STATES DEPARTMENT OF THE INTERIOR The mission of the Department of the Interior is to protect and provide access to our Nation=s natural and cultural heritage and honor our trust responsibilities to Indian tribes and our commitments to island communities. BUREAU OF RECLAMATION The mission of the Bureau of Reclamation is to manage, develop, and protect water and related resources in an environmentally and economically sound -
Social Changes and Culture in Icelandic Coastal Villages
Social Changes and culture in Icelandic Coastal villages Unnur Dís Skaptadóttir (Faculty of Social Sciences, University of Iceland) Abstract Coastal villages in Iceland which have always been character- ized by transformation have in the last two decades been shaped by restructuring of the fisheries, new economic activities such as in tourism, and growing number of foreign laborers. The article examines social and economic transformations in coastal areas based on different research projects that were all based on field research in fishery based villages the northwest part of Iceland. My discussion brings forward some issues re- garding the inhabitants’ changing perceptions of local culture during this time. In the last two decades the concept of culture has become an instrument of both local populations in marginal areas and ethnic groups all over the world with more knowled- ge of other people and other ways of living. Unlike before, cul- ture is increasingly used in the villages in North West of Iceland to describe commonalities and diversities found within them. I illustrate how inhabitants of small villages talk about culture and how they show local culture to tourists. Furthermore with a growing population of foreign origin a conception of multicul- turalism has appeared in the region which again makes the in- habitants more reflective of local culture of the region. These changes can only be understood if put into a global context. However it is important to combine a spatial perspective that 149 sheds light on transnational connections with a historical one to understand the cultural transformations in the villages. Keywords :Coastal villages, locality, culture, labour migrants, multiculture Coastal villages in Iceland have always been characterized by economic and societal changes and by mobility of people and products. -
The Hyaloclastite Ridge Formed in the Subglacial 1996 Eruption in Gjfilp, Vatnaj6kull, Iceland: Present Day Shape and Future Preservation
The hyaloclastite ridge formed in the subglacial 1996 eruption in Gjfilp, Vatnaj6kull, Iceland: present day shape and future preservation M. T. GUDMUNDSSON, F. PALSSON, H. BJORNSSON & ~. HOGNADOTTIR Science Institute, University of Iceland, Hofsvallag6tu 53, 107 Reykjavik, Iceland (e-mail: [email protected]) Abstract: In the Gjfilp eruption in 1996, a subglacial hyaloclastite ridge was formed over a volcanic fissure beneath the Vatnaj6kull ice cap in Iceland. The initial ice thickness along the 6 km-long fissure varied from 550 m to 750 m greatest in the northern part but least in the central part where a subaerial crater was active during the eruption. The shape of the subglacial ridge has been mapped, using direct observations of the top of the edifice in 1997, radio echo soundings and gravity surveying. The subglacial edifice is remarkably varied in shape and height. The southern part is low and narrow whereas the central part is the highest, rising 450 m above the pre-eruption bedrock. In the northern part the ridge is only 150-200m high but up to 2kin wide, suggesting that lateral spreading of the erupted material occurred during the latter stages of the eruption. The total volume of erupted material in Gj~tlp was about 0.8 km 3, mainly volcanic glass. The edifice has a volume of about 0.7 km 3 and a volume of 0.07 km 3 was transported with the meltwater from Gj~lp and accumulated in the Grimsv6tn caldera, where the subglacial lake acted as a trap for the sediments. This meltwater-transported material was removed from the southern part of the edifice during the eruption. -
Ice Core Drilling and Subglacial Lake Studies on the Temperate Ice Caps in Iceland
Ice core drilling and subglacial lake studies on the temperate ice caps in Iceland Iceland astride the Mid-Atlantic ridge Lecture # 36 Astrobiology Winter School Ice drilling projects in Iceland University of Hawaii, Jan. 2005 Thorsteinn Thorsteinsson ([email protected]) National Energy Authority Ice cover during the late glacial period. Combination of hot spot volcanism, spreading on the Mid-Atlantic ridge and glaciation leads to unusual geology. From Thordarson and Höskuldsson (2003). Subglacial volcanism beneath an ice sheet creates unusual landforms: Tuyas (tablemountains) and ridges. Herðubreið, N-Iceland Submarine eruptions create similar formations. Biologicial colonization monitored from the beginning Surtsey eruption, S. of Iceland, 1963-1967. Recent subglacial eruption in Grímsvötn, Vatnajökull ice cap. Jökulsárgljúfur canyons, N. Iceland: Formed in a catastrophic flood from Vatnajökull 2500 years ago. Icelandic analogs to hillside gullies on Mars Mars Mars Iceland Iceland Iceland Temperate ice caps Hofsjökull, 890 km2 cover >10% of Iceland Vatnajökull 2 Langjökull 8000 km 2 920 km Max. thickness: 950 m Mýrdalsjökull 550 km2 - Dynamic ice caps in a maritime climate. - High accumulation rates (2-4 m w.eq. yr-1) - Extensive melting during summer, except at highest elevations (> 1800 m) - Mass balance of ice caps negative since 1995 1972: A 415 m ice core was drilled on the NW-part of Vatnajökull Activities not continued at that time, drill was discarded. Mass balance of Hofsjökull Ice Cap 4 2 0 Winter balance -2 Summer balance H2O Net balance m -4 Cumulative mass balance -6 -8 -10 1987 1992 1997 2002 Climate, Water, Energy: A research project investigating the effect of climate change on energy production in the Nordic countries Temperature increase 1990-2050 °C CWE uses IPCC data to create scenarios for temperature and precipitation change in the Nordic region in the future Modelled change in volume of Hofsjökull ice cap 2000-2002, Modelled glacial meltwater using four different dT and dP discharge (run-off) 2000-2200. -
Geologica Acta, Vol.4, N°4, 2006, 409-438 |415| Ce
'geológica FOmS^Y ACTA GEOLÓGICA HISPAfilCA Geológica acta: an international earth science journal Universidad de Barcelona [email protected] ISSN (Versión impresa): 1695-6133 ESPAÑA 2006 C.C. Labandeira THE FOUR PHASES OF PLANT-ARTHROPOD ASSOCIATIONS IN DEEP TIME Geológica acta: an international earth science journal, december, año/vol. 4, número 004 Universidad de Barcelona Barcelona, España pp. 409-438 Red de Revistas Científicas de América Latina y el Caribe, España y Portugal ®re¿!alyc^ Universidad Autónoma del Estado de México http://redalyc.uaemex.mx Geológica Acta, Vol.4, N° 4, 2006, 409-438 Appendix l-IX geología acta Available online at www.geologica-acta.com The Four Phases of Plant-Arthropod Associations in Deep Time C.C. LABANDEIRA |1||2| 111 Smithsonian Institution, National Museum of Natural History P.O. Box 37012, MRC-121 Department of Paleobiology, Washington, D.C., USA 200137012. E-mail: [email protected] 121 University of Maryland, Department of Entomology College Park, Maryland, USA 20742 1 ABSTRACT I Vascular-plant hosts, their arthropod herbivores, and associated functional feeding groups are distributed spa- tiotemporally into four major herbivore expansions during the past 420 m.y. They are: (1) a Late Silurian to Late Devonian (60 m.y.) phase of myriapod and apterygote, hexapod (perhaps pterygote) herbivores on several clades of primitive vascular-plant hosts and a prototaxalean fungus; (2) a Late Mississippian to end-Permian (85 m.y.) phase of mites and apterygote and basal pterygote herbivores on pteridophyte and basal gymnospermous plant hosts; (3) a Middle Triassic to Recent (245 m.y.) phase of mites, orthopteroids (in the broadest sense) and hemipteroid and basal holometabolan herbivores on pteridophyte and gymnospermous plant hosts; and (4) a mid Early Cretaceous to Recent (115 m.y.) phase of modern-aspect orthopteroids and derived hemipteroid and holometabolous herbivores on angiospermous plant hosts. -
Indian Raids and Massacres of Southwest Virginia
Indian Raids and Massacres of Southwest Virginia LAS VEGAS FAMILY HISTORY CENTER by Luther F. Addington and Emory L. Hamilton Published by Cecil L. Durham Kingsport, Tennessee FHL TITLE # 488344 Chapters I through XV are an exact reprint of "Indian Stories of Virginia's Last Frontier" by Luther F. Addington and originally published by The Historical Society of Southwest Virginia. Chapter XVI "Indian Tragedies Against the Walker Family" is by Emory L. Hamilton. Printed in the United States of America by Kingsport Press Kingsport, Tennessee TABLE OF CONTENTS CHAPTER PAGE I. INDIANS CAPTURE MARY INGLES 1 II. MURDER OF JAMES BOONE, 27 OCTOBER 10, 1773 III. MASSACRE OF THE HENRY FAMILY 35 IV. THE INDIAN MISSIONARY 38 V. CAPTURE OF JANE WHITAKER AND POLLY ALLEY 42 VI. ATTACK ON THE EVANS FAMILY, 1779 48 VII. ATTACK ON THOMAS INGLES' FAMILY 54 VIII. INDIANS AND THE MOORE FAMILY 59 IX. THE HARMANS' BATTLE 77 X. A FIGHT FOR LIFE 84 XI. CHIEF BENGE CARRIES AWAY MRS. SCOTT 88 XII. THE CAPTIVITY OF JENNY WILEY 97 XIII. MRS. ANDREW DAVIDSON AND CHILDREN CAPTURED 114 XIV. DAVID MUSICK TRAGEDY 119 XV. CHIEF BENGE'S LAST RAID 123 XVI. INDIAN TRAGEDIES AGAINST THE WALKER FAMILY NOTE: The interesting story of Caty Sage, who was stolen from her parents in Grayson County, 1792, by a vengeful white man and later grew to womanhood among the Wyandotts in the West, is well told by Mrs. Bonnie Ball in her book, Red Trails and White, Haysi, Virginia. 1 I CAPTIVITY OF MARY DRAPER INGLES Of all the young women taken into captivity by the Indians from Virginia's western frontier none suffered more anguish, nor bore her hardships more heroically, nor behaved with more thoughtfulness to ward her captors than did Mary Draper Ingles. -
Evidence for Extending Anomalous Miocene Volcanism at the Edge of The
1 Evidence for Extending Anomalous Miocene Volcanism at the Edge of the 2 East Antarctic Craton 3 4 K. J. Licht1, T. Groth1, J. P. Townsend2, A. J. Hennessy1, S. R. Hemming3, T. P. Flood4, and M. 5 Studinger5 6 1Department of Earth Sciences, Indiana University-Purdue University Indianapolis, Indianapolis, IN, 7 USA, 2HEDP Theory Department, Sandia National Laboratories, Albuquerque, NM, USA, 3Department of 8 Earth and Environmental Sciences, Columbia University, Lamont-Doherty Earth Observatory, Palisades, 9 NY, USA, 4Geology Department, St. Norbert College, DePere, WI, USA, 5NASA Goddard Space Flight 10 Center, Greenbelt, MD, USA 11 12 Corresponding author: Kathy Licht ([email protected]) 13 14 Key Points: 15 x Olivine basalt, hyaloclastite erratics and detrital zircon at Earth’s southernmost moraine 16 (Mt. Howe) indicate magmatic activity 17- 25 Ma. 17 x The source, indicated by a magnetic anomaly (-740 nT) ~400 km inland from the West 18 Antarctic Rift margin, expands extent of Miocene lavas. 19 x Data corroborate lithospheric foundering beneath southern Transantarctic Mountains based 20 on location of volcanism (duration < 5 my). 21 22 Abstract 23 Using field observations followed by petrological, geochemical, geochronological, and 24 geophysical data we infer the presence of a previously unknown Miocene subglacial volcanic 25 center ~230 km from the South Pole. Evidence of volcanism is from boulders of olivine-bearing 26 amygdaloidal/vesicular basalt and hyaloclastite deposited in a moraine in the southern 27 Transantarctic Mountains. 40Ar/39Ar ages from five specimens plus U-Pb ages of detrital zircon 28 from glacial till indicate igneous activity 25-17 Ma.