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The Roots of Middle-Earth: William Morris's Influence Upon J. R. R. Tolkien
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 12-2007 The Roots of Middle-Earth: William Morris's Influence upon J. R. R. Tolkien Kelvin Lee Massey University of Tennessee - Knoxville Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Literature in English, British Isles Commons Recommended Citation Massey, Kelvin Lee, "The Roots of Middle-Earth: William Morris's Influence upon J. R. R. olkien.T " PhD diss., University of Tennessee, 2007. https://trace.tennessee.edu/utk_graddiss/238 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Kelvin Lee Massey entitled "The Roots of Middle-Earth: William Morris's Influence upon J. R. R. olkien.T " I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in English. David F. Goslee, Major Professor We have read this dissertation and recommend its acceptance: Thomas Heffernan, Michael Lofaro, Robert Bast Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council: I am submitting herewith a dissertation written by Kelvin Lee Massey entitled “The Roots of Middle-earth: William Morris’s Influence upon J. -
Sulphur Isotope Geochemistry of the Ores and Country Rocks at the Almadcn Mercury Deposit, Ciudad Real, Spain*
Gemhimrca 0 Comochmica Acln Vol. 56, pp. 3765-3780 OOl6-7037/92/$5.00 + 00 Copyright 0 1992 PerpamonPress Ltd. Printed tn U.S.A. Sulphur isotope geochemistry of the ores and country rocks at the AlmadCn mercury deposit, Ciudad Real, Spain* FRANCIS SAUP~~and MICHEL ARNOLD Centre de Recherches Pstrographiques et GCochimiques, BP 20, 54501 Vandoeuvre-l&s-NancyCedex. France (Received June 7, 1991: accepted in revised form April 15, 1992) Abst~ct-Seventy-four new S isotope analyses of ore minerals and country rocks are given for the Hg deposit of Almad&. The spread of the cinnabar &34Sis narrow within each of the three orebodies, but the 634S average values differ sufficiently between them (mean 634S: San Nicolas = 0.2 rt I. l%, San Francisco = 8.1 + 0.7%0, San Pedro = 5.9 f 1.0%0) to indicate three different mineralization episodes and possibly processes. The unweighted mean for all cinnabar samples is 5.6%0 and the S source is considered to be the host-rocks, either the Footwall Shales (634S = 5.5%0) or the spilites (S34S = 5.1 rt 1.3%0). For geometric and chronologic reasons, the former seem the best potential source. However, the high ?js4S values of the San Francisco cinnabar cannot be explained without addition of heavy S from reduction of seawater sulphate. Orderly distributions ofthe 634Svalues are observed in all three orebodies: ( 1) their increase from the stratigraphic bottom to the top in the San Pedro orebody is explained by a Rayleigh process, and (2) the maxima in the centres of the San Francisco and San Nicolas orebodies are explained by mixing of the S transporting hydrothermal fluids with seawater within the sediments. -
Submerged Shorelines and Shelves in the Hawaiian Islands and a Revision of Some of the Eustatic Emerged Shorelines
HAROLD T. STEARNS Hawaii Institute of Geophysics, University of Hawaii, 2525 Correa Road, Honolulu, Hawaii 96822 Submerged Shorelines and Shelves in the Hawaiian Islands and a Revision of Some of the Eustatic Emerged Shorelines ABSTRACT IS8°| 00' KAHUKU POINT __ .Type locality of Kawelo low stand The paper presents new C14 and uran.um series dates on Oahu and their bearing on 0 A H U the dating of fluctuations of sea level dm: to glacioeustatism during the Wisconsinan. The — 60- and — 120-ft shorelines are shown to be Wisconsinan. Scuba and sub- mersible diving has made it possible to study the submerged shorelines. Some of the submerged shorelines are notches in vertical cliffs and were not previously found , KAPAPA ISLAND - by detailed soundings. The —350-ft shelf, \J /¡/ Jk .Konoohe -80ft.shore line previously thought to be a drowned wave- • /^^KEKEPA ISLAND cut platform, proved to be a drowned coral v ULUPAU CRATER reef. Shorelines and drowned reefs indicate r^w « stillstands below sea level at 15, 30, 60, 80, •POPOIA ISLAND 120, 150, 185, 205, 240±, 350, 1,200 to aimanalo shore 1,800, and 3,000 to 3,600 ft. Those above line and Bellows —450 ft are thought to be glacioeustatic. \ Field formation \ MANANA ISLANO Those below —450 ft are the result of sub- Ni«^MoKai Ronge sidence. Key words: Quaternary, -60 ft. and Makapuu -120ft dune limestone, geomorphology, geo- shore lines cbronology. Honaumo Bo/ Koko-l5ft. shelf SLACK PT. KOKO HEAD INTRODUCTION •Type locality of Leahi I shore line All submerged shorelines described Figure 1. -
Topographic History of the Maui Nui Complex, Hawai'i, and Its Implications for Biogeography1
Topographic History ofthe Maui Nui Complex, Hawai'i, and Its Implications for Biogeography 1 Jonathan Paul Price 2,4 and Deborah Elliott-Fisk3 Abstract: The Maui Nui complex of the Hawaiian Islands consists of the islands of Maui, Moloka'i, Lana'i, and Kaho'olawe, which were connected as a single landmass in the past. Aspects of volcanic landform construction, island subsi dence, and erosion were modeled to reconstruct the physical history of this complex. This model estimates the timing, duration, and topographic attributes of different island configurations by accounting for volcano growth and subsi dence, changes in sea level, and geomorphological processes. The model indi cates that Maui Nui was a single landmass that reached its maximum areal extent around 1.2 Ma, when it was larger than the current island of Hawai'i. As subsi dence ensued, the island divided during high sea stands of interglacial periods starting around 0.6 Ma; however during lower sea stands of glacial periods, islands reunited. The net effect is that the Maui Nui complex was a single large landmass for more than 75% of its history and included a high proportion of lowland area compared with the contemporary landscape. Because the Hawaiian Archipelago is an isolated system where most of the biota is a result of in situ evolution, landscape history is an important detertninant of biogeographic pat terns. Maui Nui's historical landscape contrasts sharply with the current land scape but is equally relevant to biogeographical analyses. THE HAWAIIAN ISLANDS present an ideal logic histories that can be reconstructed more setting in which to weigh the relative influ easily and accurately than in most regions. -
Hawaiian Volcanoes: from Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012
AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012 Conveners Michael Poland, USGS – Hawaiian Volcano Observatory, USA Paul Okubo, USGS – Hawaiian Volcano Observatory, USA Ken Hon, University of Hawai'i at Hilo, USA Program Committee Rebecca Carey, University of California, Berkeley, USA Simon Carn, Michigan Technological University, USA Valerie Cayol, Obs. de Physique du Globe de Clermont-Ferrand Helge Gonnermann, Rice University, USA Scott Rowland, SOEST, University of Hawai'i at M noa, USA Financial Support 2 AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Meeting At A Glance Sunday, 19 August 2012 1600h – 1700h Welcome Reception 1700h – 1800h Introduction and Highlights of Kilauea’s Recent Eruption Activity Monday, 20 August 2012 0830h – 0900h Welcome and Logistics 0900h – 0945h Introduction – Hawaiian Volcano Observatory: Its First 100 Years of Advancing Volcanism 0945h – 1215h Magma Origin and Ascent I 1030h – 1045h Coffee Break 1215h – 1330h Lunch on Your Own 1330h – 1430h Magma Origin and Ascent II 1430h – 1445h Coffee Break 1445h – 1600h Magma Origin and Ascent Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Origin and Ascent III 1645h – 1900h Poster Session Tuesday, 21 August 2012 0900h – 1215h Magma Storage and Island Evolution I 1215h – 1330h Lunch on Your Own 1330h – 1445h Magma Storage and Island Evolution II 1445h – 1600h Magma Storage and Island Evolution Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Storage -
Wayne P. Barnett Principal Consultant
Resume Wayne P. Barnett Principal Consultant Profession Principal Structural Geologist Education Doctor of Philosophy in the School of Geological Sciences, University of KwaZulu-Natal, South Africa, 2007 Master of Science in Structural/Engineering Geology, University of Cape Town, South Africa, 1997 Certificate in Rock Mechanics, Chamber of Mines of South Africa, 2002. Bachelor of Science with Honours in Geology, University of Cape Town, 1995 Registrations/ Professional Geologist (APEGBC #43273), Professional Affiliations Natural Scientist (SACNASP #400237/04) Specialisation Structural Geology; Kimberlite Geology; Engineering Geology; 3D Computer-based Geological Modelling and GIS. Expertise Wayne is a Principal Consultant with 24 years of experience in the mining and exploration industry. He has been employed over a period of eight years as a mining operations-based geotechnical engineer and applied structural geologist. Subsequently, Wayne has performed the role of consulting structural geology specialist in mining and exploration in Africa, North America, South America and Asia. Consequently he specialises in defining the structural geology of mining projects in order to properly characterize the rock mass for geotechnical engineering applications - for scoping to pre-feasibility studies, as well as problem-solving in active mining operations. Wayne is a geological modelling expert and undertakes and provides training in structural and geotechnical drill core logging, open pit and underground mapping, geological data management, data QA/QC, and statistical analysis of structural data. He has provided formal applied structural geology training to over 1000 geologists and engineers internationally. These versatile skills have also allowed him to provide practical, goal-focussed structural consulting in diamond, precious and base metal exploration and resource characterization on numerous projects and active operations on all major mining-active continents; for understanding controls on mineralization and targeting purposes. -
THE HAWAIIAN-EMPEROR VOLCANIC CHAIN Part I Geologic Evolution
VOLCANISM IN HAWAII Chapter 1 - .-............,. THE HAWAIIAN-EMPEROR VOLCANIC CHAIN Part I Geologic Evolution By David A. Clague and G. Brent Dalrymple ABSTRACT chain, the near-fixity of the hot spot, the chemistry and timing of The Hawaiian-Emperor volcanic chain stretches nearly the eruptions from individual volcanoes, and the detailed geom 6,000 km across the North Pacific Ocean and consists of at least etry of volcanism. None of the geophysical hypotheses pro t 07 individual volcanoes with a total volume of about 1 million posed to date are fully satisfactory. However, the existence of km3• The chain is age progressive with still-active volcanoes at the Hawaiian ewell suggests that hot spots are indeed hot. In the southeast end and 80-75-Ma volcanoes at the northwest addition, both geophysical and geochemical hypotheses suggest end. The bend between the Hawaiian and .Emperor Chains that primitive undegassed mantle material ascends beneath reflects a major change in Pacific plate motion at 43.1 ± 1.4 Ma Hawaii. Petrologic models suggest that this primitive material and probably was caused by collision of the Indian subcontinent reacts with the ocean lithosphere to produce the compositional into Eurasia and the resulting reorganization of oceanic spread range of Hawaiian lava. ing centers and initiation of subduction zones in the western Pacific. The volcanoes of the chain were erupted onto the floor of the Pacific Ocean without regard for the age or preexisting INTRODUCTION structure of the ocean crust. Hawaiian volcanoes erupt lava of distinct chemical com The Hawaiian Islands; the seamounts, hanks, and islands of positions during four major stages in their evolution and the Hawaiian Ridge; and the chain of Emperor Seamounts form an growth. -
Kimberlite Wall Rock Fragmentation Processes: Venetia K08 Pipe Development
1 Kimberlite Wall Rock Fragmentation Processes: Venetia K08 Pipe Development The final publication is available at www.springerlink.com - 10.1007/s00445-011-0499-3 W.P. Barnett (1,2) , S. Kurszlaukis (3), M. Tait (1), P. Dirks (4) (1) Mineral Resources Management, De Beers Group Services, P/Bag X01, Southdale 2135, South Africa (2) present address: SRK Consulting, Suite 2200, 1066 West Hastings Street, Vancouver V6E3X2, BC, Canada ([email protected]; +17782388038) (3) Kimberlite Petrology Unit, De Beers Canada Inc., Toronto, Ontario, Canada (4) School of Earth and Environmental Sciences, James Cook University, Townsville, Australia Abstract Current kimberlite pipe development models strongly advocate a downward growth process with the pipe cutting down onto its feeder dyke by means of volcanic explosions. Evidence is presented from the K08 kimberlite pipe in Venetia Mine, South Africa, which suggests that some pipes or sub-components of pipes develop upwards. The K08 pipe in pit exposure comprises >90 vol.% chaotic mega-breccia of country rock clasts (gneiss and schist) and <10 vol.% coherent kimberlite. Sub-horizontal breccia layers, tens of metres thick, are defined by lithic clast size variations, and contain zones of shearing and secondary fragmentation. Textural studies of the breccias and fractal statistics on clast size distributions are used to characterize sheared and non-sheared breccia zones, and to deduce a fragmentation mechanism. Breccia statistics are compared directly with the statistics of fragmented rock produced from mining processes in order to support interpretations. Results are consistent with an initial stage of brecciation formed by upward-moving collapse of an explosively pre-conditioned hangingwall into a subterranean volcanic excavation. -
Treasures of Middle Earth
T M TREASURES OF MIDDLE-EARTH CONTENTS FOREWORD 5.0 CREATORS..............................................................................105 5.1 Eru and the Ainur.............................................................. 105 PART ONE 5.11 The Valar.....................................................................105 1.0 INTRODUCTION........................................................................ 2 5.12 The Maiar....................................................................106 2.0 USING TREASURES OF MIDDLE EARTH............................ 2 5.13 The Istari .....................................................................106 5.2 The Free Peoples ...............................................................107 3.0 GUIDELINES................................................................................ 3 5.21 Dwarves ...................................................................... 107 3.1 Abbreviations........................................................................ 3 5.22 Elves ............................................................................ 109 3.2 Definitions.............................................................................. 3 5.23 Ents .............................................................................. 111 3.3 Converting Statistics ............................................................ 4 5.24 Hobbits........................................................................ 111 3.31 Converting Hits and Bonuses...................................... 4 5.25 -
The Philippines Illustrated
The Philippines Illustrated A Visitors Guide & Fact Book By Graham Winter of www.philippineholiday.com Fig.1 & Fig 2. Apulit Island Beach, Palawan All photographs were taken by & are the property of the Author Images of Flower Island, Kubo Sa Dagat, Pandan Island & Fantasy Place supplied courtesy of the owners. CHAPTERS 1) History of The Philippines 2) Fast Facts: Politics & Political Parties Economy Trade & Business General Facts Tourist Information Social Statistics Population & People 3) Guide to the Regions 4) Cities Guide 5) Destinations Guide 6) Guide to The Best Tours 7) Hotels, accommodation & where to stay 8) Philippines Scuba Diving & Snorkelling. PADI Diving Courses 9) Art & Artists, Cultural Life & Museums 10) What to See, What to Do, Festival Calendar Shopping 11) Bars & Restaurants Guide. Filipino Cuisine Guide 12) Getting there & getting around 13) Guide to Girls 14) Scams, Cons & Rip-Offs 15) How to avoid petty crime 16) How to stay healthy. How to stay sane 17) Do’s & Don’ts 18) How to Get a Free Holiday 19) Essential items to bring with you. Advice to British Passport Holders 20) Volcanoes, Earthquakes, Disasters & The Dona Paz Incident 21) Residency, Retirement, Working & Doing Business, Property 22) Terrorism & Crime 23) Links 24) English-Tagalog, Language Guide. Native Languages & #s of speakers 25) Final Thoughts Appendices Listings: a) Govt.Departments. Who runs the country? b) 1630 hotels in the Philippines c) Universities d) Radio Stations e) Bus Companies f) Information on the Philippines Travel Tax g) Ferries information and schedules. Chapter 1) History of The Philippines The inhabitants are thought to have migrated to the Philippines from Borneo, Sumatra & Malaya 30,000 years ago. -
Airborne and Ground Electrical Surveys of the Edwards and Trinity Aquifers, Medina, Uvalde, and Bexar Counties, Texas
43 Airborne and Ground Electrical Surveys of the Edwards and Trinity Aquifers, Medina, Uvalde, and Bexar Counties, Texas By Bruce D Smith1, David V. Smith1, Jeffrey G. Paine2, and Jared D. Abraham1 1U.S. Geological Survey, MS 964, Box 25046, Denver Federal Center, Denver, CO 80225, 2Bureau of Economic Geology, Jackson School of Geological Sciences, The University of Texas at Austin, Univ. Station, Box X, Austin, TX 78713 ABSTRACT Helicopter electromagnetic (HEM) and magnetic surveys were flown in the Seco Creek area, (Medina and Uvalde Counties, TX, 2002) and in Northern Bexar County (TX, 2003). The purpose of these surveys was to map structure and lithology of the Edwards and Trinity aquifers consisting of the catchment zone (Glen Rose, Trinity Group), recharge zone (Devils River, Edwards Group), and confined zone. The latter survey concentrated on Camps Stanley and Bullis, which are located mostly on the Glenn Rose. The south- ern part of Camp Bullis includes the faulted contact between the Edwards Group (recharge zone) and the catchment (Glenn Rose). Ground geophysical surveys at Seco Creek, conducted by the USGS in April 2002, consisted of total field magnetics, dc resistivity and shallow terrain conductivity measurements. In May 2003, BEG (Bureau of Economic Geology) acquired ground electrical conductivity measurements at 379 locations. Re-mapping of the geology along the nine geophysical lines was done at the same time. The shallow ground conductivity interpretations were supplemented by time domain EM (TDEM) soundings by the USGS. Ground-based measurements demonstrate that (a) mapped geologic units consisting of Cretaceous age limestones and dolomitized limestones, marls, mudstones, shales, and Quaternary alluvial deposits have differences in apparent conductivity, (b) geologic structures such as faults and karst can have detectable apparent conduc- tivity signatures, and (c) conductivity measurements can be combined with geologic maps and outcrop stud- ies to identify hidden contacts, covered strata, and unmapped structural features. -
Humpback Whale Tagging in Hawaii
Submitted in support of the U.S. Navy’s 2019 Annual Marine Species Monitoring Report for the Pacific Humpback Whale Tagging in Support of Marine Mammal Monitoring Across Multiple Navy Training Areas in the Pacific Ocean: Preliminary Summary of Field Tagging Effort in Hawaii in March 2019 Prepared for: Commander, U.S. Pacific Fleet, and Commander, Naval Sea Systems Command Submitted to: Naval Facilities Engineering Command, Southwest under Cooperative Ecosystem Studies Unit, Department of the Navy Cooperative Agreement No. N62473‐19‐2‐0002 Prepared by: Bruce R. Mate, Daniel M. Palacios, C. Scott Baker, Barbara A. Lagerquist, Ladd M. Irvine, Tomas M. Follett, Debbie Steel, and Craig E. Hayslip Oregon State University, Marine Mammal Institute Hatfield Marine Science Center 2030 SE Marine Science Drive Newport, OR 97365 15 August 2019 Submitted in support of the U.S. Navy’s 2019 Annual Marine Species Monitoring Report for the Pacific Suggested Citation: Mate, B.R., D.M. Palacios, C.S. Baker, B.A. Lagerquist, L.M. Irvine, T.M. Follett, D. Steel, and C.E. Hayslip. 2019. Humpback Whale Tagging in Support of Marine Mammal Monitoring Across Multiple Navy Training Areas in the Pacific Ocean: Preliminary Summary of Field Tagging Effort in Hawaii in March 2019. Prepared for Commander, U.S. Pacific Fleet, and Commander, Naval Sea Systems Command. Submitted to Naval Facilities Engineering Command, Southwest, under Cooperative Ecosystem Studies Unit, Department of the Navy Cooperative Agreement No. N62473‐19‐2‐0002. Oregon State University, Newport, Oregon, 15 August 2019. 14 pp. ii Submitted in support of the U.S. Navy’s 2019 Annual Marine Species Monitoring Report for the Pacific Form Approved REPORT DOCUMENTATION PAGE OMB No.