Coding Manual 5.0
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
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. -
Tuyas: a Descriptive Genetic Classification
Dickinson College Dickinson Scholar Faculty and Staff Publications By Year Faculty and Staff Publications 3-2014 Tuyas: A Descriptive Genetic Classification J.K. Russell Benjamin R. Edwards Dickinson College Lucy Porritt C. Ryane Follow this and additional works at: https://scholar.dickinson.edu/faculty_publications Part of the Environmental Sciences Commons, Glaciology Commons, and the Volcanology Commons Recommended Citation Russell, J.K., B.R. Edwards, Lucy Porritt, and C. Ryane. "Tuyas: A Descriptive Genetic Classification." Quaternary Science Reviews 87 (2014): 70-81. https://www.sciencedirect.com/science/article/pii/ S027737911400002X This article is brought to you for free and open access by Dickinson Scholar. It has been accepted for inclusion by an authorized administrator. For more information, please contact [email protected]. Quaternary Science Reviews 87 (2014) 70e81 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Tuyas: a descriptive genetic classification J.K. Russell a,*, B.R. Edwards b, Lucy Porritt a,c, C. Ryane a a Volcanology & Petrology Laboratory, Department of Earth, Ocean & Atmospheric Sciences, University of British Columbia, Vancouver V6T 1Z4, Canada b Department of Earth Sciences, Dickinson College, Carlisle, PA 17013, USA c School of Earth Sciences, University of Bristol, Bristol, UK article info abstract Article history: We present a descriptive genetic classification scheme and accompanying nomenclature for glacio- Received 23 June 2013 volcanic edifices herein defined as tuyas: positive-relief volcanoes having a morphology resulting from ice Received in revised form confinement during eruption and comprising a set of lithofacies reflecting direct interaction between magma 23 December 2013 and ice/melt water. -
2014 Department Newsletter
Earth Sciences Newsletter 2014 The Dickin-stone-ian Department of Earth Sciences Participates in Baffin Island Field Trip by Marcus Key Thanks to the generosity of John (GEOL ‘78) and Susan Pohl (‘80), Professor Marcus Key, Liz Plascencia (ERSC ‘16), Melanie Campbell (ERSC ‘15), Leslie Milliman (ERSC ‘14) and Aleks Perpalaj (ERSC ‘14) were able to participate in an 11 day trip to Baffin Island to experience the geologic wonders of the Canadian high Arctic. In early August 2013, we set up two base camps by boat from Pond Inlet on Baffin Island at 73 degrees North latitude. The first was on Bylot Island where we did day hikes to Cretaceous sandstone outcrops (DSCN2094) and the Sirmilik glacier. The second was on Curry Island where we sea kayaked in a fjord carved into Precambrian metamorphics (DSCN2332) with narwhals. There were many firsts for us: first 24 hour daylight, first fresh polar bear tracks, first narwhals, first time sea kayaking in a fjord, and first time sea Kayaking around an iceberg. For additional photos of the trip visit our website. http://www.dickinson.edu/galleries/gallery/167/ baffin_island_field_trip Inside this issue: Department and Campus 1 News 2-7 A Letter from the Chair 4-5 Senior Research Projects 8-11 Faculty Publications 12-16 Faculty Updates 17-21 Alumni Updates 22-34 Contact Information 35 Greenland Expedition 2014 By Ben Edwards Thanks to the ongoing generosity of John (GEOL ’78) and Susan Pohl (’80), the Earth Sciences department sent another five member team (Ben Edwards, Ariana Auerbach ‘16, Katie Mattern ‘16, Amanda Santilla ‘17, Will Kochtitzky ‘16) to explore geology and climate change, this time near the second largest ice sheet on earth in Greenland. -
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. -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
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. -
Glaciovolcanic Megapillows of Undirhlíđar, Reykjanes Peninsula, Southwestern Iceland
GLACIOVOLCANIC MEGAPILLOWS OF UNDIRHLÍĐAR, REYKJANES PENINSULA, SOUTHWESTERN ICELAND Rachel Heineman Honors Research in Geology Dr. F. Zeb Page, Thesis Advisor Oberlin College 2016-2017 ABSTRACT At Undirhlíðar tindar on the Reykjanes Peninsula, southwestern Iceland, megapillows are among the features formed during a series of ridge-building glaciovolcanic eruptions. Mapping of the northeastern 3 km of the ridge and petrographic and geochemical analysis of the megapillow outcrops occurring throughout this area demonstrate their role in the multi-stage construction of the ridge modeled by Pollock et al. (2014). The outcrops exhibit radial jointing, bands of vesicles and glassy rims; they occur in high relief surrounded by basalt breccia resembling pillow rubble, and are composed of plagioclase-phyric olivine basalt with plagioclase-rich groundmass. They occur in multiple pillow lava units formed from two distinct magma batches. Two groups of outcrops are represented that are petrographically, geochemically and geographically distinct; the first group is near to and consistent with the pillow units of Undirhlíðar quarry described by Pollock et al. (2014), and the second group, located near the tephra cone, is derived from a more evolved unit of the same magma. Megapillows show significant plagioclase accumulation with variable phenocryst zoning, indicating the movement of multiple pulses of magma through the megapillows. Megapillows at Undirhlíðar may represent a significant mechanism, demonstrated elsewhere at a marine megapillow by Goto and McPhie (2004), for magmatic distribution: feeding and then overrunning pillows which propagate and are fed from their basal margins at the eruptive front. INTRODUCTION Pillow lavas are among the most common lava morphologies on Earth, yet the construction of pillow-dominated volcanoes is not widely understood due to the relative inaccessibility of the submarine environments in which they form. -
Recognizing Ice-Contact Trachyte-Phonolite Lavas at The
RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA by Kristen A. LaMoreaux B.S., Kent State University, 2002 Submitted to the Graduate Faculty of Arts and Sciences in partial fulfillment of the requirements for the degree of Master of Science University of Pittsburgh 2008 UNIVERSITY OF PITTSBURGH ARTS AND SCIENCES This thesis was presented by Kristen A. LaMoreaux It was defended on June 17, 2008 and approved by Dr. Michael Ramsey Dr. Thomas Anderson Thesis Director: Dr. Ian Skilling ii Copyright © by Kristen A. LaMoreaux 2008 iii RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA Kristen A. LaMoreaux, M.S. University of Pittsburgh, 2008 Mount Edziza Volcanic Complex (MEVC) lies within the Northern Cordilleran Volcanic Province (NCVP), in northwest British Columbia, Canada. The eruption products have been emplaced in a variety of subaerial, sub-ice and subaqueous environments from about 8Ma to less than 2000 y.b.p. (Souther, 1992). Ice Peak Formation (IPF) trachyte lava flows of approximately 1Ma age (Souther, 1992) are exposed at Ornostay Bluff (OB) and Koosick Bluff (KB). These flows comprise basal flow breccias overlain by massive conchoidally-fractured lava with large, poorly-developed columns, and local flow banding. Edziza Formation (EF) approximately 1Ma (Souther, 1992) phonolite is exposed at Triangle Dome (TD). TD can broadly be divided into an upper and lower zone. The upper zone comprises poorly-developed columns in addition to prominent jointing. In the lower zone the columns are planar and 75cm- 3m-wide in the interior of the complex grading into fan-like and curved subhorizontal columns <75cm-wide in the outer margins of the lower zone.