Earth in Upheaval – Velikovsky
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Northern Sea Route Cargo Flows and Infrastructure- Present State And
Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources. -
Which Way Now? Economic Policy After a Decade of Upheaval
CAGE POLICY REPORT Which way now? Economic policy after a decade of upheaval A CAGE Policy Report Editor: Vera E. Troeger Production Editor: Diana Egerton-Warburton Foreword: Lord O’Donnell 1 Which way now? Economic policy after a decade of upheaval A CAGE Policy Report Editor: Vera E. Troeger Production Editor: Diana Egerton-Warburton Foreword: Lord O’Donnell Centre for Competitive Advantage in the Global Economy The University of Warwick, Coventry, CV4 7AL, UK SOCIAL MARKET FOUNDATION FIRST PUBLISHED BY The Social Market Foundation, February 2019 ISBN: 978-1-910683-41-5 11 Tufton Street, London SW1P 3QB Copyright © The Social Market Foundation, 2019 The moral right of the author(s) has been asserted. All rights reserved. Without limiting the rights under copyright reserved above, no part of this publication may be reproduced, stored or introduced into a retrieval system, or transmitted, in any form or by any means (electronic, mechanical, photocopying, recording, or otherwise), without the prior written permission of both the copyright owner and the publisher of this book. THE SOCIAL MARKET FOUNDATION The Foundation’s main activity is to commission and publish original papers by independent academic and other experts on key topics in economic and social fields, with a view to stimulating public discussion on the performance of markets and the social framework within which they operate. The Foundation is a registered charity and a company limited by guarantee. It is independent of any political party and is funded predominately through sponsorship of research and public policy debates. The views expressed in this publication are those of the authors and do not necessarily reflect the views of the ESRC or the Social Market Foundation. -
Take Three More Recent Books
Take Three more recenT books Minnesota’s Geologist: The Life of Newton Horace Winchell How Could You Do This? 50 Years by Sue Leaf (Minneapolis: University of Minnesota Press, 2020, of Property- Tax- base Sharing in 280 p., Cloth, $29.95). Newton Horace Winchell (1839–1914) ven- Minnesota by Paul Gilje (St. Paul, tured with his crew throughout the state as head of the Minnesota MN: Center for Policy Design, 2021, Geological and Natural History Survey, charting the prehistory 192 p., Paper, $9.99). Policy wonks of the region, its era of inland seas, its volcanic activity, and will concur with the word “drama” its several ice ages, laying the foundation for the monumental used by the publisher to describe the five-volume Geology of Minnesota. Winchell grew up in North half- century history of Minnesota’s East, New York, near Winchell Mountain, named for the family property tax- base sharing law (more who lived in the area for almost a century. Maturing from a 15-year-old schoolteacher popularly known as the metropolitan who knew nothing about rocks to a 17-year-old who moved himself to Ann Arbor, fiscal disparities law) that began in Michigan, for higher education, Winchell at age 25 dedicated himself to geological 1968 with extensive controversy and scientific inquiry. His passionate and adventurous life story, told for the first time extends to the present day. A group of by environmental historian Sue Leaf, guides readers through the geologic history of bipartisan legislators created a more the state. Winchell strove for his work to be accessible to the nonprofessional and equitable way for municipalities of expanded his efforts to include mentoring young geologists, founding the American varying levels of wealth to compete Geological Society, and being the founding editor of American Geologist, the first jour- for tax revenues. -
69-22,173 MARKOWITZ, Allan Henry, 1941- a STUDY of STARS
This dissertation has been microfilmed exactly u received 6 9 -2 2 ,1 7 3 MARKOWITZ, Allan Henry, 1941- A STUDY OF STARS EXHIBITING COM POSITE SPECTRA. The Ohio State University, Ph.D., 1969 A stron om y University Microfilms, Inc., Ann Arbor, Michigan A STUDY OF STARS EXHIBITING COMPOSITE SPECTRA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Allan Henry Markowitz, A.B., M.Sc. ******** The Ohio S ta te U n iv e rsity 1969 Approved by UjiIjl- A dviser Department of Astronomy ACKNOWLEDGMENTS It is a sincere pleasure to thank my adviser, Professor Arne Slettebak, who originally suggested this problem and whose advice and encouragement were indispensable throughout the course of the research. I am also greatly indebted to Professor Philip Keenan for help in classifying certain late-type spectra and to Professor Terry Roark for instructing me in the operation of the Perkins Observatory telescope, I owe a special debt of gratitude to Dr. Carlos Jaschek of the La Plata Observatory for his inspiration, advice, and encourage ment. The Lowell Observatory was generous in providing extra telescope time when the need arose. I wish to particularly thank Dr. John Hall for this and for his interest. I also gratefully acknowledge the assistance of the Perkins Observatory staff. To my wife, Joan, I owe my profound thanks for her devotion and support during the seemingly unending tenure as a student. I am deeply grateful to my mother for her eternal confidence and to my in-laws for their encouragement. -
USCGC Glacier (WAGB-4)
NATIONAL REGISTER ELIGIBILITY ASSESSMENT VESSEL: USS Glacier (AGB-4) USCGC Glacier (WAGB-4) USCGC Glacier underway circa 1966-1972. Photo courtesy of U.S. Coast Guard. The icebreaker Glacier. Vessel History The former U.S. Coast Guard Cutter Glacier is an oceangoing icebreaker that was originally designed and constructed for the U.S. Navy in the mid-1950s. In 1966, Glacier was transferred to the Coast Guard. Ingalls Shipbuilding in Pascagoula, Mississippi began constructing the icebreaker in August 1953 and delivered the ship to the U.S. Navy in May 1955. It was named for Glacier Bay, Alaska, and was the fourth ship to carry this name. After its initial shakedown cruise, Glacier sailed from its homeport of Boston, Massachusetts as Admiral Richard E. Byrd’s flagship bound for the Antarctic as part of Operation Deep Freeze I1 in late 1955. It reached the 1 Operation Deep Freeze I was the codename for a series of scientific expeditions to Antarctica in 1955-56. The impetus behind the expeditions was the International Geophysical Year 1957-58. IGY was a collaborative effort of 40 nations to study the North and South Poles and points in between. Their goal was to advance knowledge of Antarctic hydrography and weather systems, glacial movements, and marine life. The U.S. Navy was charged with supporting the U.S. scientists for their portion of the IGY studies. 2 Ross Ice Pack in December where it smashed through thick ice “carving” out a harbor in Kainan Bay for ships delivering materials, supplies, and labor for the construction of Little America V.2 After clearing a channel and leading a group of ships to Kainan Bay, Glacier headed toward the Ross Ice Shelf to assist in the construction of a naval air station at McMurdo Sound. -
Equity in Education Thematic Review
EQUITY IN EDUCATION THEMATIC REVIEW COUNTRY ANALYTICAL REPORT FINLAND Finnish Ministry of Education Mars 2005 TABLE OF CONTENTS SECTION 1: COUNTRY CONTEXT AND CURRENT EQUITY SITUATION .................................. 4 CHAPTER 1. CULTURAL AND SOCIAL FACTORS................................................................................ 4 1.1. Historical background..................................................................................................................... 4 1.2. Comprehensive school.................................................................................................................... 4 1.3. Confidence in the significance of education................................................................................... 5 1.4. Teachers’ social prestige................................................................................................................. 5 1.5. Social and cultural homogeneity..................................................................................................... 5 CHAPTER 2. THE EDUCATION SYSTEM IN FINLAND......................................................................... 6 2.1. Pre-primary education..................................................................................................................... 6 2.2. Comprehensive school (basic education)........................................................................................ 7 2.3. Secondary education...................................................................................................................... -
Asymmetric Terracing of Lunar Highland Craters: Influence of Pre-Impact Topography and Structure
Proc. L~lnorPli~nel. Sci. Corrf. /Of11 (1979), p. 2597-2607 Printed in the United States of America Asymmetric terracing of lunar highland craters: Influence of pre-impact topography and structure Ann W. Gifford and Ted A. Maxwell Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institition, Washington, DC 20560 Abstract-The effects of variable pre-impact topography and substrate on slumping and terrace for- mation have been studied on a group of 30 craters in the lunar highlands. These craters are charac- terized by a distinct upper slump block and are all situated on the rim of a larger, older crater or a degraded rim segment. Wide, isolated terraces occur where the rim of the younger crater coincides with a rim segment of the older crater. The craters are all located in Nectarianlpre-Nectarian highland units, and range in age from Imbrian to Copernican. A proposed model for formation of slump blocks in these craters includes the existence of layers with different competence in an overturned rim of the pre-existing crater. Such layering could have resulted from overturning of more coherent layers during formation of the Nectarian and pre-Nec- tarian craters. A combination of material and topographic effects is therefore responsible for terrace formation. Similar terrain effects may be present on other planets and should be considered when interpreting crater statistics in relation to morphology. INTRODUCTION Slumping, terracing or wall failure is an important process in formation and mod- ification of lunar craters. The process of slumping has been investigated by both geometrical (Cintala et a1 ., 1977) and theoretical models (Melosh, 1977; Melosh and McKinnon, 1979); however, these studies are dependent on morphologic constraints imposed by the geologic setting of the craters. -
Geologic History of Minnesota Rivers
GEOLOGIC HISTORY OF MINNESOTA RIVERS Minnesota Geological Survey Ed ucational Series - 7 Minnesota Geological Survey Priscilla C. Grew, Director Educational Series 7 GEOLOGIC HISTORY OF MINNESOTA RIVERS by H.E. Wright, Jr. Regents' Professor of Geology, Ecology, and Botany (Emeritus), University of Minnesota 'r J: \ I' , U " 1. L I!"> t) J' T II I ~ !oo J', t ' I' " I \ . University of Minnesota St. Paul, 1990 Cover: An early ponrayal of St. Anthony Falls on the Mississippi River In Minneapolis. The engraving of a drawing by Captain E. Eastman of Fan Snelling was first published In 1853; It Is here reproduced from the Second Final Report of the Geological and Natural History Survey of Minnesota, 1888. Several other early views of Minnesota rivers reproduced In this volume are from David Dale Owen's Report of a Geological Survey of Wisconsin, Iowa, and Minnesota; and Incidentally of a portion of Nebraska Territory, which was published In 1852 by Lippincott, Grambo & Company of Philadelphia. ISSN 0544-3083 1 The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age, veteran status, or sexual orientation. 1-' \ J. I,."l n 1 ~ r 1'11.1: I: I \ 1"" CONTENTS 1 .... INTRODUCTION 1. PREGLACIAL RIVERS 5 .... GLACIAL RIVERS 17 ... POSTGLACIAL RIVERS 19 . RIVER HISTORY AND FUTURE 20 . ... REFERENCES CITED iii GEOLOGIC HISTORY OF MINNESOTA RIVERS H.E. Wright, Jr. A GLANCE at a glacial map of the Great Lakes region (Fig. 1) reveals that all of Minnesota was glaciated at some time, and all but the southeastern and southwestern corners were covered by the last ice sheet, which culminated about 20,000 years ago. -
John Mason Clarke
NATIONAL ACADEMY OF SCIENCES BIOGRAPHICAL MEMOIRS VOLUME XII'—SIXTH MEMOIR BIOGRAPHICAL MEMOIR OF JOHN MASON CLARKE BY CHARLES SCHUCHERT PRESENTED TO THE ACADEMY AT THE ANNUAL MEETING, 1926 JOHN MASON CLARKE BY CHARLES SCIIUCHERT In the death of John Mason Clarke, America loses its most brilliant, eloquent, and productive paleontologist, and the world its greatest authority on Devonian life and time. Author of more than 10,000 printed pages, distributed among about 450 books and papers, of which 300 deal with Geology, his efforts had to do mostly with pure science, and he often lamented, in the coming generation of doers, the lack of an adequate apprecia- tion of wondrous nature as recorded on the tablets of the earth's crust. He was peculiarly the child of his environment; born on Devonian rocks replete with fossils, in a home of high ideals and learning, situated in a state that has long appreciated science, he rose into the grandeur of geologic knowledge that was his. Clarke is survived by his wife, formerly Mrs. Fannie V. Bosler, of Philadelphia; by Noah T. Clarke, a son by his first wife, who was Mrs. Emma Sill (nee Juel), of Albany; by two stepdaughters, Miss Marie Bosler and Mrs. Edith (Sill) Humphrey, and a stepson, Mr. Frank N. Sill. Out of a family of six brothers and sisters, four remain to mourn his going: Miss Clara Mason Clarke, who, with Mr. S. Merrill Clarke, for many years city editor of the New York Sun, is living in the old homestead at Canandaigua ; Rev. Lorenzo Mason Clarke, pastor of the First Presbyterian Church of Brooklyn; and Mr. -
Appendix a Recovery of Ejecta Material from Confirmed, Probable
Appendix A Recovery of Ejecta Material from Confirmed, Probable, or Possible Distal Ejecta Layers A.1 Introduction In this appendix we discuss the methods that we have used to recover and study ejecta found in various types of sediment and rock. The processes used to recover ejecta material vary with the degree of lithification. We thus discuss sample processing for unconsolidated, semiconsolidated, and consolidated material separately. The type of sediment or rock is also important as, for example, carbonate sediment or rock is processed differently from siliciclastic sediment or rock. The methods used to take and process samples will also vary according to the objectives of the study and the background of the investigator. We summarize below the methods that we have found useful in our studies of distal impact ejecta layers for those who are just beginning such studies. One of the authors (BPG) was trained as a marine geologist and the other (BMS) as a hard rock geologist. Our approaches to processing and studying impact ejecta differ accordingly. The methods used to recover ejecta from unconsolidated sediments have been successfully employed by BPG for more than 40 years. A.2 Taking and Handling Samples A.2.1 Introduction The size, number, and type of samples will depend on the objective of the study and nature of the sediment/rock, but there a few guidelines that should be followed regardless of the objective or rock type. All outcrops, especially those near industrialized areas or transportation routes (e.g., highways, train tracks) need to be cleaned off (i.e., the surface layer removed) prior to sampling. -
Geochemistry of Darwin Glass and Target Rocks from Darwin Crater, Tasmania, Australia
Meteoritics & Planetary Science 43, Nr 3, 479–496 (2008) AUTHOR’S Abstract available online at http://meteoritics.org PROOF Geochemistry of Darwin glass and target rocks from Darwin crater, Tasmania, Australia Kieren T. HOWARD School of Earth Sciences, University of Tasmania, Hobart, Tasmania 7000, Australia Present address: Impacts and Astromaterials Research Centre, Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK Corresponding author. E-mail: [email protected] (Received 1 March 2007; revision accepted 25 July 2007) Abstract–Darwin glass formed about 800,000 years ago in western Tasmania, Australia. Target rocks at Darwin crater are quartzites and slates (Siluro-Devonian, Eldon Group). Analyses show 2 groups of glass, Average group 1 is composed of: SiO2 (85%), Al2O3 (7.3%), TiO2 (0.05%), FeO (2.2%), MgO (0.9%), and K2O (1.8%). Group 2 has lower average SiO2 (81.1%) and higher average Al2O3 (8.2%). Group 2 is enriched in FeO (+1.5%), MgO (+1.3%) and Ni, Co, and Cr. Average Ni (416 ppm), Co (31 ppm), and Cr (162 ppm) in group 2 are beyond the range of sedimentary rocks. Glass and target rocks have concordant REE patterns (La/Lu = 5.9–10; Eu/Eu* = 0.55–0.65) and overlapping trace element abundances. 87Sr/86Sr ratios for the glasses (0.80778–0.81605) fall in the range (0.76481–1.1212) defined by the rock samples. ε-Nd results range from −13.57 to −15.86. Nd model ages range from 1.2–1.9 Ga (CHUR) and the glasses (1.2–1.5 Ga) fall within the range defined by the target samples. -
Apollo 17 Index
Preparation, Scanning, Editing, and Conversion to Adobe Portable Document Format (PDF) by: Ronald A. Wells University of California Berkeley, CA 94720 May 2000 A P O L L O 1 7 I N D E X 7 0 m m, 3 5 m m, A N D 1 6 m m P H O T O G R A P H S M a p p i n g S c i e n c e s B r a n c h N a t i o n a l A e r o n a u t i c s a n d S p a c e A d m i n i s t r a t i o n J o h n s o n S p a c e C e n t e r H o u s t o n, T e x a s APPROVED: Michael C . McEwen Lunar Screening and Indexing Group May 1974 PREFACE Indexing of Apollo 17 photographs was performed at the Defense Mapping Agency Aerospace Center under the direction of Charles Miller, NASA Program Manager, Aerospace Charting Branch. Editing was performed by Lockheed Electronics Company, Houston Aerospace Division, Image Analysis and Cartography Section, under the direction of F. W. Solomon, Chief. iii APOLLO 17 INDEX 70 mm, 35 mm, AND 16 mm PHOTOGRAPHS TABLE OF CONTENTS Page INTRODUCTION ................................................................................................................... 1 SOURCES OF INFORMATION .......................................................................................... 13 INDEX OF 16 mm FILM STRIPS ........................................................................................ 15 INDEX OF 70 mm AND 35 mm PHOTOGRAPHS Listed by NASA Photograph Number Magazine J, AS17–133–20193 to 20375.........................................