4Th Project Group Minutes 3Rd-5Th December 2012, Kevo Finland
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Te Tauihu O Ngā Wānanga
Tracing of old settlements and place names in a Sea Sámi region1 Marit B. Henriksen Sámi University College, Norway [email protected] Introduction The basis for this article is my work with an old land surveying document from Finnmark, in the north of Norway. The document is named Finnmarken Sorenskriveri Landmaalerprotokol, which in English would be The Landsurveying protocol of the County of Finnmark. The main objective for this presentation is to introduce some preliminary results of my work with the protocol and I will present parts of the process, as well as maps, figures and photos showing how the process turns out. About the region Finnmark is the northernmost county of Norway. Finnmark was the last area that became part of the Norwegian territory. The border between the Norwegian and Swedish area was drawn in 1751 and the border between the Norwegian and Russian area was drawn in 1826. Before the closing of the borders, several nation states were interested in this area, that is for taxation purposes. Because of this, the (mainly Sámi) population of the area had to pay taxes to at least three different nation states in periods (Denmark/Norway, Sweden and Russia). Norway was a dependency (satellite state) of Denmark from 1537 to 1814. From 1814, Norway was in union with Sweden, until Norway was declared an independent nation state in 1905. About the Sámi people and the Sámi languages The Sámi area covers parts of four different nation states, Norway, Sweden, Finland and Russia. There are ten different Sámi languages: South Sámi, Ume Sámi, Pite Sámi, Lule Sámi, North Sámi, Inari Sámi, Skolt Sámi, Akkala Sámi, Kildin Sámi and Ter Sámi. -
ALTA – City of the Northern Lights
Alta Cruise Port Events: Alta Soul & Blues Festival, May, - Norwegian National Day, 17. May - Midsummer Night, 23 June. Cruising season: All year. Midnight sun: 16 Mai – 26 July. Northern Lights: September - April. Dark season: 24 November – 18 January. Average temperature: May: 5, June: 10,5, July:14, August: 12,5 Useful links: www.visitalta.no, www.altahavn.no, www.finnmark.com Destination Alta | page 58 Alta Destination Alta Canyon - Sautso. Photo: Henriette Bismo Eilertsen Midsummer night. Photo: Paul Nilsen Cavzo Safari. Photo: Stefan Sanne Gargia Fjelstue: Maze and Cavzo Safari: Karasjok. Visit the Sami Theme Park with a guide Duration: 4 hours. Duration: 4-5 hours. who can tell you all the good stories. ATV/Quad – Safari- Experience the fabulous Alta A genuine Sami village. Here you can have a Duration: 10 hours 59 scenery. On this exclusive trip you can se the unique nature experience on the river boats to Finnmarksplateau and experience the beauty and the Alta Dam, or on a shorter trip over to the old Snowmobile Tour: wilderness. church. You will also get the Sami experience Duration: 4 hours. in Maze when the local host tells you about the (January – April) Try to drive you own Hunting for the Aurora Borealis: Sami way of life and their history. Bidos ( sami snowmobile. A professional, experienced Duration: 2 hours. traditional food) is served in the lavvo. guide will take care of your comfort and (January – April) Follow your guide who will safety throughout the entire trip. Good winter help you hunt for the Northern Lights. Enjoy the Northern Delights: equipment to keep you warm and good. -
World War II at Sea This Page Intentionally Left Blank World War II at Sea
World War II at Sea This page intentionally left blank World War II at Sea AN ENCYCLOPEDIA Volume I: A–K Dr. Spencer C. Tucker Editor Dr. Paul G. Pierpaoli Jr. Associate Editor Dr. Eric W. Osborne Assistant Editor Vincent P. O’Hara Assistant Editor Copyright 2012 by ABC-CLIO, LLC All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, except for the inclusion of brief quotations in a review, without prior permission in writing from the publisher. Library of Congress Cataloging-in-Publication Data World War II at sea : an encyclopedia / Spencer C. Tucker. p. cm. Includes bibliographical references and index. ISBN 978-1-59884-457-3 (hardcopy : alk. paper) — ISBN 978-1-59884-458-0 (ebook) 1. World War, 1939–1945—Naval operations— Encyclopedias. I. Tucker, Spencer, 1937– II. Title: World War Two at sea. D770.W66 2011 940.54'503—dc23 2011042142 ISBN: 978-1-59884-457-3 EISBN: 978-1-59884-458-0 15 14 13 12 11 1 2 3 4 5 This book is also available on the World Wide Web as an eBook. Visit www.abc-clio.com for details. ABC-CLIO, LLC 130 Cremona Drive, P.O. Box 1911 Santa Barbara, California 93116-1911 This book is printed on acid-free paper Manufactured in the United States of America To Malcolm “Kip” Muir Jr., scholar, gifted teacher, and friend. This page intentionally left blank Contents About the Editor ix Editorial Advisory Board xi List of Entries xiii Preface xxiii Overview xxv Entries A–Z 1 Chronology of Principal Events of World War II at Sea 823 Glossary of World War II Naval Terms 831 Bibliography 839 List of Editors and Contributors 865 Categorical Index 877 Index 889 vii This page intentionally left blank About the Editor Spencer C. -
Subject of the Russian Federation)
How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country. -
Iron Isotope Systematics in Arctic Rivers
1 Comptes Rendus Geoscience Achimer November-December 2015, Volume 347 (7-8), Pages 377-385 http://dx.doi.org/10.1016/j.crte.2015.04.005 http://archimer.ifremer.fr http://archimer.ifremer.fr/doc/00273/38402/ © 2015 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved. Iron isotope systematics in Arctic rivers Escoube Raphaelle 1, 2, 9, Rouxel Olivier J. 2, 3, *, Pokrovsky Oleg S. 4, 5, 6, Schroth Andrew 7, Max Holmes Robert 8, Donard Olivier F.X. 1 1 LCABIE, Université de Pau et des pays de l’Adour, CNRS UMR 525, Hélioparc, 64053 Pau, France 2 Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, MA 02543 Woods Hole, USA 3 IFREMER, REM/GM, Centre de Brest, Plouzané, France 4 Georesources and Environment Toulouse GET, UMR 5563, CNRS, Université Paul-Sabatier, 31400 Toulouse, France 5 Institute of Ecological Problems of the North, Ural Branch RAS, Arkhangelsk, Russia 6 BIO-GEO-CLIM Laboratory, Tomsk State University, Tomsk, Russia 7 Department of Geology, University of Vermont, VT05405 Burlington, USA 8 Woods Hole Research Center, 02540 Falmouth, MA, USA 9 Universität zu Köln, Institut für Geologie und Mineralogie, Zülpicher Str. 49b, 50674 Köln, Germany * Corresponding author : Olivier J. Rouxel, email address : [email protected] Abstract : The input of iron to the Arctic Ocean plays a critical role in the productivity of aquatic ecosystems and is potentially impacted by climate change. We examine Fe isotope systematics of dissolved and colloidal Fe from several Arctic and sub-Arctic rivers in northern Eurasia and Alaska. We demonstrate that the Fe isotopic (δ56Fe) composition of large rivers, such as the Ob’ and Lena, has a restricted range of δ56Fe values ca.–0.11 ± 0.13‰, with minimal seasonal variability, in stark contrast to smaller organic-rich rivers with an overall δ56Fe range from–1.7 to + 1.6‰. -
Journal of Geodesy and Geomatics Engineering
Journal of Geodesy and Geomatics Engineering Volume 3, Number 1, Jan.-June 2016 (Serial Number 4) D DAVID PUBLISHING David Publishing Company www.davidpublisher.com Publication Information: Journal of Geodesy and Geomatics Engineering is published quarterly in hard copy (ISSN 2332-8223) by David Publishing Company located at 616 Corporate Way, Suite 2-4876, Valley Cottage, NY 10989. Aims and Scope: Journal of Geodesy and Geomatics Engineering, a monthly professional academic journal, particularly emphasizes the scientific problems of geodesy, geomatics engineering and related interdisciplinary sciences. Editorial Board Members: Murat YAKAR (Turkey), Savvaidis Paraskevas (Greece), Naoufal Raissouni (Morocco), Jaroslaw Bosy (Poland), Abolghasem Sadeghi-Niaraki (Republic of Korea), Hakan Karabörk (Turkey), Greta Deruyter (Belgium), Bashkim IDRIZI (Macedonia), Mehdi Eshagh (Sweden), Željko Hećimović (Croatia), Nita Mihai-Daniel (Romania), Caius DIDULESCU (Romania), Joep Crompvoets (Belgium), Ayman F. Habib (USA), Stefania Amici (Italy), Surabuddin Mondal (Germany), Rashid Burtiev (Moldova), Doina Vasilca (Romania), Nedim Suljić (Bosnia and Hercegovina), Agnieszka Zwirowicz-Rutkowska (Poland). Manuscripts and correspondence are invited for publication. You can submit your papers via web submission, or E-mail to [email protected], [email protected], [email protected]. Submission guidelines and web submission system are available at http://www.davidpublisher.com. Editorial Office: 616 Corporate Way, Suite -
Our. Knowledge of the Geology of the Alta District of West Finnmark Owes Much to the Work of Holtedahl (1918, 1960) and Føyn (1964)
Correlation of Autochthonous Stratigraphical Sequences in the Alta-Repparfjord Region, West Finnmark DAVID ROBERTS & EIGILL FARETH Roberts, D. & Fareth, E.: Correlation of autochthonous stratigraphical se quences in the Alta-Repparfjord region, west Finnmark. Norsk Geologisk Tidsskrift, Vol. 54, pp. 123-129. Oslo 1974. An outline of the geology of the area between Alta and the Komagfjord tectonic window is presented. Lithologies (including a tillite) constituting an autochthonous sequence are described from an area on the north-east side of Altafjord, and from their similarity to those of formations occurring in adjacent areas a revised regional stratigraphical correlation is proposed. An occurrence of biogenic structures appears to provide confirmatory evidence for an earlier suggested correlation with Late Precambrian sequences be tween west and east Finnmark. D. Roberts & E. Fareth, Norges Geologiske Undersøkelse, Postboks 3006, 7001 Trondheim, Norway. Regional setting; previous correlations Our. knowledge of the geology of the Alta district of west Finnmark owes much to the work of Holtedahl (1918, 1960) and Føyn (1964). The oldest rocks, the Raipas Group or Series (Reitan 1963a) of Precambrian (Karelian) age, are represented by a sequence of greenschist facies metasediments, metavolcanics and intrusives. Lying unconformably upon the Raipas is a quartzite formation, a thin tillite, and a mixed shale and sandstone succession. Holtedahl (1918) re ferred to these autochthonous post-Raipas rocks as the 'Bossekopavdelingen', but Føyn (1964) later demonstrated the presence of an angular uncon formity beneath the tillite and adopted this break as the border between what he termed the Bossekop Group and the overlying sediments, the Borras Group. These were later referred to as sub-groups (Føyn 1967, Pl. -
Komsa Dokumentasjonsvedlegg
DOKUMENTASJONSVEDLEGG § 19 FREDNING, KOMSA, ALTA, FINNMARK Reidun Laura Andreassen 1 1. Kvartærgeologi i Indre Altafjord Etter siste istid, for ca 10 000 år siden lå isfronten innerst i fjordene i Finnmark. Vekten av isen presset landet ned, men da avsmeltningen begynte og breens vekt minket, hevet landet seg igjen. Den enorme mengden smeltevann førte imidlertid til at havet steg, og i enkelte perioder var landhevningen og havstigningen like stor. Trykket av isen var imidlertid størst lengst inn mot bresenteret, i det indre av den Skandinaviske halvøya, og avtok gradvis ut mot kysten hvor breen var tynnest. Derfor hevet landet seg mer i de indre fjordstrøk enn ute ved kysten. Den marine grense i det indre av Altafjorden ligger på ca. 75m over dagens havnivå hvor havet stod for ca 10 000 år siden. Havet stod i flere perioder og vasket innover land, noe som førte til dannelsen av markerte strandterrasser som viser hvor havet en gang har stått. Oppover hele Altadalen ser vi merker etter havnivåene til enhver tid. Det er en generell arkeologisk oppfatning at bosetningen er knyttet til stranden, og at en derfor kan relatere boplasser til kronologi ut fra hvor høyt over havet de ligger. Kartene nedfor viser hvordan landskapet i indre Altafjord har endret seg gjennom tid i forhold til endring av havnivået. Som en ser av kartene var Komsa ei øy som gradvis ble landfast fra isens avsmeltning for ca. 10 000 år siden og helt fram til for ca 5-6000 år siden. 9 000 år siden 5500 år siden dagens havnivå 70 m.o.h 25 m.o.h Figur 1 Kartframstilling av havnivå fra forskjellige perioder. -
Getting Food During the German Occupation of Western Finnmark (1940–1944)
Getting food during the German occupation of Western Finnmark (1940–1944) Yaroslav Bogomolov In this article the author describes the food supply in the western part of Finnmark County. Despite the fact that the authorities tried to control the food supplies and secure equal access to food for all inhabitants, food distribution was never equal and civilians had to work hard and use their imagination in order to get some food to eat. 1 Introduction Nutrition as a topic was absent in historical studies for a long time. Food as a part of our daily routine is an almost invisible thing for historians. The changes have started to happen about two decades ago. As Clarkson and Crawford write “...nutritional history is moving out of the cellar”1. Today quite a lot of books have been published about human nutrition during various historical periods, but this work is still far from being finished. Aside from historical reports on Norwegians’ diet during the war2, nutrition on its own was very seldom a subject of interest for Norwegian authors3. This seems to me to be a bit strange. As we can see in articles by Mølmann et al. (2015) and Khatanzeiskaya (2015), insufficient nutrition was a cause of various health problems, so it is very important to study nutrition during the times of crisis. The topic of nutrition seems to me to be very comprehensive. It includes people’s daily diet, cuisine, ways of getting food, scientific approach to food (what kind of food is supposed to be healthy and how much of it is needed for each individual and so on) and much more. -
Translation Series No.1561
rfflmjyrS FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 1561 • Solar adtivity•and periodià fluctuations in'the ' • 'abundance of salmon • (from "Biological,foundations of the fishing - industry. and regulations of-Marine: fisheries") , By.I.B Birman . leglee - OCkUdà FISHEItiES AND eflA0TeQUE etce3 OCÉANS Original title: Periodicheskie kolebaniya chislennosti lososevykh i solnechnaya aktivnost,'("Biologicheskie osnovy rybnogo khozyaiStva i règchlirovanie morSkogo rybolovstva") From: Trudy VseSbyuznogo Nàuchno-,Issiedovatel'skogo Instituta Morskogô Rybnogo Khozyàistva i Okeanografii - (VNIRO). (Proceedings of the All-Union Research Institute of Marine - Fisheries and. Oceanography). Publ. by: Pïshchevaya PromyshlennoSt, Moscow; 67.(1):. 171-189, 1969.. t, • Translated by.the'Translation Blireau( JO) • Foreign Languages Divisicin • Department of the Secretary' of State of Canada Fisheries ReSearch Board - of Canada. Halifax Laboratory, , Halifax, N.S. .Biological . Station,. St. Andrews, N.S. .FreshWater Institute, 'Winnipeg, Manitoba ' . 1970 . • .31 pages typescript • • • DEPARTMENtOF THE SECRETARY OF STATE SECRÉTARIAT D'. ÉTAT• TRANSLATION BUREAU BUREAU DES TRADUCTIONS FOREIGN LANGUAGES DIVISION DES LANGUES CANADA • '- ÉTRANGÈRES TRANSLATED FROM — TRADUCTION DE INTO — EN Russian English AUTHOR — AUTEUR •Birman, LB. TITLE IN ENGLISH -• TITRE ANGLAIS Solar Activity and Periodic Fluctuations in the Abundance of Salmon Title in foreign language (transliterate foreign charactera) DeriodiCheskie kolebaniya chislennosti lososevykh i solnechnaya aktivnostt. RÇURENCE IN FOREIGN VANGUAGE (NAME OF BOOK OR PUBLICATION) IN'FULL. TRANSLITERATE FOREIGN CHARACTERS. REFERENCE 'EN LANGUE ETRANGàRE (NOM DU LIVRE OU. PUBLICATION), AU COMPLET.TRANSCRIRE EN CARACTàRES . PHONETIQUES. "Bioliogicheskie osnoVy-rybhogo. khozyaistva i.regulirovanie morskogo rybolovstva% . REFERENCE IN ENGLISH — RiFàRENCE EN ANGLAIS' uBiological Foundations of. the Fishing'IndustrY and Regulation of Marine FiSheries".. ••' • PUBLISH ER EDIT EUR PAGE NUMBERS IN ORIGINAL DATE OF PUBLICATION. -
GIS-Practical Experience in the Boundaries Definition of The
Journal of Geodesy and Geomatics Engineering 1 (2016) 19-24 D doi: 10.17265/2332-8223/2016.01.003 DAVID PUBLISHING GIS-Practical Experience in the Boundaries Definition of the Platform Deep Crustal Blocks on the Studying of the Earth’s Surface Fractal Divisibility: Example of the White Sea-Kuloi Plateau I. S. Sergeev St. Petersburg State University, Institute of Earth Sciences, Russia Abstract: This study examines the use of the geographic information systems (GIS) in structural geomorphology to build the model of the crust based on fractal analysis of relief. Fractal theory, developed by B. Mandelbrot, used to determination morpho-bloc divisibility of the Earth’s surface. There is the traceable statistically recurring relief structure indicate the appropriate tiered hierarchy of crustal blocks forming the tectonic and kinematic layers. This hypothesis tested on a digital elevation model (DEM) of the White Sea-Kuloi Plateau — an area of tectonic and magmatic activity of the Paleozoic era. Found the correlation of position the kimberlite magmatic bodies with the tectonic blocks certain depth according to a fractal analysis. Key words: Structural relief, tectonic blocs, geographic information systems, digital elevation model, fractal dimension. the existence of tectonic faults as the geological bodies. 1. Introduction This study based on the following position: tectonic At present days structural geomorphology defines fault is the boundary between certain moving volumes surface earth objects, “not daring” to look into the of the lithosphere, and, like in any boundary zone in depths of the earth. Geomorphology “given” this spatial development, it is the tectonic movement of the opportunity to geophysical sciences. -
Long-Term Salmon Catches in Finnmark
Kolarctic ENPI CBC - Kolarctic salmon project (KO197) - Report X Long-term salmon catches at sea in salmon districts in Finnmark Eero Niemelä1, Esa Hassinen1 and Tiia Kalske2 1Finnish Game and Fisheries Research Institute (FGFRI), Teno River Research Station Utsjoki, Finland 2Office of the County Governor of Finnmark (FMFI), Vadsø, Norway Contents Abstract ....................................................................................................................................................... 3 1. Introduction ......................................................................................................................................... 4 2. Material and methods .......................................................................................................................... 5 3. Results ................................................................................................................................................. 5 Acknowledgements ....................................................................................................................................17 Cover photo: Alta type bag net in Altafjord in year 2012. Photo: Eero Niemelä This report has been produced with the assistance of the European Union, but the contents can in no way be taken to reflect the views of the European Union. 2 Abstract In Kolarctic salmon project we made an overview of the officially reported salmon catches in four salmon district areas in Finnmark County especially studying catches taken with bag nets,