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The Anason Family in Rogaland County, Norway and Juneau County, Wisconsin Lawrence W
Andrews University Digital Commons @ Andrews University Faculty Publications Library Faculty January 2013 The Anason Family in Rogaland County, Norway and Juneau County, Wisconsin Lawrence W. Onsager Andrews University, [email protected] Follow this and additional works at: http://digitalcommons.andrews.edu/library-pubs Part of the United States History Commons Recommended Citation Onsager, Lawrence W., "The Anason Family in Rogaland County, Norway and Juneau County, Wisconsin" (2013). Faculty Publications. Paper 25. http://digitalcommons.andrews.edu/library-pubs/25 This Book is brought to you for free and open access by the Library Faculty at Digital Commons @ Andrews University. It has been accepted for inclusion in Faculty Publications by an authorized administrator of Digital Commons @ Andrews University. For more information, please contact [email protected]. THE ANASON FAMILY IN ROGALAND COUNTY, NORWAY AND JUNEAU COUNTY, WISCONSIN BY LAWRENCE W. ONSAGER THE LEMONWEIR VALLEY PRESS Berrien Springs, Michigan and Mauston, Wisconsin 2013 ANASON FAMILY INTRODUCTION The Anason family has its roots in Rogaland County, in western Norway. Western Norway is the area which had the greatest emigration to the United States. The County of Rogaland, formerly named Stavanger, lies at Norway’s southwestern tip, with the North Sea washing its fjords, beaches and islands. The name Rogaland means “the land of the Ryger,” an old Germanic tribe. The Ryger tribe is believed to have settled there 2,000 years ago. The meaning of the tribal name is uncertain. Rogaland was called Rygiafylke in the Viking age. The earliest known members of the Anason family came from a region of Rogaland that has since become part of Vest-Agder County. -
WEST NORWEGIAN FJORDS UNESCO World Heritage
GEOLOGICAL GUIDES 3 - 2014 RESEARCH WEST NORWEGIAN FJORDS UNESCO World Heritage. Guide to geological excursion from Nærøyfjord to Geirangerfjord By: Inge Aarseth, Atle Nesje and Ola Fredin 2 ‐ West Norwegian Fjords GEOLOGIAL SOCIETY OF NORWAY—GEOLOGICAL GUIDE S 2014‐3 © Geological Society of Norway (NGF) , 2014 ISBN: 978‐82‐92‐39491‐5 NGF Geological guides Editorial committee: Tom Heldal, NGU Ole Lutro, NGU Hans Arne Nakrem, NHM Atle Nesje, UiB Editor: Ann Mari Husås, NGF Front cover illustrations: Atle Nesje View of the outer part of the Nærøyfjord from Bakkanosi mountain (1398m asl.) just above the village Bakka. The picture shows the contrast between the preglacial mountain plateau and the deep intersected fjord. Levels geological guides: The geological guides from NGF, is divided in three leves. Level 1—Schools and the public Level 2—Students Level 3—Research and professional geologists This is a level 3 guide. Published by: Norsk Geologisk Forening c/o Norges Geologiske Undersøkelse N‐7491 Trondheim, Norway E‐mail: [email protected] www.geologi.no GEOLOGICALSOCIETY OF NORWAY —GEOLOGICAL GUIDES 2014‐3 West Norwegian Fjords‐ 3 WEST NORWEGIAN FJORDS: UNESCO World Heritage GUIDE TO GEOLOGICAL EXCURSION FROM NÆRØYFJORD TO GEIRANGERFJORD By Inge Aarseth, University of Bergen Atle Nesje, University of Bergen and Bjerkenes Research Centre, Bergen Ola Fredin, Geological Survey of Norway, Trondheim Abstract Acknowledgements Brian Robins has corrected parts of the text and Eva In addition to magnificent scenery, fjords may display a Bjørseth has assisted in making the final version of the wide variety of geological subjects such as bedrock geol‐ figures . We also thank several colleagues for inputs from ogy, geomorphology, glacial geology, glaciology and sedi‐ their special fields: Haakon Fossen, Jan Mangerud, Eiliv mentology. -
How Uniform Was the Old Norse Religion?
II. Old Norse Myth and Society HOW UNIFORM WAS THE OLD NORSE RELIGION? Stefan Brink ne often gets the impression from handbooks on Old Norse culture and religion that the pagan religion that was supposed to have been in Oexistence all over pre-Christian Scandinavia and Iceland was rather homogeneous. Due to the lack of written sources, it becomes difficult to say whether the ‘religion’ — or rather mythology, eschatology, and cult practice, which medieval sources refer to as forn siðr (‘ancient custom’) — changed over time. For obvious reasons, it is very difficult to identify a ‘pure’ Old Norse religion, uncorroded by Christianity since Scandinavia did not exist in a cultural vacuum.1 What we read in the handbooks is based almost entirely on Snorri Sturluson’s representation and interpretation in his Edda of the pre-Christian religion of Iceland, together with the ambiguous mythical and eschatological world we find represented in the Poetic Edda and in the filtered form Saxo Grammaticus presents in his Gesta Danorum. This stance is more or less presented without reflection in early scholarship, but the bias of the foundation is more readily acknowledged in more recent works.2 In the textual sources we find a considerable pantheon of gods and goddesses — Þórr, Óðinn, Freyr, Baldr, Loki, Njo3rðr, Týr, Heimdallr, Ullr, Bragi, Freyja, Frigg, Gefjon, Iðunn, et cetera — and euhemerized stories of how the gods acted and were characterized as individuals and as a collective. Since the sources are Old Icelandic (Saxo’s work appears to have been built on the same sources) one might assume that this religious world was purely Old 1 See the discussion in Gro Steinsland, Norrøn religion: Myter, riter, samfunn (Oslo: Pax, 2005). -
Glaciotectonic Structure and Genesis of the Herdla Moraines, Western Norway
Glaciotectonic structure and genesis of the Herdla Moraines, western Norway JAMES S. ABER & INGE AARSETH Aber, J. S. & Aarseth, 1.: Glaciotectonic structure and genesis of the Herdla Moraines, western Norway. Norsk Geologisk Tidsskrift, Vol. 68, pp. 99-106. Oslo 1988. ISSN 0029-196X. At its type locality, glaciomarine sediment of the Herdla Moraines was deformed and consolidated by overriding ice. Two phases of moraine development took place in conjunction with ice movement coming first from the east-northeast and later from the southeast. The early phase is related to development of a local ice dome on Stølsheimen during the middle Younger Dryas (about 10,500 BP), when the ice sheet reached its late glacial maximum thickness in the region. The ice sheet then thinned rapidly, due to climatic amelioration and increased calving, and shifted to southeasterly movement at Herdla. Most glaciotectonic disturbance and consolidation of sediment at Herdla happened during this late phase, perhaps as a result of a glacier surge along Herdlafjord. The glaciotectonic structures at Herdla are local in character and cannot be used for regional correlation of glacial advances in western Norway. J. S. Aber, Earth Science Department, Emporia State University, Emporia, Kansas, 66801, USA; l. Aarseth, Universitetet i Bergen, Geologisk Institutt, Avd. B. A/legt, 41. N-5007 Bergen, Norway. Y ounger Dry as moraines of western Norway Aarseth & Mangerud (1974) defined the Herdla Moraines as a morphostratigraphic unit with a type locality at Herdla island (Fig. 1). Sediments of the Herdla Moraines are part of a conspicuous system of ice marginal deposits of Younger Dryas age (10,000-11,000 BP) that has been mapped around the periphery of southern and western Norway (Mangerud et al. -
Bergen Kommune Brosjyre.ENG.Indd
The City is Bergen History • Nature • Industry • Culture Street life • Services City of Water FACTS ABOUT BERGEN With a population of 240.000, Bergen is Norway’s second largest As the capital of Western city and the largest in the county of Hordaland. It is also the capital Norway, Bergen has devel- of Western Norway, which is the leading region for all signifi cant oped close ties with other municipalities in the region, Norwegian export industries. such as joint ownership of the Port Authorities of Bergen is a charming blend of tradition and innovation. Throughout Bergen, the regional waste history Bergen has built a strong reputation as a centre for trade and management company BIR shipping. This is due to its strategic location on the coast. Proximity and the regionally owned power company BKK. to the sea has continued to provide benefi ts for the maritime and marine industries and for tourism. The Bergen region has the most complete maritime environment and is also an international centre of infl uence for fi sheries, aquaculture and seafood. Western Norway produces 80% of Norway’s exports of crude oil, and the Bergen region is home to a leading expertise within oil and gas on a global scale. Bergen has a considerable shipping fl eet, and the city is dominant in the global market of transporting chemicals and other goods. The Bergen region is also home to strong and growing industries within information and communication technology (ICT), media, the arts and education. The municipality supports several network organisations, such as Maritime Bergen, Fiskeriforum Vest, Bergen Tourist Board, Hordaland Oil and Gas, Education in Bergen and Bergen Media City. -
The Jacobson Family from Laerdal Parish, Sogn Og Fjordane County, Norway; Pioneer Norwegian Settlers in Greenwood Township, Vernon County, Wisconsin
THE JACOBSON FAMILY FROM LAERDAL PARISH, SOGN OG FJORDANE COUNTY, NORWAY PIONEER NORWEGIAN SETTLERS IN GREENWOOD TOWNSHIP, VERNON COUNTY, WISCONSIN BY LAWRENCE W. ONSAGER THE LEMONWEIR VALLEY PRESS Mauston, Wisconsin and Berrien Springs, Michigan 2018 COPYRIGHT © 2018 by Lawrence W. Onsager All rights reserved including the right of reproduction in whole or in part in any form, including electronic or mechanical means, information storage and retrieval systems, without permission in writing from the author. Manufactured in the United States of America. -----------------------------------Cataloging in Publication Data----------------------------------- Onsager, Lawrence William, 1944- The Jacobson Family from Laerdal Parish, Sogn og Fjordane County, Norway; Pioneer Norwegian Settlers in Greenwood Township, Vernon County, Wisconsin. Mauston, Wisconsin and Berrien Springs, Michigan: The Lemonweir Valley Press, 2018. 1. Greenwood Township, Vernon County, Wisconsin 2. Jacobson Family 3. Laerdal Township, Sogn og Fjordane County, Norway 4. Greenwood Norwegian-American Settlement in Vernon County, Wisconsin I. Title Tradition claims that the Lemonweir River was named for a dream. Prior to the War of 1812, an Indian runner was dispatched with a war belt of wampum with a request for the Dakotas and Chippewas to meet at the big bend of the Wisconsin River (Portage). While camped on the banks of the Lemonweir, the runner dreamed that he had lost his belt of wampum at his last sleeping place. On waking in the morning, he found his dream to be a reality and he hastened back to retrieve the belt. During the 1820's, the French-Canadian fur traders called the river, La memoire - the memory. The Lemonweir rises in the extensive swamps and marshes in Monroe County. -
Regions and Counties in Norway
Regions and counties in Norway REGIONS AND COUNTIES IN NORWAY Northern Norway Northern Norway is located in the north and is also the most eastern region. This region comprises the two counties Troms og Finnmark and Nordland. If you visit Northern Norway in December or January, you can experience the polar night. The polar night is when the sun is under the horizon the whole day. In Northern Norway, you can see the northern lights in winter. Norway is divided into five regions. Northern Norway is located in the north of Northern lights. Photo: Pxhere.com the country. Trøndelag is located in the middle of the country. Western Norway is During summer, you can see the midnight in the west, and Eastern Norway is in the sun in Northern Norway. The midnight sun east. The region located in the south is is when the sun does not set, and a part of called Southern Norway. the sun is visible above the horizon all night. Every part of the country is divided into counties. There are 11 counties in Norway. Troms and Finnmark Troms og Finnmark is located furthest north and east and borders Russia, Finland 1 The National Centre of Multicultural Education, Native languages, morsmal.no Regions and counties in Norway and Sweden. Tromsø is the largest city in Troms og Finnmark. Norway's northernmost point, Knivskjellodden, is located in Troms og Finnmark. The North Cape (Nordkapp) is better known and is located almost as far north as Knivskjellodden. The North Cape is a famous tourist destination in Norway. Skrei cod hanging to dry on a rack. -
New Datings of Three Courtyard Sites in Rogaland
Frode Iversen 26 Emerging Kingship in the 8th Century? New Datings of three Courtyard Sites in Rogaland The Norwegian ‘courtyard sites’ have variously been interpreted as special cultic, juridical, or military assembly sites, which served at more than the purely local level. Previously, on the basis of studies of artefacts and finds of pottery from these structures, the principal period of use of the courtyard sites in Rogaland has been dated to the early and late Roman Iron Age (AD 1–400) and the Migration Period (AD 400–550) through c. AD 600. To test the validity of this date range, the Avaldsnes Royal Manor Project has commissioned thirty new radiocarbon datings of material from three courtyard sites in Rogaland that Jan Petersen had excavated in 1938–50. These are Øygarden, Leksaren, and Klauhaugane; the latter is one of the largest courtyard sites in Norway. Øygarden has not previously been radiocarbon dated. For Klauhaugene, only a few radiocarbon dates had been obtained prior to this study. Leksaren was radiocarbon dated in the 1990s, with the results rather surprisingly indicating that its use continued into the 7th century. The present study demonstrates that the three investigated sites were in use during the Merovingian Period (AD 550–800) – a finding that both confirms and develops previous chronological frameworks. The courtyard sites in Rogaland fell out of use earlier than in other areas along the western coast of Norway. It is therefore suggested that their abandonment was connected to the emergence in the 8th century of royal power accompanied by greater control over jurisdiction – a royal power that subsequently expanded within the coastal zone. -
Gårds- Og Stedsnavnet Asak Av Tore Falkenhaug
1 Gårds- og stedsnavnet Asak Av Tore Falkenhaug Asak i Skedsmo sett fra Kjus Til Asak Jeg så deg i kvellinga fra høgda ved Kjus. Du lå der langs hellinga med hus etter hus nå i kveldsola så vidunderlig skjønn med skogen bakom - så frodig og grønn. Kristian Haugli 1932 Asak-navnet og tolkningen av dette har interessert lingvister i snart 160 år. Hvorfor har dette navnet vekket slik interesse? Kanskje har man ant att gårdene har en spesiell historie og at navnet kunne fortelle noe om dette. Våre gamle gårds- og stedsnavn gir historisk identitet til gårdene og til stedene, og rett tolket bidrar de til vår forståelse av hendelser og virksomheter i vår fortid så vel lokalt, regionalt som nasjonalt. For enkelte av våre gårdsnavn kan det virke som om opprinnelsen ligger skjult i en fjern tid og språklig så langt tilbake at en tolkning kanskje aldri kan bli nådd. Men det er åpenbart ikke lett å avstå fra tolkninger av navn selv om de vanskelig lar seg avkode. Avanserte hypoteser på svakt underlag bør da settes på prent med stor forsiktighet og forbehold. Har de kommet inn i skrifter og bøker der de brukes som referanser, blir de fort absolutte sannheter som blir vanskelige å rokke ved. Gårdsnavnet Asak som ofte har blitt diskutert, ser ut til å være et slikt navn. Mange tolkninger av opprinnelse og betydning har blitt framlagt. I et senere innlegg kommer jeg å vise de mange fantastiske utlegninger som har blitt gjort, fra 1800 tallet til vår tid. Denne gang vil jeg i midlertid ta for meg tolkningene av Asak som et åker-navn og vise at dette ikke er riktig. -
EGU2014-13199, 2014 EGU General Assembly 2014 © Author(S) 2014
Geophysical Research Abstracts Vol. 16, EGU2014-13199, 2014 EGU General Assembly 2014 © Author(s) 2014. CC Attribution 3.0 License. Back-analysis of the 1756 Tjellefonna rockslide (western Norway) Gro Sandøy (1), Thierry Oppikofer (1), and Bjørn Nilsen (2) (1) Geological Survey of Norway (NGU), Trondheim, Norway ([email protected]), (2) Norwegian University of Science and Technology (NTNU), Trondheim, Norway The 22nd of February 1756 the largest historically recorded rockslide in Norway took place at Tjelle in Lang Fjord (western Norway). Three displacement waves of up to 50 meters were created by the impact of the failed rock mass constituting the Tjellefonna rockslide. A total of 32 people were killed and several houses and boats around the fjord were destroyed. This study presents a back-analysis of the Tjellefonna rockslide by (1) reconstructing the topography be- fore the rockslide, (2) assessing the volumes of the initial rockslide mass, the onshore deposits and offshore deposits, (3) assessing the major discontinuities involved in the rockslide, and (4) by 2D numerical slope stability modelling for a detailed study of the parameters and trigger factors that affected the slope stability. The topography before the rockslide is reconstructed using (1) the Sloping Local Base Level technique and (2) a manual ART reconstruction in the PolyWorks software. Both topographic reconstructions yield an initial rockslide volume between 9.2 and 10.4 million m3, which is lower than previous estimates (12-15 million m3). The onshore deposits are estimated to 7.6 million m3 and only 3.9 million m3 deposited in the fjord. Finally, the volume impacting the fjord (3.9 million m3) is important for the generation of rockslide-triggered displacement waves, which highlights the necessity of precise volume estimations prior to back-analyses of landslide-triggered displacement waves. -
Vessel Import to Norway in the First Millennium AD Composition And
VESSEL IMPORT TO NORWAY IN THE FIRST MILLENNIUM A.D Composition and context. by Ingegerd Roland Ph.D. thesis. Institute of Archaeology, University College London, June 1996. ProQuest Number: 10017303 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest. ProQuest 10017303 Published by ProQuest LLC(2016). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code. Microform Edition © ProQuest LLC. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 Abstract : More than 1100 complete or fragmentary imported vessels in bronze, glass, wood, horn, clay and silver from the first millennium A.D. have been found in Norway, approximately 80% of them in graves. The extensive research already carried out has produced a vast body of literature, which generally keeps within strict chronological boundaries, concentrating on vessels from either the Roman Period, the Migration Period, or the Viking Age. Two main approaches to the material have traditionally been applied: 1) typo logical studies, on the basis of which trade connections and systems have been discussed from different theoretical perspectives, and 2) imports as status markers, from which hierarchical social systems of a general kind have been inferred. Only very rarely have their function as vessels attracted any serious consideration, and even more rarely their actual local context. -
On and Off the Coast of Western Norway: Names of Oil Fields Compared to Traditional Place-Names
;; , Place-names(geographical names) on and off the coast of Western Norway: Names of oil fields compared to traditional place-names Botolv Helleland (Professor, University of Oslo, NO/way) 1. Introduction. The aim of this paper is to investigate the function and structure of two totally different place-name systems: traditional place- names along the Norwegian coast and the names of oil fields off the coast. The question raised is in which way and to which extent do the two types differ. Do the differences have any implications as to national and international communication on the one hand and the preservation of the cultural heritage on the other hand? 2. Name function and name meaning A place-name (geographical name, name of a topographic feature) is a monoreferential linguistic expression whose task is to identify a tOJX)graphic feature and to distinguish it from another topographic feature in a given linguistic context. It serves, with other words, as an address or a label. When a place-name is used. within a group of competent language users the name will, when it is mentioned, bring the same topographic feature to mind. A more complicated question, which will not be discussed in detail here, is to which extent a name avokes the same connotations to different users of the name. Certainly the answer depends on the background of the name users and how familiar they are with the n~e in Question and its reference. Language philosophers like John Stuart Mill and John Searle have discussed the matter from two different approaches the fonner claiming «the Genuine Reference Theory» as the correct understanding of a name's function (a , name has no meaning beyond its reference), whereas the second is defending «the Genuine Reference Theory» or «Cluster Theory », saying that the meaning of a name cannot be expressed in general tenns; instead one has to count on a group of meanings (clusters or criteria) which are represented in the name, and that those criteria may change over time, however without a fundamental - 8 - change of the meanmg.