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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. -
Diploma Rogra M Fall 2017
Arkitektur- og designhøgskolen i Oslo The Oslo School of Architecture and Design DIPLOMA ROGRAM FALL 2017 Diploma candidate: Robert Sømod Institute: FTH Main supervisor: Beate Hølmebakk Second supervisor: Lars Danielsen Holen External supervisor: Company cooperation: Ti tie of project: Lysebotn 1 Pre-diploma rapport ”Lysebotn 1” Robert Sømod AHO, Fall 2017 Supervisor: Beate Hølmebakk Introduction Lysebotn1 water power facility began construction in 1947, with an aim to sup- ply the county of Rogaland in the south-west Norway with power in a time when society had an ever-increasing consumption of electricity. Due to post-war politics and restrains, the facility was constructed 50 meters inside a mountain. Both to secure this important facility from bomb-raids and to save cost in materials. It was constructed next to a natural mountain shelf in the beautiful Lysefjorden. Historically, because of intervention in nature, waterpower-facilities have been controversial, but in the same time it has brought work and pride to locals. Today, some look at these spaces as something sacred. The owners of Lysebotn1 is constructing a new facility, Lysebotn2, which will take over and increase the production. Lysebotn 1 and its halls carved out of mountain will then close down. I consider these halls to be highly interesting, and want to open them for public. My fascination is that the aim of the infrastructural program has do with the most essential needs of structure. In the fact that these industrial facilities require spe- cific logic systems, and programs that deal with infrastructure demands a specific architecture in means that only the most necessary will be done. -
Helpful Information for Your Kjerag Trip 2016
Helpful Information For Your Kjerag Trip 2016 Check out the Ferry Boat times to co-ordinate them with your flight times. In general arriving at the Stavanger Sola Airport (SVG) in the morning hours on a Monday, Wednesday, or Friday work best for scheduling so that you can leave the airport quickly and catch the *12:30 Fast Ferry ( *new summer time schedule from dates in June sometime ). If your coming for the Heliboogie Monday June 20th would be your best choice for early morning arrival into Stavanger. Do not purchase expensive airline tickets that get you into Stavanger later and then missing the ferry boats into the fjord and having to stay overnight in a hotel just to catch the Lauvvik slow ferry or Lysefjord Tourist Bus in the next day. There is a city map of Stavanger web link as well as other helpful links below. When you get to the Sola Airport catch the blue and white airport Flybussen bus (or taxi) to the "Fiskepiren" destination, Fiskepirterminalen building in Stavanger. Dock Route # 13 located next to Fiskepirterminalen Building, where the Fast Ferry leave from in Stavanger, the street address there is 14 Verksgata street. Verify with ferry web links below as 2016 does have some slow ferry departures leaving from Lauvik and a bus is needed to get from Stavanger to Lauvvik. These Ferry final destination is at Lysebotn where the Base Klubb and accommodations are located. City map of Stavanger web link is http://www.stavanger- guide.no/regionstavanger/stavanger/map_english.pdf Ground Transportation -Airport Bus Transportation from the Sola Airport to Stavanger are the blue and white Flybussen, which drops you of at the Fiskepiren Ferry Docks. -
Dermatology Abroad
Dermatology Abroad Specialist in Dermato-Venereology in Norway and Denmark CA RSTEN SA UER MIKKELSEN Dermatologist, Private Practice, Brønderslev, Denmark. E-mail: [email protected] Carsten Sauer Mikkelsen has visited the Department of Dermatology at the University Hospital in Stavanger, Norway and strongly recommends a visit to the city with its majestic natural surroundings. I recently had the opportunity to work as a dermatologist in involved in areas of dermatological research. The frequent the Department of Dermatology at the University Hospital, meetings with the Dermatopathology Service are also of high Stavanger, Norway, for 6 months (1 May–31 September 2009). educational value. Stavanger is a city and municipality in the county of Rogaland. The municipality has a population of approximately 122,000, The guidelines, procedures and daily work were quite similar and 190,000 people live in the Stavanger conurbation, making to work at the departments of dermatology at university hos- Stavanger the third largest city in Norway. It is the centre of the Norwegian petroleum industry. During my stay in Stavanger I learned a lot about clinical and surgical dermatology and was involved in various areas of dermatological research. Dermatology in Stavanger involved work within all standard dermatological treatment modalities, including cutaneous surgery, ultraviolet therapy (UVA and UVB), Bucky therapy, and many different laser procedures. Biological treatment was also frequently used. Education of residents is given high priority, including daily supervision from senior dermatologists, literature review, presentation of different skin conditions, and participa- tion in international congresses. The senior doctors are all Fig. 2. End to end, Lysefjord measures 42 km with rocky walls falling nearly vertically over 1000 m into the water. -
The Stavanger Region
THE REGION AND LYSEFJORD ACB STORD Sunde Odda & Bergen TEGNFORKLARING LEGEND E 39 13 Sagvåg BERGEN 48 Siggjarvåg Ranavik Utaker TURISTINFORMASJON 175 km Leirvik D Bremnes N Røldal E 134 TOURIST INFORMATION MAPS Matre A L OSLO NORWAY A D N Skjersholmane D A NASJONALE TURISTVEGER BØMLO Sydnes R L Røldal kr O K NATIONAL TOURIST ROUTES 48 A Skisenter R 1 Valevåg H G A 1 Skånevik O M R E BADING Mosterhamn L Utbjoa 13 E BATHING den T BERGEN jor Holmavatnet laf TURISTVEG 2 m Etne UTSIKT Bø E 39 RYFYLKE Nesflaten Langevågen Sauda SCENIC VIEW Buavåg 520 RYFYLKEVEGEN Ølen Århus Sandvatnet CAMPINGPLASS Tengesdal CAMPING SITE Sandeid R NORTH SEA ROAD E 134 E BOBIL SERVICESENTER 47 D & TØMMING Ropeid Tangen Hylen G Mostølen A MOBILE HOME SERVICE - Vikedal 140 km 46 Suldalsvatnet T CENTRE 15 12 Suldal S Røværsholmen n U SKI TERRENG d e Sand A V i n d a f j o r SKIING AREAS HAUGESUND Vormestrand LAKSESAFARI Aksdal Gullingen FYRTÅRN 2 Marvik 2 2 E 39 Sandsavatnet LIGHTHOUSE Nedstrand 13 Hebnes 1 STAVANGER LUFTHAVN Helganes RYFYLKEVEGEN Utsira STAVANGER AIRPORT KARMØY Erøy Vindsvik Kårstø Foldøy Jelsa BJERGØY Blåsjø 2 HAUGESUND LUFTHAVN UTSIRA OMBO Kopervik 6 Nesheim Nesvik HAUGESUND AIRPORT SJERNARØY Skipavik Føresvik 5 Eidssund 47 KYRKJØY Helgøysund 16 MOTORVEI BOKN MOTORWAY FINNØY Judaberg RANDØY Hjelmeland Svartevatn Arsvågen Halsnøy RYFYLKE 105 km Fister EUROPAVEI Skudeneshavn RENNESØY Ladstein EUROPEAN ROAD Mortavika kr Nes = DISTRICT MAP Hanasand FYLKESVEI med Fogn Årdal Nilsebu NATUROPPLEVELSE Vikaholmane Talgje Godfardalen PRIMARY ROUTES with -
UNFC Case Studies from Finland/Estland, Sweden and Norway
United Nations ECE/ENERGY/GE.3/2020/10 Economic and Social Council Distr.: General 15 April 2020 Original: English only Economic Commission for Europe Committee on Sustainable Energy Expert Group on Resource Management Eleventh session Geneva, 20-24 April 2020 Item 11 of the provisional agenda Application of the United Nations Framework Classification for Resources (UNFC) in different geographical contexts. United Nations Framework Classification for Resources Case Studies from Finland/Estland, Sweden and Norway – Nordkalk limestone and Forsand sand and gravel mines Prepared by the Geological Survey of Norway, the Geological Survey of Sweden, Nordkalk, Forsand Sandkompani and Petronavit a.s. Summary This study demonstrates how the United Nations Framework Classification for Resources (UNFC) is being used to classify industrial mineral extraction projects for limestone in Estland and Sweden, and for a gravel and sand project in Norway. The report summarizes the main features of UNFC before describing the Nordkalk limestone projects. These projects demonstrate the usefulness of UNFC in categorizing environmental, social economic conditions and technical feasibility that may facilitate or hamper project development. The gravel and sand project demonstrates the use of UNFC in a case with few complications. This also shows an accounting method based on a standard that is common in national statistics as well as in project management. The gravel and sand case is also used to show how a UNFC inventory built with respect for the quality requirements embedded in the Committee for Mineral Reserves International Reporting Standards (CRIRSCO) may be translated into a CRIRSCO inventory. This allows for new UNFC accounts to be compared with existing CRIRSCO accounts and thus prevents a break in the records when going from a CRIRSCO standard to the UNFC standard ECE/ENERGY/GE.3/2020/10 Contents Page I. -
SVR Brosjyre Kart
VERNEOMRÅDA I Setesdal vesthei, Ryfylkeheiane og Frafjordheiane (SVR) E 134 / Rv 13 Røldal Odda / Hardanger Odda / Hardanger Simlebu E 134 13 Røldal Haukeliseter HORDALAND Sandvasshytta E 134 Utåker Åkra ROGALAND Øvre Sand- HORDALAND Haukeli vatnbrakka TELEMARK Vågslid 520 13 Blomstølen Skånevik Breifonn Haukeligrend E 134 Kvanndalen Oslo SAUDA Holmevatn 9 Kvanndalen Storavassbu Holmevassåno VERNEOMRÅDET Fitjarnuten Etne Sauda Roaldkvam Sandvatnet Sæsvatn Løkjelsvatnhytta Saudasjøen Skaulen Nesflaten Varig verna Sloaros Breivatn Bjåen Mindre verneområdeVinje Svandalen n e VERNEOMRÅDAVERNEOVERNEOMRÅDADA I d forvalta av SVR r o Bleskestadmoen E 134 j Dyrskarnuten f a Ferdselsrestriksjonar: d Maldal Hustveitsåta u Lislevatn NR Bråtveit ROGALAND Vidmyr NR Haugesund Sa Suldalsvatnet Olalihytta AUST-AGDER Lundane Heile året Hovden LVO Hylen Jonstøl Hovden Kalving VINDAFJORD (25. april–31. mai) Sandeid 520 Dyrskarnuten Snønuten Hartevatn 1604 TjørnbrotbuTjø b tb Trekk Hylsfjorden (15. april–20. mai) 46 Vinjarnuten 13 Kvilldal Vikedal Steinkilen Ropeid Suldalsosen Sand Saurdal Dyraheio Holmavatnet Urdevasskilen Turisthytter i SVR SULDAL Krossvatn Vindafjorden Vatnedalsvatnet Berdalen Statsskoghytter Grjotdalsneset Stranddalen Berdalsbu Fjellstyrehytter Breiavad Store Urvatn TOKKE 46 Sandsfjorden Sandsa Napen Blåbergåskilen Reinsvatnet Andre hytter Sandsavatnet 9 Marvik Øvre Moen Krokevasskvæven Vindafjorden Vatlandsvåg Lovraeid Oddatjørn- Vassdalstjørn Gullingen dammen Krokevasshytta BYKLE Førrevass- Godebu 13 dammen Byklestøylane Haugesund Hebnes -
Water Chemistry and Acidification Recovery in Rogaland County
INNSENDTE ARTIKLER Water chemistry and acidification recovery in Rogaland County By Espen Enge Espen Enge is senior engineer, Environmental Division, County Governor of Rogaland. Sammendrag Introduction Redusert forsuring av fjellvann i Rogaland Due to exceptionally slow weathering bedrock, fylke. Her bearbeides resultater fra i alt 1144 the concentrations of ions in river and lake water prøver fra 2002, 2007 og 2012. Tre ulike forsurings in the mountain areas of southern Norway are modeller antydet at forsuringen i fjellområdene i generally very low (Wright and Henriksen 1978). Rogaland (>500 m) i dag er begrenset, og at In Rogaland, 12% of the surveyed lakes in 1974 vannkvaliteten trolig er nær en opprinnelig ufor 1979 (Sevaldrud and Muniz 1980) had conduc suret vannkvalitet. Mange lavereliggende inn tivity of <10 µS/cm, and the minimum value was sjøer var tilsynelatende fortsatt forsuret, men 4.2 µS/cm. disse estimatene kan være forbundet med usik Dilute, weakly buffered water is highly sensi kerhet. Ioneinnholdet i vannet i fjellområdene er tive to acidification. Thus, as early as the 1870s ekstremt lavt, noe som i seg selv trolig utgjør en the brown trout population (Salmo trutta) in begrensning for utbredelsen av aure. Sandvatn in Hunnedalsheiene declined close to extinction (HuitfeldtKaas 1922), possibly due to Summary emerging acidification (Qvenild et al. 2007). In The current study compiles data from 1144 water the 1920s massive fish kills due to acidic water samples from three large regional water chemical were observed in the salmon rivers Dirdal, Fra surveys, performed in 2002, 2007 and 2012. fjord and Espedal (HuitfeldtKaas 1922). -
Iconic Hikes in Fjord Norway Photo: Helge Sunde Helge Photo
HIMAKÅNÅ PREIKESTOLEN LANGFOSS PHOTO: TERJE RAKKE TERJE PHOTO: DIFFERENT SPECTACULAR UNIQUE TROLLTUNGA ICONIC HIKES IN FJORD NORWAY PHOTO: HELGE SUNDE HELGE PHOTO: KJERAG TROLLPIKKEN Strandvik TROLLTUNGA Sundal Tyssedal Storebø Ænes 49 Gjerdmundshamn Odda TROLLTUNGA E39 Våge Ølve Bekkjarvik - A TOUGH CHALLENGE Tysnesøy Våge Rosendal 13 10-12 HOURS RETURN Onarheim 48 Skare 28 KILOMETERS (14 KM ONE WAY) / 1,200 METER ASCENT 49 E134 PHOTO: OUTDOORLIFENORWAY.COM PHOTO: DIFFICULTY LEVEL BLACK (EXPERT) Fitjar E134 Husnes Fjæra Trolltunga is one of the most spectacular scenic cliffs in Norway. It is situated in the high mountains, hovering 700 metres above lake Ringe- ICONIC Sunde LANGFOSS Håra dalsvatnet. The hike and the views are breathtaking. The hike is usually Rubbestadneset Åkrafjorden possible to do from mid-June until mid-September. It is a long and Leirvik demanding hike. Consider carefully whether you are in good enough shape Åkra HIKES Bremnes E39 and have the right equipment before setting out. Prepare well and be a LANGFOSS responsible and safe hiker. If you are inexperienced with challenging IN FJORD Skånevik mountain hikes, you should consider to join a guided tour to Trolltunga. Moster Hellandsbygd - A THRILLING WARNING – do not try to hike to Trolltunga in wintertime by your own. NORWAY Etne Sauda 520 WATERFALL Svandal E134 3 HOURS RETURN PHOTO: ESPEN MILLS Ølen Langevåg E39 3,5 KILOMETERS / ALTITUDE 640 METERS Vikebygd DIFFICULTY LEVEL RED (DEMANDING) 520 Sveio The sheer force of the 612-metre-high Langfossen waterfall in Vikedal Åkrafjorden is spellbinding. No wonder that the CNN has listed this 46 Suldalsosen E134 Nedre Vats Sand quintessential Norwegian waterfall as one of the ten most beautiful in the world. -
HØLE Berggrunnskart
" " " " " " " * " " * " * # " " " # " " " # " " " " " " " " " " " " " " " " " " " " " " " " " " * " " # " " " " " # # * " 3 3 " 19 20 21 22 23 24 25 26 27 28 29 30 31 32 * 33 34 35 36 37 38 39 340 " " # " " " " " " " " " " " " " " " " " " " " "" " " " " " " " " " " " " " " " 17 5 5 " " " " " " " " " 12 Troppeknuten * LØSMASSER FRA KVARTÆRTIDEN # " 44 " # " " Jøssang " " " # " " # " " " " " 18 # 1 " # 43 " 5 " " " 18 17 # # DEPOSITS OF QUATERNARY AGE " " " " 5 " " " Svines "" " " " " " " " # # # " " " " # " " " " # Berggrunnskart " " " " " " " " " " " "" " " " " " " " " " " " " " " " " " " " " " " " " " " " " Løsmasser, udifferensiert # " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " # " " " " " " " " " " 0 " " " " " " " " " " " " " " " " " " " " * " " " " " " " " " " " " 8" 260 Lammatoknuten Superficial deposits, undifferentiated " " " " " " " " " " " " " " " " " " " " " " " " " " " " " " * " " " Rindane 2 " * " 11 6 " " " × " 53 " " " " " " # 5 Ådnanesnuten 3 Tangane " × " " Bedrock map " " " " Vatne # " " " " " 20 " " " " " " " " " " 17 " * " " " " 1 " " " " 64 " " " 15 " # " " # " " " " " " " " " # 24 " " " " " # " " " " " " " 4 10 " " " " " " " 43 " " " " " " " " " " " " " " " * Husafjellet BERGARTER FREMSKJØVET UNDER DEN KALEDONSKE " " 17 # " " " " " " " 1 184 " " " " 42 " " " " Idse " 76 Dormåls- 5 " " 17 " " " " " * R " " " " " 8 " " # " Idsal 170 " " " Kalvberg " " " " e " FJELLKJEDEDANNELSEN # " # # " v * " " " 14 " " " " 706 " " " " " # s * " " " " " * " Storvarde " " 10 " n " " # #" -
Historiske Byrom Historiske Møteplasser I Sandnes
Torgdag på Gamlatorget, trolig i tidlig etterkrigstid. Foto Kolbjørn Rostrup. HISTORISKE BYROM HISTORISKE MØTEPLASSER I SANDNES Dokumentet er utarbeidet som: ➢ kunnskapsgrunnlag i plan og byggesaksprosesser. ➢ kunnskapsgrunnlag for de som ønsker å bli kjent med historien og lokal identitet gjennom fysiske spor ➢ supplement til registreringene i Kulturminneregisteret Arbeidet med å samkjøre kulturminnene i Forsand og Sandnes er påbegynt, og rapportene vil senere bli komplettert. Automatisk fredete kulturminner er ikke omtalt her. For informasjon om disse se Riksantikvarens database Askeladden. 0 Byantikvaren i Sandnes. Rev. 20.08.2020 INNHOLD Historiske byrom Innledning .............................................. 1 Typer historiske byrom .......................... 1 Historiske møteplasser i Sandnes Historiske byrom enkeltvis ..................... 9 Byens møterom ................................ 9 Neset/Kaien ...................................... 9 Moulandbrygga .............................. 10 Krossen .......................................... 10 Sandnes’ første jernbanestj ........... 11 Gamlatorget ................................... 11 Ruten – det nye torget ................... 18 Storkommunens nye rådhus .......... 19 Skeiane .......................................... 19 Parkene .......................................... 21 Jernbaneparken 21 Kirkeparken .................................... 21 Sykehusparken .............................. 22 Gandsparkene................................ 22 Jonas Øglænds plass ................... -
Fish Death in Mountain Lakes in Southwestern Norway During Late 1800S and Early 1900S – a Review of Historical Data
INNSENDTE ARTIKLER Fish death in mountain lakes in southwestern Norway during late 1800s and early 1900s – a review of historical data By Espen Enge, Tore Qvenild and Trygve Hesthagen E. Enge is researcher at University of Stavanger. T. Qvenild is senior engineer at Environmental Division, County Governor of Hedmark. T. Hesthagen is senior researcher at Norwegian Institute for Nature Research (NINA). Sammendrag 1930. Our results support the most recent hypo Fiskedød i fjellsjøer i Sørvest-Norge på slutten thesis, that a combination of “sea salt episodes” av 1800-tallet og begynnelsen av 1900-tallet – and emerging acidification may have contributed en gjennomgang av historiske data. to the fish death in the latter of these two periods. Mye av de historiske dataene om fisk og fiske bestander i fjellsjøer i SørvestNorge er i dag lite Introduction tilgjengelige. Her har vi skaffet til veie en rekke Due to the geography, comprising numerous av disse gamle datakildene, og har hentet ut data migration barriers, most of the trout (Salmo om fisk og fiskebestander. Disse gamle dataene trutta L.) in the inland and mountain areas in viser at aurebestandene i SørvestNorge ble sterkt Norway have at some point of time been stocked redusert eller døde ut, tilsynelatende i de to (HuitfeldtKaas 1924, Sømme 1941). At Hardan period ene 18601890 og 19101930. Våre funn gervidda mountain plateau (10001300 m a.s.l.), støtter hypotesen om at “sjøsaltepisoder”, kombi trout bones dating back to the Stone Age have nert med begynnende forsuring, kan ha vært been found (Indrelid 1994), and a discription of medvirkende årsak til fiskedøden, i hvert fall i Eilifr Elgr stocking fish (trout) in Lake Raudsjøen den siste perioden.