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Western Karmøy, an Integral Part of the Precambrian Basement of South Norway
WESTERN KARMØY, AN INTEGRAL PART OF THE PRECAMBRIAN BASEMENT OF SOUTH NORWAY TOR BIRKELAND Birkeland, T.: Western Karmøy, an integral part of the Precambrian basement of south Norway. Norsk Geologisk Tidsskrift, Vol. 55, pp. 213-241. Oslo 1975. Geologically, the western side of Karmøy differs greatly from the eastern one, but has until recently been considered to be contemporaneous with the latter, i.e. of Caledonian age and origin. The rocks of western Karmøy often have a distinctly granitoid appearance, but both field geological studies and labora tory work indicate that most of them are in fact metamorphosed arenaceous rudites which have been subjected to strong regional metamorphism under PT conditions that correspond to the upper stability field of the amphibolite facies, whereas the Cambro-Ordovician rocks of the Haugesund-Bokn area to the east have been metamorphosed under the physical conditions of the green schist facies. From the general impression of lithology, structure, and meta morphic grade, the author advances the hypothesis that the rocks of western Karmøy should be related to a Precambrian event rather than to rock-forming processes that took place during the Caledonian orogeny. T. Birkeland, Liang 6, Auklend, 4000 Stavanger, Norway. Previous investigations The first detailed description of the rocks of western Karmøy was given by Reusch in his pioneer work from 1888. Discussing the mode of development of these rocks, he seems to have inclined to the opinion that the so-called 'quartz augen gneiss' and the other closely related rocks represent regionally metamorphosed clastic sediments. Additional information of the rocks con cerned is found in his paper from 1913. -
27 Aristocratic Presence Along the Karmsund Strait 2000 BC–AD 1368
Dagfinn Skre 27 Aristocratic Presence along the Karmsund Strait 2000 BC–AD 1368 Pursuing the ARM research strategy (Ch. 4), this chapter summarises, analyses, and contextual- ises the evidence on aristocratic presence at Avaldsnes and along the Karmsund Strait presented in previous chapters in this book. In SP I (2000–350 BC) aristocratic presence was introduced and long-distance overseas connections to southern Scandinavia were established. In SP II (350 BC–AD 200) these connec- tions were maintained, warrior burials were introduced, and agrarian production increased, probably leading to population increase. In SP III (AD 200–600) major changes occurred. Princely graves were entombed in the ancient Flaghaug mound, a prominent stone monu- ment was raised, a monumental hall building, a boathouse, and a longhouse were erected; most of these buildings and monuments are without parallel in western Scandinavia, while the stone monument and one of the graves are unique in the whole of Scandinavia. The evi- dence for aristocratic presence is strong in SP III’s first two centuries, somewhat weaker in its latter two centuries. Features are few from SP IV (AD 600–900), the most substantial of which are remains of a palisade, which indicates external threats and hostilities as well as local mil- itary capabilities. Near Avaldsnes, the Salhus mound from early SP IV and the Grønhaug and Storhaug shipgraves from late SP IV provide evidence for aristocratic presence in this period. In early SP V (AD 900–1250) food-processing activities in the farmyard increase, and around the turn of the millennium a building appears to have been raised on the location where the hall building stood in SP III. -
Rennesøy Finnøy Bokn Utsira Karmøy Tysvær Haugesund Vindafjord
227227 ValevValevåg Breiborg 336 239239 Ekkje HellandsbygHellandsbygd 236236 Hellandsbygda Utbjoa SaudaSauda 335 Etne Sauda Bratland 226226 Espeland VihovdaVihovda Åbødalen Brekke Sandvikdal Roaldkvam 240240 241241 Kastfosskrys 334 Egne Hjem UtbjoaUtbjoa Saunes 236 Skartland sør EtneEtne en TTråsavikikaaNærsonersone set 225225 Saua Førderde Gard Kvame Berge vest Ølen kirke Ølen Ørland Hytlingetong Gjerdevik ø EiodalenØlen skule den 332 SveioSveio 222222 Ølensvåg 235235 333 st Hamrabø Bråtveit Saudafjor 237237 224224 Øvrevre VatsVats SvandalSvandal MaldalMaldal 223223 Vindafjord SandeidSandeid Ulvevne Øvre Vats Skole Bjordalsveien Sandeid Fjellgardsvatnet Hylen Landa Løland Tengesdal 223 331 Knapphus Hordaland Østbø Hylen Blikrabygd 238238 Sandvik VanvikVanvik 328328 Vindafjord Hylsfjorden Skrunes SuldalseidSuldalseid Skjold 216216 218218 Sandeidfjorden 230230 Suldal NordreNordre VikseVikse Ørnes 228228 RopeidRopeid Isvik SkjoldSkjold Hustoft VikedalVikedal 217217 Slettafjellet Nesheim Vikedal Helganes 228 330330 Vikse kryss VestreVestre Skjoldafjo Eskedalen 221221 Suldalseid SuldalsosenSuldalsosen Haugesund Stølekrossen Førland Åmsoskrysset Åmsosen IlsvIlsvåg Stole Ølmedal Kvaløy Ropeid Skipavåg Sand Suldalsosen rden 230 Byheiene 229229 Roopeid 327 327327 Stakkestad SkipevSkipevåg kryss SandSand Kariås Røvær kai Nesheim Eikanes kryss Lindum Årek 329329 camping 602 VasshusVasshus Røvær 200200 220220 Suldalsl HaugesundHaugesund ågen Haraldshaugen 205205 Kvitanes Grindefjorden NedreNedre VatsVats Vindafjorden Kvamen Haugesund Gard skole -
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. -
Experience Karmøy
E39 E134 Experience BUS SERVICE TO E134 VANDVIK ØRJAN B. IVERSEN, CAMILLA APPEX.NO / PHOTOS: OSLO, BERGEN, AKSDAL STAVANGER HAUGESUND DYRAFJELLET 172 M.A.S.L Karmøy FAST FERRY: N HAUGESUND - FEØY 20 MIN 9-HOLES HAUSKE GÅRD MINIGOLF 18-HOLES E134 VIKING FARM VISNES MINE AREA KVEITEVIKEN THE FIVE POOR MAIDENS E39 FV47 OLAV’S CHURCH E134 STATUE OF LIBERTY HAUGESUND AIRPORT, E134 KARMØY FV47 HÅVIK HØYEVARDE BUS SERVICE 19 KM K AR TO STAVANGER MØYTUNNELEN AND BERGEN NORDVEGEN HISTORY CENTRE FV47 16 KM Haugalands- KARMØY FISHERY MUSEUM vatnet VEAVÅGEN 12 KM FV47 KOPERVIK ÅKREHAMN COASTAL MUSEUM FV511 ÅKREHAMN 4 KM BEAUTIFUL SILKY BEACHES B SÅLEFJELL PEAK UR MA VE GE BOATHOUSES N AT HOP 8 KM E39 13 KM 8 KM 9-HOLES GREAT SURFING BEACHES FERRY: ARSVÅGEN - MORTAVIKA 20 MIN SKUDENESHAVN JUNGLE PARK STAVANGER HISTORIC SKUDENESHAVN SYRENESET FORT THE MUSEUM IN MÆLANDSGÅRDEN SKUDENESHAVN VIKEHOLMEN GEITUNGEN SIGHTSEEING HIKING AND BIKING TRAILS ACCOMMODATION COMMUNICATIONS Avaldsnes Viking Farm. Follow in the foot- The Karmøy countryside is attractive and diverse Park Inn, Haugesund Airport Hotel Airlines steps of the ancient kings through the historic with many opportunities to get outdoors and Helganesveien 24, 4262 Avaldsnes RyanAir: T: +47 52 85 78 00, www.ryanair.com landscape at Avaldsnes. Bukkøy island features be active or simply relax: T: +47 52 86 10 90 Norwegian: T: +47 815 21 815, www.norwegian.no many reconstructed Viking buildings. Meet www.haugalandet.friskifriluft.no E-mail: [email protected] SAS: T: +47 05400, www.sas.no Vikings for activities and tours in the summer www.parkinnhotell.no/hotell-haugesund Widerøe: T: +47 810 01 200, www.wideroe.no season. -
Det-Norske-Myrselskap-1949
MEDDELELSER FRA DET NORSl(E MYRSELSl(AP Nr. 6 Desember 1949 47. årgang Redigert av Aasulv Løddesøl. MYRENE I KYSTHERREDENE I NORD-ROGALAND. Av konsulent Ose. Hovde. Nord-Rogaland er vanlig benevnelse for den del av Rogala,nd fylke som ligger nord for Boknafjorden. De typiske kystherreder i Nord-Rogaland - regnet nordfra -- er følgende 8: Skåre, Torvastad, Avaldsnes, Utsira, Åkra, Stangaland, Skudenes og Bokn. Innen dette kystområde ligger også 3 bykommuner, nemlig Haugesund, Kopervik og Skudeneshavn. Nærmere geografisk bestemt ligger disse herreder mellom 59°08' og 59°31' nordlig bredde og mellom 5~10' og 6° vestlig lengde (Oslo meridian). Herredenes totalareal er 407,96 km2 og land• arealet 392,02 km2• Av hele Rogaland fylke utgjør dette område 4,50 %. Det meste av Skåre og Avaldsnes herreder med Haugesund by og en mindre del av Torvastad ligger på fastland (Haugalandet), men for øvrig ligger de andre herreder på øyer. Den største av disse er Karmøya. Her ligger de tre herreder Skudenes, Akra og Stanga• land i sin helhet og dessuten det meste av Torvastad og en del av Avaldsnes. Her er dessuten de to bykommuner Kopervik og Skude·• neshavn. Karmøya er således Norges folkerikeste og tettest bebodde øy. Bokn herred ligger på flere øyer øst for Karmøya, og Utsira her• red ligger langt ute i havet (16 km) rett vest av Karmøya, Kommunikasjonene innen området er stort sett gode, men den svære trafikk over Karmsundet ·gjør krav om bru eller bedre ferje• forbindelse berettiget. Ruten på Karmøya trafikeres med busser av Norges Statsbaner. F j e 11 grunnen innen området består stort sett av 3 temmelig skarpt atskilte områder. -
Norway Maps.Pdf
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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. -
Rural Infant Mortality in Nineteenth Century Norway1
Rural Infant Mortality in Nineteenth Century Norway1 Gunnar Thorvaldsen uch previous research on the Norwegian mortality decline has focused on specific localities, employing databases with linked microdata. One Mgood choice is Rendalen, a parish on the Swedish border, representative of the world record low Norwegian mortality rates. The focus on the role of women, given their access to more abundant material resources towards the end of the eighteenth century, is a most interesting explanation for the declining level of infant mortality.2 Another well-researched locality is the fjord-parish Etne, south of Bergen, where infant mortality was significantly higher – also an area where the role of women is highlighted. More recent studies have been done on Asker and Bærum, south of Oslo, with infant mortality levels closer to the national average. The present article will not attempt to match these penetrating studies of well- researched rural localities, nor William Hubbard’s insights into many aspects of urban mortality.3 Rather it broadens the scope to include the whole country. My study is limited primarily to Norway’s sparsely populated rural areas, where 90 percent of the population lived in 1801, a figure that was declining towards 60 percent by 1900, when the national infant mortality rate (IMR) had fallen below ten percent.4 My basic aim is to track the development of infant mortality rates in Norway over time, and, where possible, to say something about regional differences in the proportion of children who died before they reached their first birthday. The 1 Another version of this article will also be published inStudies in Mortality Decline. -
Karmøy-Kopervik
Karmøy - Kopervik Prisant: 20 000 000 + omk Gofarnes, 4250 Kopervik Meglerhuset Rele er i dag ledende aktør innen nærings- megling på Haugalandet, Sunnhordland, Sauda og Odda og distriktene rundt, og utfører tjenester innen salg, utleie, verdivurdering og rådgivning. Vi har lang erfaring, unik kompetanse og svært god kjennskap til markedet, hvilke er avgjørende suksessfaktorer ved kjøp og salg av nærings- eiendom. Som kunde hos Meglerhuset Rele kan en være trygg på at en blir ivaretatt på en profesjonell måte. Meglerhuset Rele - det komplette meglerhuset 2KOPERVIK GOFARNES DIN MEGLER PÅ DENNE EIENDOMMEN: Jan Audun Lutro Næringsmegler T: 90 22 22 91 [email protected] Jan Audun Lutro er daglig leder og næringsmegler i Meglerhuset Rele. Han har jobbet med næringseiendom i mange år, og er en engasjert og profilert figur i næringslivet på Haugalandet og omegn. Med sin brede erfaring, lune vesen og sjarmerende Hardingmål er Jan Audun det naturlige samarbeidsvalget for mange. KOPERVIK GOFARNES 3 4KOPERVIK GOFARNES Del 1 -Gofarnes Eiendommen Bilder - Eiendomsinfo KOPERVIK GOFARNES 5 Nøkkelinfo 6KOPERVIK GOFARNES EIENDOMSTYPE: PRISANTYDNING: Boligtomt Kr.20 000 000 + omk. EIENDOMSBETEGNELSE: TOMT: Gnr.66 Bnr.26 iKarmøy Areal: 26474 m2 KOPERVIK GOFARNES 7 Høydepunkter Regulert tomteområde til sjø til salgs Gofarnes er et boligprosjekt med praktfull beliggenhet med utsikt mot Karmsundet. Tomten som selges er nevnt i regulering som B1a, B1b, B1c og B2 og er på totalt 26.474 m2. B1a: 3,1 daa, 35% BYA, mønehøyde 12 m, gesimshøyde 9 m. Mulig utbygging pr plan 1085 m2, over 3,5 plan. Totalt ca 3.800 m2 B1b: 5,4 daa, 35% BYA, mønehøyde 12 m, gesimshøyde 9 m. -
ROGALAND 23. JULY – 4. AUGUST 2014 Sunday the 27Th We Traveled
ROGALAND 23. JULY – 4. AUGUST 2014 Sunday the 27th we traveled to Karmøy. We drove Here we have parked. through the new tunnel in the triangular connection to Skudesneshavn. We stopped at Skudenes Camping. We parked at this place. The following day, Sunday the 28th, we took a trip down to Skudesneshavn. Those who live here can park their boat right outside Here we are at Kanalen. their door. View across the strait to Vaholmen. Terraces with moored boats. View south towards the bridge that goes over to Skudenes Mekaniske Verksted was built in 1916. Here Steiningsholmen. were the Skude engines produced. I the end of the house is written the name on the wall. Here we come to the square located down by the harbor. Skudeneshavn is a town and a former municipality in Karmøy municipality in Rogaland. Skudesneshavn had 3,327 inhabitants as of 1 January 2013, and is located on Skudeneset on the southern tip of the island Karmøy. Skudesneshavn grew up in the late Middle Ages and the urban society grew rapidly during the herring fishery in the 1800s.Today, the city has modern shipbuilding industry and one of the largest offshore shipping. Solstad Offshore has one of the world's most advanced offshore fleets in service throughout the world. The well-preserved wooden buildings along the harbor, Søragadå, has become one of the region's most visited tourist destination. The flounder fisherman The lobster fisherman The statues in Nordmand valley, Denmark In Nordmandsdalen in Fredensborg Palace Gardens stand 60 statues from various parts of Norway. -
Administrative and Statistical Areas English Version – SOSI Standard 4.0
Administrative and statistical areas English version – SOSI standard 4.0 Administrative and statistical areas Norwegian Mapping Authority [email protected] Norwegian Mapping Authority June 2009 Page 1 of 191 Administrative and statistical areas English version – SOSI standard 4.0 1 Applications schema ......................................................................................................................7 1.1 Administrative units subclassification ....................................................................................7 1.1 Description ...................................................................................................................... 14 1.1.1 CityDistrict ................................................................................................................ 14 1.1.2 CityDistrictBoundary ................................................................................................ 14 1.1.3 SubArea ................................................................................................................... 14 1.1.4 BasicDistrictUnit ....................................................................................................... 15 1.1.5 SchoolDistrict ........................................................................................................... 16 1.1.6 <<DataType>> SchoolDistrictId ............................................................................... 17 1.1.7 SchoolDistrictBoundary ...........................................................................................