Geomorphology Abstract For the past three years NGU has worked on 25 unstable and potentially unstable rock slopes in Sogn og Fjordane. Mapping on land included structural mapping of ten sites by on-site field mapping and nine sites by remote structural mapping using terrestrial laser scanning technology TLS. Synthetic Aperture Radar was app lied for the entire county but slide velocities could only be mapped out at one locality at Osmundneset Gloppen municipality. Three large instabilities have been discovered or taken into the monitoring program. These are Osmundneset in Gloppen municipality, Skrednipa in Sogndal municipality, and the Ovris valley in Vik municipality. The largest movements with 1. Our data suggest a slight acceleration of this instability. Acceleration was also documented for a However at that site a collapse of a rockslope with a volume of
Construction[ edit ] Gol stave church , belonging to the Borgund group. The drawing is slightly erroneous, as the sill under the church floor is missing. Archaeological excavations have shown that stave churches, best represented today by the Borgund stave church , are descended from palisade constructions and from later churches with earth-bound posts. Similar palisade constructions are known from buildings from the Viking Age. Logs were split in two halves, set or rammed into the earth generally called post in ground construction and given a roof.
This proved a simple but very strong form of construction.
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Ferry trip along the deepest and longest fjord in Norway. Enjoy the stunning views! A Sognefjord Safari Published: March 03, Rating: Rick Steves Europe Glaciers spent eons carving up western Norway as they worked their way to the sea. Slowly, they gouged u-shaped valleys that later filled with water, creating the defining feature of Norway’s
Bygstad is a village in Gaular Municipality in Sogn og Fjordane county, Norway. The village is located on the northern shore of the Dalsfjorden, about 2 kilometres ( mi) northwest of .
Abstract The investigation of textiles and textile production can yield important information about the infrastructure and resource management in ancient societies. Before the 19th century textiles made of plant material in Scandinavia were mainly made from locally available raw materials: This investigation demonstrates that hemp, in some cases at least, was also used for fine textile production in Viking Age Scandinavia.
The aim of this paper is to investigate this topic further. The collection is extensive and belongs to one of the oldest archaeological collections in Norway. It contains finds from western Norway mainly. We identified a total of 45 grave finds with more than different weaves in the collection. Plant fibres do not keep well under the burial conditions in Norway, but we managed to identify ten non-mineralized and non-charred finds with fragments of plant fibre material belonging most probably to clothing and accessories.
Fibres from these ten finds were investigated using the modified Herzog test. In addition, morphological features were observed carefully. Nine samples were identified as flax, one sample could only be identified as a bast fibre.
Statsarkivet i Kongsberg, for Buskerud, Vestfold and Telemark fylker. Statsarkivet i Hamar, for Hedmark and Oppland fylker. Statsarkivet i Stavanger, for Rogaland fylke. How the archives can help you If you know where your family came from, you should approach the statsarkiv for that district. In most cases, the regional archives are the best places to start your investigation.
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The method and physical process behind the making of hunters’ rock art in Western Norway: An Approach for a better dating and understanding of their meaning and function. Vingen – et naturens kolossalmuseum for helleristninger. The World Heritage Site in Alta. The rock art of Norway. Samfunn, symboler og identitet. Sikring av Bergkunst – Forvitringsfaktorer og bevaringstiltak. Dating of rock art and the effect of human activity on vegetation: The complementary use of archaeological and scientific methods.
Human induced land-cover changes in western Norway. Boletin de la Asociacion Latinamericana de Paleobotanica y Palinologia. Treatment of corpses, consumption of the soul and production of rock art: Approaching Late Mesolithic mortuary practises reflected in the rock art of Western Norway.
History Location in Sognefjord map of Norway inserted The church was built around or shortly thereafter, and still stands in its original location; it is believed to be the oldest of its kind. It provides a link between Christian architecture and the architecture and artforms of the Viking Age with typical animal-ornamentation, the so-called ” Urnes style ” of animal-art. Archaeological investigations have discovered the remains of three churches on the site prior to the current building.
It is not known if this church had a raised roof above the central space of the nave like the present church. The earliest possible dating of this church is the early eleventh century.
Fjærland. Fjærland is located in Sogndal municipality in Sogn og Fjordane. Here, the mighty Sognefjord meets the Jostedalsbreen Glacier and lots of peopleconsider Fjærland to be the most beautiful glacier village in the world!
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Brev til komitemedlemmane, 19 Notat med tilrding Hovedorganisasjon: Hageselskapet Sogn og Fjordane Stiftet: Vi samler inn informasjon om alle som besker oss.
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But they can be deciphered in the following way: Transport[ edit ] Transport is made more difficult because of the fjords and the mountains. These schedules are however only found in Norwegian. Route 55 from Lom is a beautiful scenic drive over the highest mountain pass in Norway, m ft above sea level. Gulen and Solund are part of the Hordaland police district.
Schedules for all public transportation can be found on internet. The country is divided into 19 counties. By rail[ edit ] Sogn og Fjordane has only one railway line. However with some planning it is possible to experience Sogn og Fjordane by bus. A county is also an election area, with popular votes taking place every 4 years. Gulen and the rest of the Nordhordland district of the county of Hordaland All of the municipalities of Sogn og Fjordane except Gulen and Solund are part of the Sogn og Fjordane police district.
Low pressure systems come in from the west and meet the mountains a phenomenon known as orographic lifting and cause rain and snowfall.
Urnes Stave Church
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Available online 10 April 10 April The wide variety of features that are traditionally classified by glacial geomorphologists as moraines include both terrestrial and subaqueous forms and the impressive structures created by glacitectonic disturbance. This chapter concentrates specifically on all those landforms deposited at the margins and on the surface of glaciers and ice sheets with the exception of large glacitectonic structures, because they are the subject of another chapter.
Moraines are here classified according to the process-form relationships involved in their construction. They are deposited in three environments, including terrestrial glacier and ice sheet margins, supraglacial settings, and the subaqueous margins of glaciers. Terrestrial glacier margins produce push and squeeze moraines, dump moraines, and ice-marginal aprons and laterofrontal fans and ramps including features traditionally termed lateral and terminal moraines.
Ice shelf moraines are constructed at the terrestrial-marine interface. Supraglacial deposition results in the englacial and supraglacial production of moraines that are progressively lowered onto the substratum by glacier ablation, including medial moraines, hummocky moraines, and controlled moraines. However, because mass movement, glaciofluvial and glaciolacustrine processes work in juxtaposition on melting glacier surfaces, they are commonly characterized by hybrid sediment-landform associations that include medial, hummocky, and controlled moraines in addition to kame and kettle topography, ice-walled lake plains, kame terraces, and pitted sandar.
Subaqueous ice-marginal environments are characterized by moraines deposited at or close to the grounding lines of water-terminating glaciers, including morainal banks and subaqueous grounding line fans and De Geer moraines.
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Abstract The long-term evolution of rock slope failures involves different stages, from incipience of slope instability to catastrophic failure, through a more or less long-lasting slope deformation phase that also involves creeping or sliding. Topography, lithology, and structural inheritance are the main intrinsic factors that influence this evolution. Here, we investigate the role of these intrinsic factors on the rock slope failure development of the Ivasnasen and Vollan rock slopes Sunndal Valley, western Norway using a multitechnique approach that includes geomorphologic and structural field mapping, kinematic analysis, terrestrial cosmogenic nuclide exposure dating, topographic reconstruction, and deformation quantification.
Ivasnasen is a rock slope failure complex with several past rock slope failures and a present unstable rock slope, located on a cataclinal NW-facing slope and developed in augen gneiss. Vollan on the opposite valley side is a deep-seated gravitational slope deformation DSGSD affecting the whole mountainside, developed in quartzite in the upper part and micaschist in the lower part.
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