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. These different lithologies belong to different nappe complexes that were emplaced and folded into a series of syn- and anticlines during the Caledonian orogeny. These folds lead to different lithologies being exposed in different structural orientations on the opposite valley flanks, which in turn leads to different types and evolution of rock slope failures. For the present 2. The Vollan DSGSD is characterized by a steep major back scarp with its up to m-wide graben, which opened along the subvertical foliation in the quartzite, and a conspicuous array of counter-scarps in the micaschist. The morphologic features are explained by a flexural toppling mechanism in the micaschist, which likely initiated in the lower slope section and propagated retrogressively until reaching the massive quartzite at the back scarp.
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. You should realize, however, that the primary responsibility of these institutions is to preserve the records and to make them available for research use.
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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. If set in gravel, the wall could last many decades, even centuries. An archaeological excavation in Lund uncovered the postholes of several such churches.
GLACIAL LANDFORMS | Moraine Forms and Genesis
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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.
A stave church is a medieval wooden Christian church building once common in north-western name derives from the building’s structure of post and lintel construction, a type of timber framing where the load-bearing ore-pine posts are called stafr in Old Norse (stav in modern Norwegian).Two related church building types also named for their structural elements, the post .
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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.
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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 Videos provided by Youtube are under the copyright of their owners.
This list contains brief abstracts about monuments, holiday activities, national parcs, museums, organisations and more from the area as well as interesting facts about the region itself. Where available, you’ll find the corresponding homepage. Otherwise the related wikipedia article. The stave church is assumed to have been built around and still stands at its original location.
In , a series of samples from the logs were collected for dendrochronological dating of the church. The fjord is about 4 kilometres long.
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.
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Last flight on Bispen. Ground camera – Tomas Galasek. A Sognefjord Safari Slowly, they gouged u-shaped valleys that later filled with water, creating the defining feature of Norway’s landscap Sognefjord in a nutshell from Fjord Tour Flo Rida ft Sean Kingston – Roll full The stave church is assumed to have been built around and still stands at its original location. In , a series of samples from the logs were collected for dendrochronological dating of the church.
It is located in the county of Sogn og Fjordane, surrounding the Sognefjord. The fjord is about 4 kilometres long. On its south side lies the municipal centre of Balestrand. On the north side is the village of Dragsviki, which has ferry connections to Hella in Leikanger and to Vangsnes in Vik. The Tjugum church is located on the shore of the Esefjorden, just east of Dragsviki.
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Located between the Val d’Orcia and the hills of the Sienese Chianti, the farmhouse is on two floors: On the ground floor there is a living room with stone flooring, a fully equipped professional kitchen with dishwasher, fridge, and brick barbecue. On request possibility of cooking courses, wine tastings of the best Sienese wines and typical Tuscan dinners. The farmhouse, furnished with style and elegance, preserves the ancient terracotta flooring and wooden beamed ceilings and is part of a seven hectare estate composed of land and forest, surrounded by a large private garden with swimming pool, sun deck with river sand, and a small pond.
Thanks to its superb location the farmhouse is the ideal starting point to visit the Val di Chiana and Val d’Orcia with its wonderful medieval towns such as Cortona, Montepulciano, San Quirico d’Orcia, Pienza, as well as Montalcino and San Gimignano and the beautiful art towns of Siena, Florence and Arezzo.
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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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The village is located on the western shore of the Lustrafjorden , the innermost part of the Sognefjorden. The village sits directly across the fjord from the village of Ornes , where the famous 12th-century Urnes Stave Church is located. The village of Hafslo lies about 4 kilometres 2. The village is the site of the historic Walaker Hotel , dating back to about Solvorn Church , built in , is located in the village.
There has been a regular ferry route from Solvorn to Ornes, across the fjord, since
Ornes, Luster, Sogn og Fjordane county, Norway: Geographic coordinates: The earliest possible dating of this church is the early eleventh century. In the 17th century the nave of the church, which is a raised central room surrounded by an aisle, was extended southwards.
The two old parishes of Hopperstad and Hove was abolished in , and replaced by the new, united, Vik parish. The new Vik Church was finished in , and the two middle age churches of Hopperstad and Hove have sice then been museum churches. In , a series of samples from the logs were collected for dendrochronological dating of the church. A total of seven samples produced an estimate for the construction ranging from to and resulted in no definite conclusion. The only possible conclusion is that this is one of the oldest stave churches still standing.
History About years after its construction the church was abandoned and its exterior stripped. The church was in very poor condition for many years until the Society for the Preservation of Ancient Norwegian Monuments purchased the building in Using the Borgund Stave Church as a model, architect Peter Andreas Blix reconstructed the church between and During the reconstruction carved sections were found beneath the floor which indicates that the new church replaced an older church, which was probably built in the latter half of the 11th century.