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Lovatnet
Lovatnet (also Loenvatnet) is a lake in the municipality of Stryn in Vestland county, Norway. It is located about southeast of the village of Loen and about east of the village of Olden. The lake lies just southwest of the mountain Skåla. The water from the lake flows down from the mountains; especially from the Jostedalsbreen and Tindefjellbreen glaciers. It then flows out through the Loelva river into the Nordfjorden. Water from the tiered horsetail waterfall Ramnefjellsfossen with a total height of 818m flows into the lake from a short distance away, by some criteria among the highest dozen waterfalls in the world. It is fed by meltwater from the glacier Ramnefjellbreen, an arm of the Jostedalsbreen glacier. Landslides into the southern end of the lake from the mountain Ramnefjellet caused two major tsunamis in 1905 and 1936. On 15 January 1905, a landslide with a volume of fell into the lake from a height of , generating three megatsunamis of up to in height ...
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Megatsunami
A megatsunami is a very large wave created by a large, sudden displacement of material into a body of water. Megatsunamis have quite different features from ordinary tsunamis. Ordinary tsunamis are caused by underwater tectonic activity (movement of the earth's plates) and therefore occur along plate boundaries and as a result of earthquakes and the subsequent rise or fall in the sea floor that displaces a volume of water. Ordinary tsunamis exhibit shallow waves in the deep waters of the open ocean that increase dramatically in height upon approaching land to a maximum run-up height of around in the cases of the most powerful earthquakes. By contrast, megatsunamis occur when a large amount of material suddenly falls into water or anywhere near water (such as via a meteor impact or volcanic activity). They can have extremely large initial wave heights ranging from hundreds and possibly up to thousands of metres, far beyond the height of any ordinary tsunami. These giant wave hei ...
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Ramnefjellsfossen
Ramnefjellsfossen (also known as: Utigardsfossen or Utigordsfossen) is unofficially listed as the third-highest waterfall in the world in several publications. On the other hand, The World Waterfall Database, a waterfall enthusiast website, which includes all minor and seasonal waterfalls in the country, lists it as eleventh-tallest. The falls are located on the mountain, Ramnefjellet, in the municipality of Stryn in Vestland county, Norway–about southeast of the villages of Loen and Olden. The tiered horsetail waterfall has four drops measuring , with the longest single drop measuring . The average width of the falls are over the long run from top to bottom. The average flow of the falls are , with the best flow in the summer. The falls are fed by the Ramnefjellbreen glacier, an arm of the great Jostedalsbreen glacier. After the falls, the water flows into the lake Lovatnet. The falls are easily reached by boat, sea plane, or road, and a campsite is located within ...
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Loen, Norway
Loen is a village in Stryn Municipality in Vestland county, Norway. It is located in the inner part of the Nordfjord region, at the easternmost end of the Nordfjorden. Loen is located about north of the village of Olden and about southeast of the municipal center of Stryn. The lake Lovatnet is located just to the southeast of the village of Loen. The Hotel Alexandra was established in Loen in 1884. The historic Loen Church is also located in the village. History Loen is the home to some of the oldest farms in Norway: ''Sæten'' (Setin), ''Tjugen'' (Tyfin), and ''Loen''. They were probably established long before the time of Christianity. Much of the upper Loen valley was devastated from two rockfall slides (one in 1905 and one in 1936) that created huge waves that swept with them most of the houses and vegetation. A total of 135 people were killed in these two incidents. Attractions Some nearby attractions include the Jostedalsbreen nasjonalparksenter museum, Jostedalsbreen ...
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Stryn
Stryn is a municipality in the county of Vestland, Norway. It is located in the traditional district of Nordfjord. The administrative center of the municipality is the village of Stryn. The municipality is located along the innermost part of the Nordfjorden. Some of the main villages in Stryn include Loen, Innvik, Utvik, Randabygda, Olden, and Flo. Farming, forestry, fruit growing, animal breeding for furs, small manufacturing industries, tourism, and the service trades provide the main occupations. The wide river Stryneelva enters the village of Stryn from the east after meandering through the fertile Stryn Valley, from the large lake Oppstrynsvatn. The Jostedalsbreen National Park Centre is situated on the shore of this lake. At the east end of the lake, the road enters the narrower Hjelledalen and shortly zigzags up some to Ospeli and the entrance of the first of the three tunnels of the mountain highway ( Riksvei 15) leading to Geiranger and Grotli. Stryn is kno ...
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List Of Lakes In Norway
This is a list of lakes and reservoirs in Norway, sorted by county. For the geography and history of lakes in that country, see Lakes in Norway, including: * List of largest lakes in Norway * List of deepest lakes in Norway Akershus *Bjørkelangen * Bogstadvannet *Dælivannet * Engervannet * Hallangen *Hurdalsjøen * Lyseren *Mangen * Mjøsa *Øgderen * Østernvann * Øyangen (Gran) *Øyeren *Rødenessjøen *Setten Aust-Agder *Åraksfjorden * Blåsjø *Botnsvatnet *Botsvatn * Breidvatn *Byglandsfjorden * Fisstøylvatnet * Grøssæ * Gyvatn *Hartevatnet *Herefossfjorden * Holmavatnet * Holmevatnet *Homstølvatnet *Hovatn *Høvringsvatnet *Kilefjorden * Kolsvatnet *Kvifjorden *Longerakvatnet *Måvatn * Myklevatnet *Nasvatn *Nelaug * Nesvatn *Nystølfjorden *Ogge *Ormsavatnet * Østre Grimevann * Øyarvatnet * Ramvatn *Reinevatn * Rore *Rosskreppfjorden * Sæsvatn *Skyvatn *Store Bjørnevatn *Store Urevatn * Straumsfjorden * Svartevatnet *Syndle *Topsæ *Uldalsåna *Vatndals ...
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Tindefjellbreen
Tindefjellbreen is a glacier in the municipality of Stryn in Vestland county, Norway. The glacier lies about east of the mountain Skåla, roughly halfway between the villages of Bødalen and Erdalen. The glacier is in the mountains east of the lake Lovatnet and south of the lake Oppstrynsvatn. The glacier is part of Jostedalsbreen National Park, about east of the village of Loen. See also *List of glaciers in Norway These are the largest glaciers on mainland Norway.The largest glaciers ...


References

Stryn Glaciers of Vestland {{Vestland-geo-stub ...
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Nordfjorden (Sogn Og Fjordane)
Nordfjorden is the sixth longest fjord in Norway. It flows through the municipalities of Stryn, Gloppen, Stad, Bremanger, and Kinn, and it is the central feature of the entire Nordfjord region which makes up the northern third of the county. The long fjord stretches from Husevågøy island in Kinn Municipality to the village of Loen in Stryn Municipality. The fjord starts as runoff from the Jostedalsbreen, Europe's largest mainland glacier, in the east and it flows west, emptying into the ocean just south of the Stadlandet peninsula. The mouth of the fjord lies between the large islands of Vågsøy and Bremangerlandet (with the smaller island of Husevågøy lying in the middle of the mouth). There are several smaller fjords which branch off the main Nordfjorden: Eidsfjorden, Ålfotfjorden, Hyefjorden, and Gloppefjorden. The fjord reaches a maximum-depth of near the mouth of the Eidsfjorden and also by the village of Bryggja. Transportation The fjord has no road or ...
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Lakes Of Vestland
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Loelva River
The Alna River''Berlitz: Oslo Pocket Guide''. 2013. London: Berlitz. ( no, Alnaelva) is a river that runs through Oslo, Norway, from Alnsjøen to the Oslo Fjord at Bjørvika. It also drains Breisjøen, Steinbruvann, Tokerudbekken, and Østensjøvannet. It runs through the boroughs of Gamle Oslo, Nordstrand, Helsfyr, Østensjø, Alna, and Grorud. Large sections of the river run in culvert A culvert is a structure that channels water past an obstacle or to a subterranean waterway. Typically embedded so as to be surrounded by soil, a culvert may be made from a pipe, reinforced concrete or other material. In the United Kingdom ...s and the river is highly polluted, partially because it is used as a sewer drain. The Municipality of Oslo is creating linked walking trails and green spaces along the length of the Alna. References Rivers of Oslo Rivers of Norway {{Norway-river-stub ...
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Grain Mill
A gristmill (also: grist mill, corn mill, flour mill, feed mill or feedmill) grinds cereal grain into flour and middlings. The term can refer to either the grinding mechanism or the building that holds it. Grist is grain that has been separated from its chaff in preparation for grinding. History Early history The Greek geographer Strabo reports in his ''Geography'' a water-powered grain-mill to have existed near the palace of king Mithradates VI Eupator at Cabira, Asia Minor, before 71 BC. The early mills had horizontal paddle wheels, an arrangement which later became known as the " Norse wheel", as many were found in Scandinavia. The paddle wheel was attached to a shaft which was, in turn, attached to the centre of the millstone called the "runner stone". The turning force produced by the water on the paddles was transferred directly to the runner stone, causing it to grind against a stationary "bed", a stone of a similar size and shape. This simple arrangement required ...
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Sawmill
A sawmill (saw mill, saw-mill) or lumber mill is a facility where logs are cut into lumber. Modern sawmills use a motorized saw to cut logs lengthwise to make long pieces, and crosswise to length depending on standard or custom sizes (dimensional lumber). The "portable" sawmill is of simple operation. The log lies flat on a steel bed, and the motorized saw cuts the log horizontally along the length of the bed, by the operator manually pushing the saw. The most basic kind of sawmill consists of a chainsaw and a customized jig ("Alaskan sawmill"), with similar horizontal operation. Before the invention of the sawmill, boards were made in various manual ways, either rived (split) and planed, hewn, or more often hand sawn by two men with a whipsaw, one above and another in a saw pit below. The earliest known mechanical mill is the Hierapolis sawmill, a Roman water-powered stone mill at Hierapolis, Asia Minor dating back to the 3rd century AD. Other water-powered mills followe ...
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