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Hornelen
Hornelen is a mountain in Bremanger Municipality in Vestland county, Norway. The mountain sits on the eastern end of the island of Bremangerlandet, along the Frøysjøen strait, in the Nordfjord region of Norway. At , it is the highest sea cliff in Europe (see illustration left), and has for a long time been used as a landmark for naval navigation. It is a 4-hour hike to the summit from Berleneset (across the small fjord from the village of Berle). The horizontal distance from the summit to the sea is approximately . Approximately to the west of the cliffside is the highest point on the island Bremangerlandet, called Svartevassegga which has an elevation of . The rock in Hornelen consists of sandstone of Devonian age, and it constitutes an important part of the geology of Norway. See also *List of mountains of Norway There are 291 peaks in Norway with elevations of over above sea level and that have a topographic prominence of more than 10 meters. The following list inc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bremanger Municipality
Bremanger is a municipality in Vestland county, Norway. The village of Svelgen is the administrative centre of the municipality. Other villages include Bremanger, Berle, Davik, Isane, Kalvåg, Svelgen, Rugsund, and Ålfoten. Bremanger is the only municipality in Vestland, which is located in two districts. The northern and eastern parts comprising the villages of Oldeide, Berle, Rugsund, Davik, Isane, and Ålfoten is located in the Nordfjord region, while the villages of Bremanger, Kalvåg, Svelgen, Sørgulen, and Botnane are located in the Sunnfjord region. Politically, the municipality works with the Nordfjord region in the council of Nordfjord municipalities. Bremanger has many tourist destinations such as Kalvåg, which has one of the largest and best-kept waterfront environment in the county, the Grotlesanden ocean beach, the Hornelen mountain, with the tallest sea cliff in Northern Europe, Rock carvings at Vingen, and the old trading stations of Rugsund and Smørhavn. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bremangerlandet
Bremangerlandet is an island in Bremanger Municipality in the traditional district of Nordfjord in Vestland county, Norway. The island is one of the largest islands in the county. The highest point on the island is the tall mountain Svartevassegga, however the cliff at Hornelen, located to the east, is more well-known and has an elevation of . The long lake Dalevatnet is located in the central part of the island. The island is located northeast of the smaller island of Frøya. Bremangerlandet island lies on the southern side of the mouth of the large Nordfjorden and the island of Vågsøy lies on the north side of the fjord's mouth. The small island of Husevågøy lies in the middle of the fjord, just north of Bremangerlandet. The island is connected to the island of Frøya (to the southwest) by a series of bridges. There is a ferry connection to Husevågøy and Vågsøy islands to the north. There is also a road that connects Bremangerlandet to the island of Rugsundà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Norway
The geology of Norway encompasses the history of Earth that can be interpreted by rock types found in Norway, and the associated sedimentological history of soils and rock types. The Norwegian mountains were formed around 400 million years ago (Ma) during the Caledonian orogeny. Precambrian Rocks of Archean age in Norway are confined to a few 10 km-scale areas within younger metamorphic belts exposed on islands off the west coast of northern Norway and as smaller fragments locally in the Western Gneiss Region in south-central Norway. Despite intense reworking during the Caledonian orogeny in some areas, three major belts can be recognised in the Proterozoic rocks of Norway, the Neoproterozoic and Mesoproterozoic Gothian and Sveconorwegian, the Palaeoproterozoic Svecokarelian and the intervening Transscandinavian Igneous Belt of late Palaeoproterozoic age. About 1400 million years ago in the Mesoproterozoic tectonic extension and continental magmatism led to the formatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berle
Berle is a village on the west coast of Norway. It is located on the eastern coast of Bremangerlandet island in the municipality of Bremanger in Vestland county. The village lies along the Berlepollen fjord, a small inlet off the Frøysjøen strait which separates it from the mainland. The village of Berle lies about west of the Hornelen cliff and about a drive west from the village of Bremanger. Berle Church is located in the village, serving the people in this part of the municipality. The population (2001) of the village is 135. Name The name of the village comes from the name of the small river nearby ( non, Berðla). The small Berlepollen fjord nearby is similarly named. The name ''Berðla'' comes from the Old Norse word ''barð'', meaning "edge", possibly since it is on the edge of the island. The village's name is mentioned as early as in the Egils saga. History The history of Berle goes back to the 8th century. The best known Viking who lived there at the time ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frøysjøen
Frøysjøen is a fjord (or more accurately, a strait) in Bremanger Municipality in Vestland county, Norway. The fjord is about long and between wide. The fjord runs on a northeast–southwest axis between the mainland of Norway (on the east) and the islands of Bremangerlandet and Frøya (on the west). The Gulen fjord branches off the Frøysjøen to the east. The main settlements along the fjord include Kalvåg and Berle on the western shore. The mountain Hornelen lies along the shore of the fjord, northeast of Berle. The fjord connects with the open ocean on the west end and it connects to the Nordfjorden on the northeast end. The fjord is a main shipping lane between the towns of Måløy and Florø is a town and the administrative centre of the municipality of Kinn, Vestland, Norway. The town was founded by royal decree in 1860 as a ladested on the island of Florelandet, located between the Botnafjorden and Solheimsfjorden. Florø is No .... References Fjord ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vestland
Vestland is a county in Norway established on 1 January 2020. The county is located in Western Norway and it is centred around the city of Bergen, Norway's second largest city. The administrative centre of the county is the city of Bergen, where the executive and political leadership is based, but the County Governor is based in Hermansverk. The county is one of two counties in Norway that have Nynorsk as their official written language form (the others are neutral as to which form people use). Vestland was created in 2020 when the former counties of Hordaland and Sogn og Fjordane (with the exception of Hornindal municipality, which became part of Volda municipality in Møre og Romsdal county) were merged. History Vestland county is a newly created county, but it has been inhabited for centuries. The area was made up of many petty kingdoms under the Gulating during the Middle Ages. The northern part was the known as ''Firdafylke'' (now the Fjordane region; Nordfjord-Sunnfjord), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of Norway
There are 291 peaks in Norway with elevations of over above sea level and that have a topographic prominence of more than 10 meters. The following list includes those 186 that have a topographic prominence of 50 meters or more. The topographic isolation refers to the shortest ''horizontal'' distance one would have to travel to find a higher summit. Location of peaks Most of these peaks are in the municipalities of Lom, Skjåk, Luster, and Vågå, connected to the mountain chain that reaches its prominence with Jotunheimen. There are also several peaks in Dovrefjell, Rondane, Dovre, Lesja, and Folldal that also reach above 2000 meters. All the peaks are to be found in 14 topographical maps ( Norge 1:50000) published by the Norwegian government cartography office, of which 21 peaks are in ''1518 II Galdhøpiggen'', 18 in ''1618 III Glittertinden'', and 13 in ''1617 IV Gjende''. The northernmost is in the Dovre area, meaning there are no 2000 m peaks in northern Norway, even thoug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landmark
A landmark is a recognizable natural or artificial feature used for navigation, a feature that stands out from its near environment and is often visible from long distances. In modern use, the term can also be applied to smaller structures or features, that have become local or national symbols. Etymology In old English the word ''landmearc'' (from ''land'' + ''mearc'' (mark)) was used to describe a boundary marker, an "object set up to mark the boundaries of a kingdom, estate, etc.". Starting from approx. 1560, this understanding of landmark was replaced by a more general one. A landmark became a "conspicuous object in a landscape". A ''landmark'' literally meant a geographic feature used by explorers and others to find their way back or through an area. For example, the Table Mountain near Cape Town, South Africa is used as the landmark to help sailors to navigate around southern tip of Africa during the Age of Exploration. Artificial structures are also sometimes built to a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
