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Trongisvágsfjørður
Trongisvágsfjørður is a fjord on the island of Suðuroy in the Faroe Islands. There are four villages around the fjord. Furthest east on the northern side of the fjord is Froðba, in the bottom of the fjord is Trongisvágur. In between Trongisvágur and Froðba is Tvøroyri, the largest of these villages. South of Trongisvágur in a bay is Øravík, a part of Øravík is called Øravíkarlíð, it is located close to Trongisvágur and not visible from Øravík. These villages are in the Municipality of Tvøroyri. The ferry port on Krambatangi The ferry port of Krambatangi is on the southern side of the fjord between Trongisvágur and Øravík. The ferry port was on Drelnes before 2005 when the new ferry MS Smyril, Smyril arrived, which necessitated building a new ferry port. Drelnes is just a few hundred metres further east than Krambatangi. The Salt Silo on Drelnes There is an old Salt Silo on Drelnes which is a ruin, but there is a plan called Project Salt which intend ...
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Suðuroy
Suðuroy (pronounced: �suːwʊrɔior �suːri ‘South Island’, ) is the southernmost of the Faroe Islands. The island covers 163.7 square kilometres (63.2 sq mi). In 2018 the population was 4,601. Suðuroy region ( sýsla) comprises this island and Lítla Dímun, the next isle northward in the Faroes, which is uninhabited. History One ancient settlement, Víkarbyrgi was abandoned late in the 1990s. Another settlement, Akraberg was abandoned around 1350 because of the Black Death; the people who lived there at that time came from Friesland, and legend has it that people in Hørg (in Sumba) can trace their ancestry back to this settlement, which was situated on the southernmost point of the island. In the 17th century, Suðuroy was subjected to repeated attacks by North African pirates, who in the Faroe Islands were referred to as Turks when North Africa belonged to the Ottoman Empire. One well known such incident was the Slave raid of Suðuroy. They abducte ...
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Trongisvágur
Trongisvágur () is a village on the island of Suduroy in the Faroe Islands. Trongisvágur is the village in the bottom of Trongisvágsfjørður ( fjord) on the east coast of Suduroy. Trongisvágur and the neighbouring villages of Tvøroyri and Øravík have grown into one entity (the northern part of Øravík, which is called Øravíkarlíð, is where the ferry port Krambatangi is). A river called Stórá that runs through the valley passes through a plantation that is worth visiting on a good day, and then flows into the inlet at a nearby beach. There is a debate whether the name Trong is Norse or Gaelic in origin. Another version of the name is Trungisvágur. Trungisvágsbotnur is on the west coast, west of Trongisvágur. There are binoculars there in summertime, so people can have a closer look at birds and the vertical cliffs there. The place is called Á Røðini, but some people call it Kikarin, because of the binoculars. Shortly after the Park of Trongisvágur is the t ...
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Froðba
Froðba () is a village located farthest out on the north brink of Trongisvágsfjørður, an inlet on the east coast of the island of Suðuroy in the Faroe Islands. History The village has eventually merged with the harbour-city of Tvøroyri. Froðba is usually divided into smaller places such as Hamri, Undir Skorum, Støðlunum, Torvheyggur and Bøur. Bøur is usually referred to as "Úti á Bø" the oldest inhabited area in Froðba, Bøur has a small graveyard which used to be the only one in Trongisvágsfjørður. It is no longer in use and Froðba used to have a church which was in Bø but after Froðba merged with the growing nearby town of Tvøroyri, the small church was moved to Tvøroyri, and later as the population grew the church was replaced and moved to Sandvík. Tradition says that Froðba is the oldest village on Suðuroy and in the Faroe Islands. A legendary Danish king, Frode or Fróði, ran ashore and settled here. The place is named after him. The name Froðba wa ...
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Tvøroyri
Tvøroyri is a village on the north side of the Trongisvágsfjørður on the east coast of Suðuroy island in the Faroe Islands. Together with Froðba, Trongisvágur, Líðin and Øravík it forms Tvøroyri Municipality. The village is considered to have been founded in 1836, when the Danish Royal Trade Monopoly in the Faroe Islands, Royal Danish Monopoly Trade Store was founded on a small tongue of land, called Tvøroyri. In a short span of years, Tvøroyri grew into a large village, mainly after 1856 when the monopoly state of the store was abolished. Around the turn of the 20th century, Tvøroyri was one of the largest towns on the Faroe Islands and had one of the main fishing industries. Overview Church of Tvoroyri, The church in Tvøroyri was constructed in Norway as a building set, moved to Tvøroyri and then built here in 1907, ready to use in 1908. The old church was moved to Sandvík. Trongisvágur Trongisvágur is the village furthest to the west of the inlet of Trong ...
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Krambatangi
Krambatangi is the ferry port of Suðuroy in the Faroe Islands. The ferry MS Smyril, MS ''Smyril'' M/F disembarks 2–3 times daily from Krambatangi to Tórshavn. Krambatangi is located on the southern side of Trongisvágsfjørður halfway between Trongisvágur and Øravík, opposite Tvøroyri. The ferry port was earlier on Drelnes, which is a few hundred metres further east of Krambatangi. But in 2005 a new ferry arrived, which was much bigger than the prior one, and therefore required a new ferryport at Krambatangi. Krambatangi does not belong to the municipality of Tvøroyri, and there have been some disagreements between the Tvøroyri municipality and Strandfaraskip Landsins (SSL) because they didn't pay harbour dues for entering the port of Tvøroyri. The Faroese court decided that SSL ought to pay for entering the port of Tvøroyri,
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Øravík
Øravík (also spelled Ørðavík, ) is a village on the east coast of the island of Suðuroy in the Faroe Islands. The village is located in the center of the island on a crossroad where the road to Fámjin goes towards west over the mountains to the west coast. One part of the village is located in the bay of Øravík, the other part is 3 km further north near the ferry port Krambatangi. The northern part of Øravík and the southern part of Trongisvágur have grown together. Øravík is one of the few places in Suðuroy which still has cattle. Besides from that there are other domestic animals like sheep and geese. There is a small harbour in Øravík and some boat houses. Varðagøtur Just south of Øravík up in the mountains is a place called Mannaskarð, where the old walking paths from five villages meet, these paths are called varðagøtur in Faroese, named after "varðar", which means cairn. These are all around the island between the villages and other places, so ...
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MS Smyril
The ''Smyril'' is a passenger and car ferry owned and operated by the Faroese transport company Strandfaraskip Landsins. She is the largest ferry in the fleet and the fifth vessel to carry the name Smyril, which is the Faroese word for merlin. The ferry takes 200 cars and 975 passengers. The ferry services Suðuroy with 2-3 daily trips from Tórshavn to Krambatangi. The trip takes 2 hours and 5 minutes. Strandfaraskip Landsins meets all arrivals and departures with buses to Vágur, Tvøroyri and Hvalba, while dial-a-ride services link the ferry to/from other villages, including Fámjin. History The current ''Smyril'' was built at the IZAR shipyard in San Fernando, Spain. She entered service on the 15 October 2005. Previous vessels Since the 1890s the Strandfaraskip Landsins have operated five different ships named ''Smyril''. ''Smyril'' (I) Smyril I was built in the 1890s and began as a smaller transport boat in Tvøroyri in the Faroe islands. ''Smyril'' (II) Smyril II wa ...
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Fjord
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ...
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Faroe Islands
The Faroe Islands ( ) (alt. the Faroes) are an archipelago in the North Atlantic Ocean and an autonomous territory of the Danish Realm, Kingdom of Denmark. Located between Iceland, Norway, and the United Kingdom, the islands have a population of 54,609 and a land area of 1,393 km². The official language is Faroese language, Faroese, which is partially mutually intelligible with Icelandic language, Icelandic. The terrain is rugged, dominated by fjords and cliffs with sparse vegetation and few trees. As a result of its proximity to the Arctic Circle, the islands experience perpetual Twilight, civil twilight during summer nights and very short winter days; nevertheless, they experience a Oceanic climate#Subpolar variety (Cfc, Cwc), subpolar oceanic climate and mild temperatures year-round due to the Gulf Stream. The capital, Tórshavn, receives the fewest recorded hours of sunshine of any city in the world at only 840 per year. Færeyinga saga, Færeyinga Saga and the writin ...
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Fjords Of The Faroe Islands
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or glacia ...
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