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Þórðarhöfði
in Höfðaströnd is a 202-meter-tall rocky headland that runs toward the eastern side of Skagafjörður directly north of Hofsós. At first glance, the headland seems like an island but it is connected to the mainland. Two low Isthmus, isthmuses, and , connect it to the land and there a is a large, 10-kilometer squared Lagoon, coastal lagoon between them called Höfðavatn, where there is excellent fishing for arctic char. In the early 20th century, the poet Jóhann Sigurjónsson proposed that an ocean liner harbor be built, but it did not happen. is the ruins of an old volcanic eruption. Trap rock, Basalt rock formations are located in the stone, and these are best seen from the sea. References

{{Authority control Headlands of Iceland Skagafjörður ...
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Höfðaströnd
is a region on the coast around Hofsós on the eastern side of Skagafjörður, Iceland. Its southernmost farm is Gröf, and the closest to the sea is Höfði. The region is named after Þórðarhöfði, which is a predominant feature of the landscape. Within is Höfðavatn, 's biggest lake, which is actually a coastal lagoon. History There has long been a considerable amount of fishing based out of , both from and from in Bær in , where there were workman's cottages. People there lived on fishing and fowling in Drangey, in addition to certain lichens. The area's general store was in in since 1600, when Kolkuós's port facilities deteriorated dramatically, and up until the end of the 19th century, when Sauðárkrókur became 's principal commercial area. There were also shops in Grafarós from around 1840 until 1915. was previously a part of Hofshreppur but has belonged to Skagafjörður County since the area's hreppurs unified. There are two church sites in , H ...
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Hofsós
Hofsós () is one of the oldest trading ports in northern Iceland dating back to the 16th century. The tiny village Hofsós in the Northern Region in Iceland was a rather busy trading post in the 17th and 18th century, but despite the merchant activities this small village did not develop into a larger village or a town in the 20th century. Hofsós had all the historical prerequisites to become a large town. It was a trading post for the Danish Trade Monopoly, it was not far away from the fishing grounds, it was central in the region, and it had a relatively good landing spot for boats. The Drangey Exhibition is in Pakkhús, the Hofsós warehouse built in 1777, during the time of the trading monopoly. Massacre hill farm (''Mannskaðaholl'') at the south end of Lake Höfðavatn, is named for the massacre of English marauders, which took place there in 1431. Other services offered are accommodation in guesthouses, a restaurant, coffee-house, and a camping site. There are also pleas ...
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Höfðavatn
Höfðavatn () is a lagoon-like lake in northern Iceland. It is located in the municipality of Skagafjörður. Geography Höfðavatn lies at the fjord of Skagafjörður about 7 km north of the village of Hofsós. The surface of the Höfðavatn is about 10 km2; the maximum depth is 6.4 m, the middle depth 3.9 M. North of the lake lies the Málmeyjarsund , west of Þórðarhöfði in Höfðaströnd is a 202-meter-tall rocky headland that runs toward the eastern side of Skagafjörður directly north of Hofsós. At first glance, the headland seems like an island but it is connected to the mainland. Two low Isthmus, isthmuse ... . References Lakes of Iceland Skagafjörður {{Iceland-geo-stub ...
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Skagafjörður
Skagafjörður () is a deep fjord and its valley in northern Iceland. Location Skagafjörður, the fjord, is about 40 km long and 15 km wide, situated between Tröllaskagi to the east and the Skagi, Skagi Peninsula to the west. There are two municipalities in the area, Skagafjörður Municipality (approx. 4140 inhabitants) and Akrahreppur, Akrahreppur Municipality (approx. 210 inhabitants). This is one of Iceland's most prosperous agricultural regions, with widespread dairy and sheep farming in addition to the horse breeding for which the district is famed. Skagafjörður is the only county in Iceland where horses outnumber people. It is a centre for agriculture, and some fisheries are also based in the settlements of Sauðárkrókur and Hofsós. The people living in Skagafjörður have a reputation for choir singing, horsemanship, and gatherings. There are three islands in the bay: Málmey, Drangey and Lundey, Skagafjörður, Lundey (Puffin Island). The bay is l ...
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Iceland
Iceland is a Nordic countries, Nordic island country between the Atlantic Ocean, North Atlantic and Arctic Oceans, on the Mid-Atlantic Ridge between North America and Europe. It is culturally and politically linked with Europe and is the region's westernmost and most list of countries and dependencies by population density, sparsely populated country. Its Capital city, capital and largest city is Reykjavík, which is home to about 36% of the country's roughly 380,000 residents (excluding nearby towns/suburbs, which are separate municipalities). The official language of the country is Icelandic language, Icelandic. Iceland is on a rift between Plate tectonics, tectonic plates, and its geologic activity includes geysers and frequent Types of volcanic eruptions, volcanic eruptions. The interior consists of a volcanic plateau with sand and lava fields, mountains and glaciers, and many Glacial stream, glacial rivers flow to the sea through the Upland and lowland, lowlands. Iceland i ...
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Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosio ...
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Isthmus
An isthmus (; : isthmuses or isthmi) is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. A tombolo is an isthmus that consists of a spit or bar, and a strait is the sea counterpart of an isthmus, a narrow stretch of sea between two landmasses that connects two larger bodies of water. Isthmus vs land bridge vs peninsula ''Isthmus'' and ''land bridge'' are related terms, with isthmus having a broader meaning. A land bridge is an isthmus connecting Earth's major land masses. The term ''land bridge'' is usually used in biogeology to describe land connections that used to exist between continents at various times and were important for the migration of people and various species of animals and plants, e.g. Beringia and Doggerland. An isthmus is a land connection between two bigger landmasses, while a peninsula is rather a land protrusion that is connected to a bigger landmass on one side only and surrounded by ...
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Lagoon
A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') and ''atoll lagoons''. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as Estuary, estuaries. Lagoons are common coastal features around many parts of the world. Definition and terminology Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, reef, coral reef, or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis J ...
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Arctic Char
The Arctic char or Arctic charr (''Salvelinus alpinus'') is a cold-water fish in the family Salmonidae, native to alpine lakes, as well as Arctic and subarctic coastal waters in the Holarctic realm, Holarctic. Distribution and habitat It Spawn (biology), spawns in freshwater and its populations can be lacustrine, riverine, or anadromous, where they return from the ocean to their fresh water birth rivers to spawn. No other freshwater fish is found as far north; it is, for instance, the only fish species in Lake Hazen, which extends up to on Ellesmere Island in the Northern Canada, Canadian Arctic. It is one of the rarest fish species in Great Britain and Ireland, found mainly in deep, cold, glacial lakes, and is at risk there from acidification. In other parts of its range, such as the Nordic countries, it is much more common, and is fishery, fished extensively. In Siberia, it is known as ''golets'' () and it has been introduced in lakes where it sometimes threatens less hardy ...
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Jóhann Sigurjónsson
Jóhann Sigurjónsson (June 19, 1880 – August 31, 1919) was an Icelandic playwright and poet. Atypically, Jóhann wrote plays and poetry in both his native Icelandic and in Danish. Biography Jóhann was the son of an Icelandic farmer and was born in Laxamýri, Iceland. In 1899 he emigrated to Denmark to study at The Royal Danish Veterinary and Agricultural University, but abandoned his studies in 1902 to devote himself to literature. During this period, he came under the influence of the Danish writer Georg Brandes and the philosophy of Friedrich Nietzsche. He is probably best known for his play ''Fjalla-Eyvindur'' (Danish: ''Bjærg-Ejvind og hans hustru'', English: ''Eyvindur of the Mountains''), which was first published in 1911. The play was a success in Germany and Scandinavia and was also produced in the United States. It was cinematised by Victor Sjöström in 1918 as '' The Outlaw and His Wife''. The play is based on an Icelandic folk tale about a notorious outlaw. ...
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Volcanic Eruption
A volcanic eruption occurs when material is expelled from a volcanic vent or fissure. Several types of volcanic eruptions have been distinguished by volcanologists. These are often named after famous volcanoes where that type of behavior has been observed. Some volcanoes may exhibit only one characteristic type of eruption during a period of activity, while others may display an entire sequence of types all in one eruptive series. There are three main types of volcanic eruptions. Magmatic eruptions involve the decompression of gas within magma that propels it forward. Phreatic eruptions are driven by the superheating of steam due to the close proximity of magma. This type exhibits no magmatic release, instead causing the granulation of existing rock. Phreatomagmatic eruptions are driven by the direct interaction of magma and water, as opposed to phreatic eruptions, where no fresh magma reaches the surface. Within these broad eruptive types are several subtypes. The we ...
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Trap Rock
Trap rock, also known as either trapp or trap, is any dark-colored, fine-grained, non-granitic intrusive or extrusive igneous rock. Types of trap rock include basalt, peridotite, diabase, and gabbro.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.) American Geological Institute, Alexandria, Virginia. 779 pp. Trap is also used to refer to flood (plateau) basalts, such as the Deccan Traps and Siberian Traps.Le Maitre, R. W., ed. (2002) ''Igneous Rocks: A Classification and Glossary of Terminology''. Cambridge University Press, New York. 236 pp. The erosion of trap rock created by the stacking of successive lava flows often creates a distinct stairstep landscape from which the term ''trap'' was derived from the Swedish word , which means "stairs". The slow cooling of magma either as a sill or as a thick lava flow sometimes creates systematic vertical fractures within the resulting layer of trap rock. These fractures of ...
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