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Djúpadalsá
river, or for short, is a spring creek in the Blönduhlíð district of Skagafjörður, Iceland. It originates in valley, which runs deep into the eastern Tröllaskagi mountain range. It is south of Glóðafeykir and south of the river the valley is named after, Akradalur valley, which belongs to Stóru-Akrar. The valley forks at Tungufjall mountain where the river flows into the from the northeast. The river's source is in the lakes, at around an altitude of 900 meters. The mouth of the river, right next to the Djúpidalur farm in the middle of the valley, flows into a deep gorge and, where the valley ends, the river creates expansive, triangular, sandbars that are stony with thick patches of vegetation. The river has continuously meandered back and forth around the sandbars and divided the channel, however there is now a levee at the riverbed's southernmost sandbars, between the and Minni-Akrar farms. In July 1954, when northern Iceland was beset by heavy rains resul ...
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Djúpidalur
is a farm in the Blönduhlíð district of Skagafjörður, Iceland located in the mouth of Dalsdalur valley, which runs eastward and is located south of Glóðafeykir mountain. The valley branches around Tungufjall mountain (one of three mountains to share that name in the mountains) and the branches run deep into the mountain range. Djúpadalsá, also called , flows through the valley and is in a deep, rather large gorge at the outer end of the valley. The river has formed extensive sandbars in the lowlands that have thick patches of vegetation. The Battle of Haugsnes was fought on these sandbars in 1246. There was a church or chapel in for centuries but it was decommissioned early in the 18th century. Mera-Eiríkur Bjarnason, a farmer in starting in 1733, was famous for his horses. He got into a dispute in Stóru-Akrar with sheriff Skúli Magnússon Skúli Magnússon (12 December 1711 – 9 November 1794) was an Icelandic civil servant. He is often referred to as the ...
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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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Skagafjörður (municipality)
Skagafjörður () is a municipality that covers most of the land area of the region around the fjord with the same name (see Skagafjörður for details on the region) in northern Iceland. Overview The municipality was created in 1998 when 11 out of the 12 municipalities in Skagafjörður held votes on whether they should merge or not. The merge was approved in all the municipalities that held the vote. Akrahreppur was the only municipality in Skagafjörður that did not participate. In February 2022, residents of Akrahreppur and Skagafjörður voted to merge into a single municipality; the merger will be formalized in the spring of 2022. The merge joined the town of Sauðárkrókur, the villages of Hofsós and Varmahlíð and several rural districts. It also includes the historic cathedral site of Hólar which is the site of a growing university today. Localities * Ábær * Hofsós * Hólar * Keta * Miklibær * Reynistaður * Sauðárkrókur * Silfrastaðir * Varmah ...
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Blönduhlíð
Blönduhlíð is a district in Iceland in eastern Skagafjörður that lies along the Héraðsvötn river. It spans the area from the Bóluá river in the south of and the Kyrfisá river to the north. Brekknapláss is the outermost part of in , from the to the Kyrfisá river. There are a few farms there, such as , the birthplace of the priest Jón Steingrímsson—known as the "fire-and-brimstone" preacher—which is in the southernmost part of . , a little further south, is where prime minister Hermann Jónasson was from and where there is a monument in his honor. Hermann was the father of Steingrímur Hermansson, who also served as Iceland's prime minister. Places in Blönduhlíð The following farms are located in : * Akrar (Skagafjörður) * Bóla * Djúpidalur * Flugumýri Flugumýri is a town and church site in the Blönduhlíð district of Skagafjörður, Iceland, at the base of Glóðafeykir mountain. It was, and is, a manorial estate. The town was the hom ...
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Spring Creek
A spring creek is a type of free flowing river whose name derives from its origin: an underground Spring (hydrology), spring or set of springs which produces sufficient water to consistently feed a unique river. The water flowing in a spring creek may additionally be fed by snow pack or rain run-off, as in most traditional free-flowing rivers, but often the entire water source for a spring creek is an aquifer or other underground water source. For this reason, spring creeks are often filled with very pure, clean water and also demonstrate water flows that are smooth, consistent, and unwavering throughout the seasons of the year - unlike rivers filled with run-off or spring and summer melt-off from snow pack, whose water flows, water clarity, and water conditions often vary highly over the course of the year. In addition, water temperatures in spring creeks tend to vary less throughout the seasons of the year than traditional creeks and rivers because they are fed by underground w ...
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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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Tröllaskagi
Tröllaskagi () is a peninsula in northern Iceland on the Greenland Sea, between the fjords of Eyjafjörður and Skagafjörður. The peninsula is mountainous, with several peaks reaching over 1,000 meters above sea level, the tallest being Kerling (1,538 m). It is the part of Iceland with the highest elevation outside the central highlands. The peninsula is cut by several deep valleys that were carved by glaciers during the glacial periods of the last Ice age and later by the rivers that now flow down those valleys. A few permanent glacial ice caps still exist in central Tröllaskagi, but they are all rather small. Human settlement is only extant in the relatively flat lowlands along the coast and in the valleys, but these lowlands are densely populated by Icelandic standards with important agricultural regions and a few towns and villages that mostly base their livelihood on fisheries. Those settlements are (clockwise around the peninsula beginning in Skagafjörður): Hofsós, ...
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Glóðafeykir
is a mountain in eastern Skagafjörður, Iceland in the middle of the Blönduhlíð mountain range, directly opposite Varmahlíð. Its shape is gabled and it is rather striking. The mountain is rocky towards the top, but is still fairly easy to hike. , also often called or , is 910 meters tall. Deep valleys run through the Tröllaskagi mountain range on both sides of : valley to the north and Dalsdalur valley to the south. Two farms are located at the base of the mountain, Flugumýri to the north and Djúpidalur at the mouth of Dalsdalur. Sources say that, in the summer of 1551, , a mistress of Bishop Jón Arason, hid in a tent in the hollow behind from soldiers that the Danish King had sent to Hólar. The Youth Association (), was named after the mountain and operated in Akrahreppur Akrahreppur (, regionally also ), previously called Blönduhlíðarhreppur, is a former municipality, or hreppur, situated in the Northwestern Region of Iceland, and located east of the H ...
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Akrar (Skagafjörður)
Akrar is a cluster of farms at the base of Akrafjall mountain in the Blönduhlíð district of Skagafjörður, Iceland. There are four farms, located in close proximity, collectively named , and . Akrar includes the Akradalur valley, which goes far into the mountains east of . The Lǫgréttumaðr, lögréttumaður Eggert Jónsson had a residence in Akrar, but his son Jón Eggertsson managed the abbey in Hörgárdalur#Möðruvellir in Hörgárdalur, Möðruvellir. There used to be a Cable ferry, ferry landing on the Héraðsvötn at Akrar, and by 1930, it was the last cable ferry. Akratorfa consists of several farms and is located just outside the deserted farms of and , along with the farm . These farms are named after the farm Stóru-Akrar (or "Akrir" as some in also call it). Akrar, Akratorfan, and Stóru-Akrar are all names typically used to describe the same group of farms, depending on who one asks. Stóru-Akrar ("Big Akrar") is the most well-known of the Akratorfa far ...
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Shoal
In oceanography, geomorphology, and Earth science, geoscience, a shoal is a natural submerged ridge, bank (geography), bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water close to the surface or above it, which poses a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared crest and trough, troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''shoal'' is also used in a number of ways that can be either similar to, or quite different from, how it is used in geologic, geomorphic, and oceanographic literature. Sometimes, the term refers to either any relatively shallow place in a stream ...
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Landslide
Landslides, also known as landslips, rockslips or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Landslides are frequently made worse by human development (such as urban sprawl) and resource exploitation (such as mining and deforestation). Land degradation freque ...
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Flash Flood
A flash flood is a rapid flooding of low-lying areas: washes, rivers, dry lakes and depressions. It may be caused by heavy rain associated with a severe thunderstorm, hurricane, or tropical storm, or by meltwater from ice and snow. Flash floods may also occur after the collapse of a natural ice or debris dam, or a human structure such as a man-made dam, as occurred before the Johnstown Flood of 1889. Flash floods are distinguished from regular floods by having a timescale of fewer than six hours between rainfall and the onset of flooding. Flash floods are a significant hazard, causing more fatalities in the U.S. in an average year than lightning, tornadoes, or hurricanes. They can also deposit large quantities of sediments on floodplains and destroy vegetation cover not adapted to frequent flood conditions. Causes Flash floods most often occur in dry areas that have recently received precipitation, but they may be seen anywhere downstream from the source of the prec ...
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