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Eyvindarstaðaheiði
Eyvindarstaðaheiði is an expansive plateau and rangeland located between the Blanda river in Austur-Húnavatnssýsla and Vestari-Jökulsá in Skagafjörður, Iceland. It is close to the Hofsjökull glacier at a lower elevation than the common grazing pastures in Skagafjörður and Húnavatnssýsla. Geography Eyvindarstaðaheiði is the easternmost of the plains that encompass the plateau from the north of Langjökull glacier and Kjölur. Auðkúluheiði plateau is west of Eyvindarstaðaheiði and east of that is Hofsafrétt. The plateau used to belong to Eyvindarstaðir in Blöndudalur valley, from which it derives its name. The area's grazing land is held collectively between Húnavatnssýsla and Skagafjörður counties, which border it. The landscape on the western side of the plateau is shaped by the glaciers and is widely covered with thick moraine and sedimentary layers. The land there is flat, level, and covered in a decent amount of vegetation. Most of the area is ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svartá
The Svartá river ("Black River") is a spring creek on the inner, western side of Skagafjörður, Iceland. A considerable amount of spring water runs in the river up to the highland where it then begins to resemble a direct run-off river as it flows on. The river surfaces in the Eyvindarstaðaheiði plateau and runs through Svartárdalur valley, then continues between Neðribyggð and Reykjatunga where there is a waterfall called Reykjafoss. Some ways below it, around Vindheimamelar, the river’s name changes to Húseyjarkvísl. It flows into the bottom of Varmahlíð and into the Héraðsvötn shortly before reaching Glaumbær Glaumbær is an Icelandic town and church site in the middle of Langholt, west of Héraðsvötn in Skagafjörður, formerly a part of the rural municipality Seyluhreppur. It is now home to the Skagafjörður Folk Museum. History The Glaumbær .... In old literature, the Jökulsá river, or part of the Héraðsvötn, is said to have flowed west ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or an ''affluent'', is a stream or river that flows into a larger stream (''main stem'' or ''"parent"''), river, or a lake. A tributary does not flow directly into a sea or ocean. Tributaries, and the main stem river into which they flow, drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean, another river, or into an endorheic basin. The Irtysh is a chief tributary of the Ob (river), Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vesturdalur
Vesturdalur ("west valley") is a valley that runs from the head of Skagafjörður, Iceland and cuts far into the central Highlands of Iceland, highlands. Austurdalur valley runs parallel to it. The valleys are surrounded by tall, steep mountains. Geography The lowest town in western Vesturdalur is the church site Goðdalir. Just inside the valley, the Vestari-Jökulsá river flows out of Hofsdalur valley, which is very long and goes south into the highlands. The valley is narrow and uninhabited. The river that runs along Vesturdalur and flows into Vestari-Jökulsá is, however, named Hofsá (Vesturdalur), Hofsá and is mostly a spring creek. This river is named for Hof (Hof í Vesturdal), settled by Eiríkur Hróaldsson, who owned all the land south up to Hofsjökull, Hofsjökull glacier. The valley's eastern side has a few farms, including , and . The abandoned farm is farther into the valley and was for many years the valley's innermost farm, however there were even more fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Svartárdalur
Svartárdalur is a valley deeper into the interior of Skagafjörður, Iceland. It was previously a part of Lýtingsstaðahreppur Lýtingsstaðahreppur was a hreppur, an old Icelandic municipality, in the interior of Skagafjörður County, Iceland, located to the west of the Héraðsvötn. It was named after the Lýtingsstaðir farm in Tungusveit. The spanned from the K ..., but now belongs to Skagafjörður County. It is a rather short valley and the Svartá river runs through it. There are few farms there, and some have been abandoned. The homestead Írafell is in the valley. There is another Svartárdalur and another Svartá on the Húnavatnssýsla side of the mountain and they are occasionally confused because they are so close to each other. References {{Authority control Skagafjörður Valleys of Iceland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a solid material that is transported to a new location where it is deposited. It occurs naturally and, through the processes of weathering and erosion, is broken down and subsequently sediment transport, transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension (chemistry), suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial, fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and stream channel, river channel deposits are examples of fluvial transport and deposition (geology), deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and Rock (geology), rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French language, French , which in turn is derived from the Savoyard dialect, Savoyard Italian ('mound of e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Route F35 (Iceland)
Kjalvegur (, ) is a highland road in Iceland, crossing Kjölur from north to south. History Formerly, the name referred to a horse-track closer to Langjökull, west of the current road. This track now goes by the name ''Kjalvegur hinn forni'' (Ancient Kjalvegur), and is closed to motorized traffic. Geography The road begins in the south of Iceland near Haukadalur and behind the Gullfoss waterfall, ending in the north near ''Blönduós''. The road traverses the interior between two glaciers, Langjökull and Hofsjökull. It is the second longest of the roads through the Highlands of Iceland. It takes about 5 hours to traverse by car, the road is generally rough, but river crossings are bridged. See also * Route 35 (Iceland) * Sprengisandsleið * Kjölur Kjölur () is a plateau in the highlands of Iceland, roughly defined as the area between the Langjökull and Hofsjökull glaciers. It lies at an elevation of about 600–700 metres. Geography At the northern end of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austur-Húnavatnssýsla
Iceland was historically divided into 23 counties known as ''sýslur'' (), and 23 independent towns known as ''kaupstaðir'' (). Iceland is now split up between 24 sýslumenn (magistrates) that are the highest authority over the local police (except in Reykjavík where there is a special office of police commissioner) and carry out administrative functions such as declaring bankruptcy and marrying people outside of the church. The jurisdictions of these magistrates often follow the lines of the historical counties, but not always. When speaking of these new "administrative" counties, the custom is to associate them with the county seats rather than using the names of the traditional counties, even when they cover the same area. Composition Independent towns (''kaupstaðir'') were first created in the 18th century as urbanisation began in Iceland; this practice continued into the 1980s. The last town that was declared an independent town was Ólafsvík in 1983. Since then, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Langjökull
Langjökull (, Icelandic for "long glacier") is the second largest ice cap in Iceland (), after Vatnajökull. It is situated in the west of the Icelandic interior or Highlands of Iceland and can be seen clearly from Haukadalur. It covers the higher parts of the Langjökull volcanic system. Its volume is and the ice is up to thick. The highest point of the ice cap (at ''Baldjökull'' at the northern end of Langjökull) is about above sea level. In the past, the largest recorded surface area was in 1840. Situation and form The glacier is roughly parallel to the direction of the country's active volcanic zone: north-east to south-west. It is about long and wide, and has a slightly narrower point roughly between the lake Hvítárvatn on the Kjölur mountain road to the east and the Þrístapajökull glacier to the west, near another smaller glacier, Eiríksjökull, which is not quite connected to Langjökull. It is the nearest large glacier to Reykjavík. The area o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
