Jostedalsbreen in the context of "Sogndal Municipality"

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⭐ Core Definition: Jostedalsbreen

Jostedal Glacier or Jostedalsbreen (Norwegian) is the largest glacier in continental Europe. It is in Vestland county in Western Norway. Jostedalsbreen is located in the municipalities of Luster, Sogndal, Sunnfjord, and Stryn (all in Vestland county), plus the northeastern tip of the glacier extends into Skjåk Municipality (in Innlandet county). The highest peak in the area is Lodalskåpa at a height of 2,083 metres (6,834 ft).

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Jostedalsbreen in the context of Abrasion (geology)

Abrasion is a process of weathering that occurs when material being transported wears away at a surface over time, commonly occurring with ice and glaciers. The primary process of abrasion is physical weathering. Its the process of friction caused by scuffing, scratching, wearing down, marring, and rubbing away of materials. The intensity of abrasion depends on the hardness, concentration, velocity and mass of the moving particles. Abrasion generally occurs in four ways: glaciation slowly grinds rocks picked up by ice against rock surfaces; solid objects transported in river channels make abrasive surface contact with the bed with ppl in it and walls; objects transported in waves breaking on coastlines; and by wind transporting sand or small stones against surface rocks. Abrasion is the natural scratching of bedrock by a continuous movement of snow or glacier downhill. This is caused by a force, friction, vibration, or internal deformation of the ice, and by sliding over the rocks and sediments at the base (that also causes an avalanche) that causes the glacier to move.

Abrasion, under its strictest definition, is commonly confused with attrition and sometimes hydraulic action however, the latter less commonly so. Both abrasion and attrition refers to the wearing down of an object. Abrasion occurs as a result of two surfaces rubbing against each other, resulting in the wearing down of one or both of the surfaces. However, attrition refers to the breaking off of particles (erosion) which occurs as a result of objects hitting against each other. Abrasion leads to surface-level destruction over a period of time, whereas attrition results in more change at a faster rate. Today, the geomorphology community uses the term "abrasion" in a looser way, often interchangeably with the term "wear".

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Jostedalsbreen in the context of Svartisen

Svartisen is a collective term for two glaciers located in Nordland county in northern Norway. It is part of Saltfjellet-Svartisen National Park, located in the Saltfjell mountain range. The glaciers are located in the municipalities of Beiarn, Meløy, Rana, and Rødøy. Svartisen consists of two separate glaciers that are separated by the 1-kilometre (0.62 mi) long Vesterdalen valley. The two glaciers are:

  • Vestisen or Vestre Svartisen ("western Svartisen") has an area of 221 square kilometres (85 sq mi) which makes it the second largest glacier on the Norwegian mainland after the Jostedalsbreen glacier. (There are larger glaciers on Svalbard.)
  • Østisen or Østre Svartisen ("eastern Svartisen") has an area of 148 square kilometres (57 sq mi) which makes it the country's fourth largest glacier.

There are also a number of minor glaciers in the area surrounding Svartisen, such as Glombreen in the northern part of Meløy Municipality, and Simlebreen in Beiarn Municipality. One of the outlet glaciers of Svartisen, Engabreen ends at the lowest point of any glacier on the European mainland, at 20 metres (66 ft) above sea level (in 2007). The Norwegian Water Resources and Energy Directorate has monitored the glacier mass balance of the glacier since 1970 and operates a sub-glacial laboratory beneath Engabreen.

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