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Revision as of 10:21, 5 March 2023 by Emstrur (talk | contribs)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)The Highland of Iceland is an uninhabited area that covers most of the interior or backland of Iceland. It is often mistakenly called highlands like the Scottis Highlands. The HIGHLAND is situated above 300–400 meters (1000–1300 feet) and are mostly uninhabitable volcanic desert, because the water precipitates as rain or snow infiltrate so quickly into the ground that it is unavailable for plant growth.It is also covered with snow from October until the beginning of June. This results largely in a surface of grey, black or brown earth, lava, and volcanic ashes. A few oasis-like areas, such as Herðubreiðarlindir near Askja, are found only in proximity to rivers.
Most of the numerous glaciers, such as Vatnajökull, Langjökull and Hofsjökull, are also part of the Icelandic Highland. Vegetation is only found on the shores of the glacier rivers. There is also the danger of glacial outburst floods, or "glacier runs" at times of eruptions and volcanic activity.
Some of the most interesting parts of Iceland with volcanic activity are to be found in the Highland, such as Landmannalaugar and the region around Askja and Herðubreið.
Interior routes
The Highland can be crossed only during the Icelandic summer. For the rest of the year the highland roads are closed. The best known highland roads are Kaldidalur, Kjölur and Sprengisandur. Most highland roads require four-wheel drive vehicles, because it is necessary to cross rivers. However, the Kjölur route can easily be traversed in an ordinary car and is therefore one of the more popular highland roads. Off-road driving is forbidden entirely in Iceland where there is no snow, including the Highlands, to protect the environment.
See also
References
- "Mountain Roads" (PDF). Environment Agency of Iceland. 2014. Archived from the original (PDF) on 21 April 2015. Retrieved 26 February 2012.
External links
Media related to Highland of Iceland at Wikimedia Commons
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