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] dominates the central Highland, through which the ] road winds its way]]
] dominates the central Highland, through which the ] road winds its way]]
The '''Highland''' (]: ''Hálendið)'' or The Central Highland<ref>{{Cite journal |last1=Bishop |first1=Michaël Virgil |last2=Ólafsdóttir |first2=Rannveig |last3=Árnason |first3=Þorvarður |date=February 2022 |title=Tourism, Recreation and Wilderness: Public Perceptions of Conservation and Access in the Central Highland of Iceland |journal=Land |language=en |volume=11 |issue=2 |pages=242 |doi=10.3390/land11020242 |issn=2073-445X |doi-access=free }}</ref> is an area that comprises much of the interior land of ]. The Highland is situated above 300–400 meters (1000–1300 feet) and is mostly uninhabitable. The soil is primarily ], and the terrain consists of basalt mountains and ]s. Snow covers the Highland from October until the beginning of June.<ref>{{Cite web |title=Weather and climate in Iceland |url=https://www.visiticeland.com/article/weather-and-climate/ |access-date=2023-09-06 |website=www.visiticeland.com}}</ref> A few ]-like areas such as ] and ] are also found in the Highland. The Highland has many notable natural features and hiking trails.<ref name=":0">{{Cite web |title=Visit Iceland - Official Tourist Info for Iceland |url=https://www.visiticeland.com/geography-of-iceland/ |access-date=2023-09-06 |website=www.visiticeland.com}}</ref>
The '''Highland''' (]: ''Hálendið)'' or The Central Highland<ref>{{Cite journal |last1=Bishop |first1=Michaël Virgil |last2=Ólafsdóttir |first2=Rannveig |last3=Árnason |first3=Þorvarður |date=February 2022 |title=Tourism, Recreation and Wilderness: Public Perceptions of Conservation and Access in the Central Highland of Iceland |journal=Land |language=en |volume=11 |issue=2 |pages=242 |doi=10.3390/land11020242 |issn=2073-445X |doi-access=free }}</ref> is an area that comprises much of the interior land of ]. The Highland is situated above 300–400 meters (1000–1300 feet) and is mostly uninhabitable. The soil is primarily ], and the terrain consists of ] mountains and ]s. Snow covers the Highland from October until the beginning of June.<ref>{{Cite web |title=Weather and climate in Iceland |url=https://www.visiticeland.com/article/weather-and-climate/ |access-date=2023-09-06 |website=www.visiticeland.com}}</ref> A few ]-like areas such as ] and ] are also found in the Highland. The Highland has many notable natural features and hiking trails.<ref name=":0">{{Cite web |title=Visit Iceland - Official Tourist Info for Iceland |url=https://www.visiticeland.com/geography-of-iceland/ |access-date=2023-09-06 |website=www.visiticeland.com}}</ref>
Crossing a river in the Icelandic Highland Icelandic HighlandDesert dominates the central Highland, through which the Kjölur road winds its way
The Highland (Icelandic: Hálendið) or The Central Highland is an area that comprises much of the interior land of Iceland. The Highland is situated above 300–400 meters (1000–1300 feet) and is mostly uninhabitable. The soil is primarily volcanic ash, and the terrain consists of basalt mountains and lava fields. Snow covers the Highland from October until the beginning of June. A few oasis-like areas such as Herðubreiðarlindir and Þórsmörk are also found in the Highland. The Highland has many notable natural features and hiking trails.
Natural features in the Highland
The Highland is made of various geological features, including Landmannalaugar, Torfajökull, Eldgjá, Þórsmörk, Herðubreið, Askja, Hveradalir, Lakagígar, and the Fagrifoss Waterfall. Sites in the Highland are difficult to access and may be accessible only during summer months. Most sites in the Highland require all-wheel drive or all-terrain vehicles for access, due to unpaved dirt roads. Careful planning is recommended when traveling in the Highland.
Landmannalaugar provides some of the most interesting vista points to visit in the Icelandic Highland, for instance this point located at the northwest part of the colorful caldera Torfajökull, showing characteristic rhyolite lava fields and mountains
Glaciers and volcanoes in the Highland
The largest glaciers in the Highland are Vatnajökull, Langjökull, Eyjafjallajökull, Mýrdalsjökull and Hofsjökull with multiple runoff outlet glaciers. Many glaciers occur atop volcanoes, some of which erupt regularly, such as the Bárðabunga volcano. The most famous of these volcanoes in recent times is Eyjafjallajökull, which erupted in 2010. In the sandy Highland, vegetation is found only at the edges of glaciers and near rivers and creeks that flow through the Highland. There is a pervasive danger of glacial outburst floods, or "glacier runs," at times of eruptions and volcanic activity. The radiating heat causes the underside of glaciers to melt, creating large pockets of water that collect until they burst. This phenomenon is specifically unique to Iceland and is internationally known by the Icelandic term jökulhlaup.
The Highland can be crossed only during the Icelandic summer. For the rest of the year, Highland roads are closed. Driving off-road is forbidden, to protect both drivers and environmental features.
The best-known Highland roads are Kaldidalur, Kjölur, Kjalvegur, Fjallabak syðri, Fjallabak nyrðri, Lakavegur, Kverkfjöll, and Sprengisandur. Most Highland roads require four-wheel drive vehicles, which also assist in crossing rivers. However, the Kjölur route can be traversed easily in an ordinary car and is therefore one of the more popular Highland roads.
Media related to Highland of Iceland at Wikimedia Commons
