Herðubreið (, ''broad-shouldered'') is a

tuya A tuya is a flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. They are rare worldwide, being confined to regions which were covered by glaciers and had active volcanism during the same period. As lava ...

in northern part of Vatnajökull National Park,

Iceland Iceland ( is, Ísland; ) is a Nordic island country in the North Atlantic Ocean and in the Arctic Ocean. Iceland is the most sparsely populated country in Europe. Iceland's capital and largest city is Reykjavík, which (along with its ...

. It is situated in the

Highlands of Iceland The Highlands of Iceland ( is, hálendið ) are a sparsely inhabited plateau that covers most of the interior of Iceland. They are situated above 400–500 metres (1300–1600 feet) and are mostly an uninhabitable volcanic desert, because the wa ...

at the east side of the Ódáðahraun

desert A desert is a barren area of landscape where little precipitation occurs and, consequently, living conditions are hostile for plant and animal life. The lack of vegetation exposes the unprotected surface of the ground to denudation. About on ...

and close to Askja volcano. The desert is a large

lava Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or ...

field originating from

eruption Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ...

s of Trölladyngja and other

shield volcano A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the more vi ...

es in the area. Herðubreið was formed beneath the icesheet that covered

during the last

glacial period A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate betwe ...

Overview

Due to the mountain's steep and unstable sides, the first ascent was in 1908 despite centuries of knowledge of its existence. The Mountain is often referred to as "The Queen of Icelandic Mountains" by Icelanders due to its beautiful shape. Near the mountain lies an

oasis In ecology, an oasis (; ) is a fertile area of a desert or semi-desert environment'ksar''with its surrounding feeding source, the palm grove, within a relational and circulatory nomadic system.” The location of oases has been of critical imp ...

called Herðubreiðarlindir with a campground and hiking trails. In former times, outcasts who had been excluded from Icelandic society because of crimes they had committed lived at the oasis. One such outlaw was Fjalla-Eyvindur, who lived there during the winter of 1774–1775. In 2019 Herðubreið became a part of Vatnajökull National Park.

References

External links

Official Website of Vatnajökull National Park
* ;Images:

* http://isafold.de/panorama/panoram.htm (via "Askja") {{DEFAULTSORT:Herdubreid Mountains of Iceland Tuyas of Iceland Pleistocene volcanoes North Volcanic Zone of Iceland One-thousanders of Iceland

Overview

See also

References

External links