Reykjahlíð
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Reykjahlíð () is a village situated on the shores of Lake
Mývatn () is a shallow lake situated in an area of active volcanism in the north of Iceland, not far from Krafla volcano. It has a high amount of biological activity. The lake and the surrounding wetlands provides a habitat for a number of waterbirds, e ...
in the north of
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 s ...
. It is the seat of the municipality of
Skútustaðahreppur Skútustaðahreppur (, regionally also ) is a former rural municipality located in East Iceland, in Northeastern Region. Its seat is in the village of Reykjahlíð. In 2022 the municipality merged with Þingeyjarsveit under the name of the latte ...
. It has 227 inhabitants as of 2021.


Overview

During the so-called Mývatn fires, caused by the eruption of the nearby
volcano A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ...
Krafla Krafla () is a volcanic caldera of about 10 km in diameter with a 90 km long fissure zone. It is located in the north of Iceland in the Mývatn region and is situated on the Iceland hotspot atop the Mid-Atlantic Ridge, which forms the ...
in 1729, the village was destroyed by a
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 un ...
stream. However, the inhabitants were saved when the lava flow stopped in front of the village church on higher ground, allegedly as the result of the prayers of the village priest. The church is still there, although the present building dates from 1972.


Main sights

From Reykjahlíð, it is possible to go to many sights in the area, most notably Krafla. The volcano last erupted in 1984, but the vapour of a warm lava field and of
sulphur Sulfur (or sulphur in British English) is a chemical element with the symbol S and atomic number 16. It is abundant, multivalent and nonmetallic. Under normal conditions, sulfur atoms form cyclic octatomic molecules with a chemical formula ...
springs can still be seen. Not far from there is the crater Víti (meaning "hell" in Icelandic), but looking today rather harmless with a blue lake at its bottom. Its apparent tranquility belies the fact that its last eruption was as recent as 1976. Other interesting places are on the lake itself, like the volcano Hverfjall, the pseudo-craters of Skútusstaðir and
Dimmuborgir Dimmuborgir (''dimmu'' "dark", ''borgir'' "cities" or "forts", "castles"; pronounced ) is a large area of unusually shaped lava fields east of Mývatn in Iceland. The Dimmuborgir area is composed of various volcanic caves and rock formations, rem ...
(a strange lava formation). A local airport provides sightseeing during the summer. A plant for extraction and processing of
diatomite Diatomaceous earth (), diatomite (), or kieselgur/kieselguhr is a naturally occurring, soft, siliceous sedimentary rock that can be crumbled into a fine white to off-white powder. It has a particle size ranging from more than 3  μm to le ...
was a main point in local economy until 2004 when it was shut down.
Mývatn () is a shallow lake situated in an area of active volcanism in the north of Iceland, not far from Krafla volcano. It has a high amount of biological activity. The lake and the surrounding wetlands provides a habitat for a number of waterbirds, e ...
Nature Baths opened on 30 June 2004.


Climate

Reykjahlíð features a
tundra climate The tundra climate is a polar climate sub-type located in high latitudes and high mountains. undra climate https://www.britannica.com/science/tundra-climateThe Editors of Encyclopaedia Britannica, 2019 It is classified as ET according to Köppen ...
(
Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notabl ...
: ET), bordering on a
subarctic climate The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, ge ...
(
Köppen climate classification The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notabl ...
: Dfc). Summers are typically cool with crisp nights while winters are very long and cold, but not severely cold.


Photogallery

Reykjahlíð.2.jpg, Panoramic view Viti.jpg, Víti crater Reykjahlid.jpg, Diatomite plant Myvatn Nature Baths by Bruce McAdam.jpg, Nature Baths


See also

*
Mývatn () is a shallow lake situated in an area of active volcanism in the north of Iceland, not far from Krafla volcano. It has a high amount of biological activity. The lake and the surrounding wetlands provides a habitat for a number of waterbirds, e ...
*
Volcanism of Iceland :''The volcano system in Iceland that started activity on August 17, 2014, and ended on February 27, 2015, is Bárðarbunga.'' :''The volcano in Iceland that erupted in May 2011 is Grímsvötn.'' Iceland experiences frequent volcanic activity, d ...


Notes and references


External links


Skútustaðahreppur municipal websiteMyvatn Nature Baths
{{DEFAULTSORT:Reykjahlid Populated places in Northeastern Region (Iceland)