Oddnýjarhnjúkur-Langjökull Volcanic System
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The Oddnýjarhnjúkur-Langjökull (Langjökull) volcanic system of Iceland last erupted about 3600 years ago and is associated with current geothermal activity. The area of its
central volcano A central volcano is a type of volcano formed by basalts and silica-rich volcanic rocks. They contain very few or no volcanic rocks of intermediate composition, such that they are chemically bimodal volcanism, bimodal. Large silicic eruptions at c ...
is at present under the second largest ice cap in Iceland.


Geography

The volcanic system is located north of Lake Thingvallavatn and its southern lava flows contribute to the floor of the
Þingvellir Þingvellir (, anglicised as ThingvellirThe spelling ''Pingvellir'' is sometimes seen, although the letter "p" is unrelated to the letter thorn (letter), "þ" (thorn), which is pronounced as "th".) was the site of the Althing, Alþing, the annual ...
rift valley A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear ...
central to Icelandic cultural history and the
fissure system A fissure is a long, narrow crack opening along the surface of Earth. The term is derived from the Latin word , which means 'cleft' or 'crack'. Fissures emerge in Earth's crust, on ice sheets and glaciers, and on volcanoes. Ground fissure A ...
which is up to wide extends up to north. The Laugarfjall lava dome on the western side of the Haukadalur valley that houses the
Geysir Geysir (), sometimes known as The Great Geysir, is a geyser in south-western Iceland, that geological studies suggest started forming about 1150 CE. The English word ''geyser'' (a periodically spouting hot spring) derives from Geysir. The name ' ...
geothermal area with its
geyser A geyser (, ) is a spring with an intermittent water discharge ejected turbulently and accompanied by steam. The formation of geysers is fairly rare and is caused by particular hydrogeological conditions that exist only in a few places on Ea ...
s and other geothermal features is part of the southern fissure swarm. The
shield volcano A shield volcano is a type of volcano named for its low profile, resembling a 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 viscous lava ...
of
Skjaldbreiður Skjaldbreiður (, "broad shield") is an Icelandic lava shield formed in a huge and quite protracted eruption series from about roughly 9,500 years ago. The extensive lava fields which were produced by this eruption, flowed southwards, and f ...
is prominent to the north of the rift valley with a height of and to the north the
Langjökull Langjökull (, Icelandic for "long glacier") is the second largest ice cap in Iceland (), after Vatnajökull. It is situated in the west of the Icelandic interior or Highlands of Iceland and can be seen clearly from Haukadalur. It covers the ...
ice cap at in area and second in area in Iceland, covers its central volcano of Oddnýjarhnjúkur. The highest point within the Langjökull icecap is to its north east where the Baldjökull part of the ice cap covers 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 ...
of the same name with a height of . The geothermal area of
Hveravellir Hveravellir () is a geothermal field (high temperature field) of the Oddnýjarhnjúkur-Langjökull volcanic system - in the north of the Langjökull glacier. Description Hveravellir geothermal area is a small nature reserve and a tourist centre ...
with
hot spring A hot spring, hydrothermal spring, or geothermal spring is a Spring (hydrology), spring produced by the emergence of Geothermal activity, geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow ...
s,
fumarole A fumarole (or fumerole) is a vent in the surface of the Earth or another rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcani ...
s and
mud pool A mudpot, or mud pool, is a type of acidic hot spring, or fumarole, with limited water. It usually takes the form of a pool of bubbling mud, as a result of the acid and microorganisms decomposing surrounding rock into clay and mud. Description ...
s is to the north east of the central volcano in the northern part of the fissure swarm which is dominated by Kjalhraun at . To the west is the
Prestahnúkur The peak Prestahnúkur () with a height of , is in the Western Volcanic Zone to the west of the Highlands of Iceland to the west of Langjökull glacier, or to be more specific, to the west of Geitlandsjökull glacier, a part of the Langjökull ...
volcanic system with the small ice cap of
Eiríksjökull Eiríksjökull ( Icelandic for "Eirík's glacier", ) is a glacier north-west of Langjökull in Iceland, with an area of reaching a height of , atop the largest table mountain in Iceland which goes by the same name. Geology This volcano which ...
in area, and to the east of Langjökull is the
Hofsjökull volcanic system __NOTOC__ The Hofsjökull volcanic system (also Hofsjökull-Kerlingarfjöll volcanic system) contains the largest active central volcano in Iceland. It is called Hofsjökull ( Icelandic: "temple glacier", ), after the icecap of the same name. ...
with the large
Hofsjökull __NOTOC__ Hofsjökull (Icelandic language, Icelandic: "temple glacier", ) is the third largest ice cap in Iceland after Vatnajökull and Langjökull and covers the largest active central volcano in the country, which has the same name. It is si ...
ice cap and to its south the
Kerlingarfjöll Kerlingarfjöll () is a tall volcanic massive in Iceland situated in the Highlands of Iceland near the Kjölur highland road. It is usually regarded as part of a large tuya fissure system of in the southern portion of the Hofsjökull volcanic ...
volcanic massif. A large tuya and
composite volcano A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a ...
Hrútfell with a height of is located between Baldjökull and Kerlingarfjöll at the southern end of the
Kjölur Kjölur () is a plateau in the highlands of Iceland, roughly defined as the area between the Langjökull and Hofsjökull glaciers. It lies at an elevation of about 600–700 metres. Geography At the northern end of the Kjölur road, near the h ...
plateau between the two volcanic systems which is reached by the Kjalvegur road (F35).


Activity

Currently apart from the geothermal activity already mentioned at Geysir and Hveravellir there have been earthquake swarms to the south-east of the Langjokull glacier and north of Hveravellir. While some of the fairly recently erupted Hallmundarhraun lava flow came from vents immediately adjacent to the north-west boundary of the system these eruptions are now assigned to the Prestahnúkur volcanic system.


Geology

The Oddnýjarhnjúkur-Langjökull volcanic system is mountainous as it has ice age subglacially erupted tuyas and
tindar Tindar (, also Romanized as Tīndar) is a village in Zalaqi-ye Sharqi Rural District, Besharat District, Aligudarz County, Lorestan Province, Iran Iran, officially the Islamic Republic of Iran (IRI) and also known as Persia, is a count ...
s up to long, with post glaciation lava shields and volcanic fissures with the predominant lava being
olivine The mineral olivine () is a magnesium iron Silicate minerals, silicate with the chemical formula . It is a type of Nesosilicates, nesosilicate or orthosilicate. The primary component of the Earth's upper mantle (Earth), upper mantle, it is a com ...
tholeiite basalt The tholeiitic magma series () is one of two main magma series in subalkaline igneous rocks, the other being the calc-alkaline series. A magma series is a chemically distinct range of magma compositions that describes the evolution of a mafic ...
. Only effusive eruptions have been identified. The Oddnýjarhnjúkur central volcano has caldera structures that have at their rim silicic hyaloclastite that formed during the ice age. The oldest deposits are about 800,000 years old. The Skjaldbreiður lava shield has three lava units deposited between 6000 and 9000 years BP, and covers with a volume of about . It is sometimes considered a separate volcanic system with the southern fissures having erupted lavas with ages between 10,200 years and the most recent Thjófahraun lava field of the Oddnýjarhnjúkur-Langjökull volcanic system of 3600 years ago. The 7800 years BP Kjalhraun flow to the north-east has a similar area but covers only with its eastern portion broken up by faulting from the
Hofsjökull volcanic system __NOTOC__ The Hofsjökull volcanic system (also Hofsjökull-Kerlingarfjöll volcanic system) contains the largest active central volcano in Iceland. It is called Hofsjökull ( Icelandic: "temple glacier", ), after the icecap of the same name. ...
. On the Kjalhraun flow's northern edge is the Hveravellir high-temperature geothermal field with an area of .


Tectonics

As part of the Western volcanic zone of Iceland which is a receding rift, and the north–western edge of the
Hreppar microplate The geological deformation of Iceland is the way that the rocks of the island of Iceland are changing due to tectonic forces. The geological deformation help to explain the location of earthquakes, volcanoes, fissures, and the shape of the island. ...
, the Oddnýjarhnjúkur-Langjökull volcanic system does not accommodate currently as much of the mutual movement of the North American Plate and Eurasian Plate as the volcanic zones to its south or east. The Western volcanic zone is an ultra-slow divergent spreading center, spreading at about /year at the
Hengill Hengill () is a volcanic table mountain situated in the south-west of Iceland, to the south of Þingvellir. The volcano is still active, as evidenced by its numerous hot springs and fumaroles, but the last eruption occurred approximately 2,000&n ...
triple junction at its south and with no spread where the Mid-Iceland belt which is the northern boundary of the Hreppar microplate meets the Western volcanic zone at Langjökull. The closeness of the
Iceland hotspot The Iceland hotspot is a hotspot that is partly responsible for the high volcanic activity that has formed the Iceland Plateau and the island of Iceland. It contributes to understanding the geological deformation of Iceland. Iceland is one ...
to the east is believed to increase the magma supply.


Notes


References


Sources

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External links


Oddnýjarhnjúkur-Langjökull
in the
Catalogue of Icelandic Volcanoes The Catalogue of Icelandic Volcanoes (CIV) is a web resource that was created to serve as an official source of information about potentially active volcanoes monitored by Iceland. The creation of the website followed the disruptive 2010 eruption ...
* {{DEFAULTSORT:Langjökull Central volcanoes of Iceland Active volcanoes West Volcanic Zone of Iceland Volcanic systems of Iceland