Öræfajökull

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Template:Short description Template:Infobox mountain

Hvannadalshnúkur, the highest peak of Öræfajökull.

Öræfajökull ({{#invoke:IPA|main}}; 'Öræfi glacier' or 'wasteland glacier') is an ice-covered volcano in south-east Iceland. The largest active volcano and the highest peak in Iceland at Template:Convert, it lies within the Vatnajökull National Park and is covered by part of the glacier.

The original Norse settlers named the volcano Knappafellsjǫkull (Old Norse: {{#invoke:IPA|main}}; Modern Icelandic: Hnappafellsjökull {{#invoke:IPA|main}}; 'knobs mountain glacier').<ref name="volcano-cafe">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The current name, Öræfajökull, was eventually adopted after the 1362 eruption.

Description

Öræfajökull is located at the southern extremity of the Vatnajökull glacier and overlooking the Ring Road between Höfn and Vík. It is the largest active volcano in the country, and on the summit crater's north-western rim is Hvannadalshnúkur, the highest peak in Iceland at Template:Convert.

Geographically, Öræfajökull as the glacier, is considered part of Vatnajökull, and the area covered by glacier is within the boundary of Vatnajökull National Park. There are a number of outlet glaciers in the ice cap within the area of the central volcano which clockwise from north are: Breiðamerkurjökull, Fjallsjökull, Hrútárjökull, Bræðrajökull, Kviarjökull, Hólárjökull, Stórhöfðajökull, Gljúfursárjökull, Rótarfjallsjökull (which has a western branch called Kotárjökull), Grænafjallsjökull, Falljökull, Virkisjökull, Svinafellsjökull and Skaftafellsjökull.<ref name=NLSI>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> While most of the outlet glaciers have reasonably clear catchments, not all do. Some of the icecap feeds directly into river catchments without a named glacier and this happens between the Hrútárjökull and Bræðrajökull, and the Virkisá river drains a number of glaciers between Rótarfjallsjökull and Svinafellsjökull (see map on this page).<ref name=NLSI /><ref name=Magnússon2012>Template:Cite journal</ref>Template:Rp

The summit caldera of this stratovolcano is Template:Cvt and the volcano is Template:Cvt in diameter.<ref name=CIV>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> It is the most southern of the volcanoes in the Öræfi volcanic belt (Öræfajökull volcanic belt), which is possibly an embryonic rift parallel and to the east of the Eastern volcanic zone.<ref name=Barsotti2018>Template:Cite journalTemplate:Rp</ref> The presently active summit caldera may have a subcaldera within it.<ref name=Magnússon2012 />Template:Rp Eruptions in this area are most likely to result in jökulhlaups that will produce floods at the outlets of the Kviarjökull and Virkisá catchments as these overlap the present caldera.<ref name=Magnússon2012 />Template:Rp There is possibly an old caldera to the north of the current caldera and flank eruptions could produce jökulhlaup from other outlet glaciers.<ref name=Magnússon2012 /> The topographical map on this page can be enlarged to show this detail.

Activity

Öræfajökull has erupted twice in historical times, in 1362 and 1728. These were explosive silicic eruptions with bulk tephra volumes of Template:Cvt and jökulhlaups occurred.<ref name=CIV /> The deposits closer to the central volcano are rhyolytic but the more distal lava flows which can extend for Template:Cvt from the caldera are alkali olivine basalt and both have been erupted in the Holocene.<ref name=CIV />

1362 eruption

In 1362, Knappafellsjökull erupted explosively, ejecting 10 cubic kilometres of tephra,<ref name="about">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> similar in scale to the 1991 eruption of Mount Pinatubo.<ref name="volcano-cafe" /> The eruption sequence lasted for several months, being from a medium-potassium alkali rhyolite and has been assigned a VEI of 6 although dense-rock equivalent volume may be less than previous estimates at Template:Cvt.<ref name=Barsotti2018 /> The wealthy district of Litlahérað was destroyed by floods, pyroclastic flows and ashfall.<ref name="about" /> Sailors reported pumice “in such masses that ships could hardly make their way through it.” Thick volcanic deposits obliterated farmland, and ash travelled as far as western Europe. Forty farms were destroyed.<ref name=EBI2011>{{#if: |

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  }}{{#ifeq:  ||}}</ref> More than 40 years passed before people again settled the area, which became known as Öræfi. The name literally means 'an area without harbour,' but it took on a meaning of 'wasteland' in Icelandic, as the 1362 eruption had drastically altered the environment around the mountain.<ref name="Guardian 3 Dec 2017"/>  The volcano likewise took on the new name Öræfajökull.

1728 eruption

An eruption in August 1727–1728 was smaller than 1362, though floods are known to have caused three fatalities when the meltwater swept their farm away.<ref name="Guardian 3 Dec 2017">Template:Cite news</ref>

1899 map of Öræfajökull from a nautical chart

2017 activity

Increased earthquake activity in the form of small tremors ranging from a depth of 1.5–10 km beneath the summit crater, began in August 2017 according to the Icelandic Meteorological Office.

The Aviation Colour Code of the United States was raised to yellow on 17 November 2017, after the appearance of an ice cauldron inside the main crater and increased geothermal activity under the glacier.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

2018 activity

The seismic and geothermal activity which began in August 2017 continued into 2018, but at reduced levels. On 4 May 2018, the Icelandic Meteorological Office lowered the Aviation Colour Code to green. <ref name="GVP">Template:Cite gvp</ref>

Landslide

In 2013 due to paraglacial slope failure, a large landslide affecting an area of Template:Cvt occurred, that deposited debris on the volcano's Svínafellsjökull outlet glacier.<ref>Template:Cite journal</ref>

See also

References

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