Holuhraun is situated at the southern end of Ódáðahraun [ˈouːˌtauːðaˌr̥œyːn], which is one of the largest lava fields in the country. The main volume of the Jökulsá á Fjöllum river flows from the eastern side of Holuhraun, in the Kverkfjöll area.^[1] Hrímalda [ˈr̥iːmˌalta], Urðarháls [ˈʏrðarˌhauls] and Kistufell [ˈcʰɪstʏˌfɛtl̥] are to the west of Holuhraun, with Dyngjuháls [ˈtiɲcʏˌhauls] and Trölladyngja beyond.^[4] The Dyngjujökull glacier, which is part of Vatnajökull, is to the immediate south.^[1][4] Holuhraun is about 15 km (9.3 mi) south of the Askja caldera,^[5] and the Bárðarbunga volcano is 41.39 km (25.7 mi) to the south-west^[6] of Holuhraun. Holuhraun is traversed by an unnumbered road, which connects to the Route F910 gravel road at both the east and the west ends.^[7][8]

Located at the northern and southern extensions of the Bárðarbunga and Askja fissure systems, respectively, the soil is mainly composed of lavas derived from these volcanoes, either in the form of flows or alluvial deposits of volcanic origin. The geological configuration, along with the presence of nearby subglacial volcanoes such as Bárðarbunga and Grímsvötn, is responsible for the risk of jökulhlaups, which have affected Holuhraun repeatedly.

Until 2014, the surface of the lava field was of an older lava flow, which was assumed to have erupted from a vent associated with Askja in 1797, but this is no longer accepted.^[a] In the early hours of 29 August 2014, a small fissure eruption occurred in Holuhraun at the northern end of a magma intrusion which had moved progressively north, since 16 August, from the Bárðarbunga volcano.^[3] The progression of the magma intrusion was accompanied by an earthquake swarm.^[13] The eruption began just after midnight and stopped at 04:00 GMT.^[14] The active fissure was about 600 m (660 yd) in length.^[15]

Another fissure eruption started in Holuhraun at around 05:05 GMT on the morning of 31 August 2014, in the same rift as the eruption which had occurred two days earlier.^[16] The eruptive fissure was estimated to be 1.5 km (0.93 mi) long.^[15] By 4 September, the total area of the lava flow was estimated at 10.8 km² (4.2 sq mi).^[15] Two new eruptive fissures formed south of the main eruption site, on 5 September.^[15] The new fissures were substantially smaller than the older fissure.^[15] By 7 September, the lava flow had extended 11 km (6.8 mi) to the north, and had reached the main western branch of the Jökulsá á Fjöllum river.^[15] The eruption showed no visible activity in the southern fissure, on the evening of 7 September.^[15] The lava flow is considered to be the largest in recent decades in Iceland and covered 44 km² (17 sq mi) on 29 September.^[17] The volcanic eruption in Holuhraun continued with similar intensity as the previous few weeks. The lava field covered 63 km² (24 sq mi) in late October. On 11 November, it was reported that the lava field extended to 70 km² (27 sq mi) and more than 1 km³ (0.24 cu mi) in volume - the largest in Iceland since the Laki eruption of 1783.^[3][18]

The eruption ended on 27 February 2015. The Holuhraun lava field measures more than 85 km² (33 sq mi) and the volume is around 1.6 km³ (0.38 cu mi).

Several names were proposed for the new lava field in the Holuhraun area, among them Flæðahraun, Nornahraun, and Urðarbruni. Finally, the decision was to keep the existing name Holuhraun,^[19] which is also consistent with current geological thought.^[a]

• Volcanism of Iceland
  • List of volcanic eruptions in Iceland
  • List of volcanoes in Iceland

• Icelandic Meteorological Office page with latest updates on the Holuhraun eruption
• 3d map of volcanic activity in Holuhraun updated live from IMO