Iceland is located on the Mid-Atlantic Ridge, a divergent plate boundary where two plates are moving apart. This area is highly volcanic due to the molten rock (magma) from the Earth’s mantle being forced up through the gap between the two plates. The magma then cools and solidifies to form new crust, which is then pushed away from the ridge by the two plates. This process is known as seafloor spreading and is the main cause of volcanic activity in Iceland.

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.

Active volcanic areas and systems in Iceland

Volcanic and transform zones of Iceland

Eruption column of Eyjafjallajökull in 2010

Iceland experiences frequent volcanic activity, due to its location both on the Mid-Atlantic Ridge, a divergent tectonic plate boundary, and over a hot spot. Nearly thirty volcanoes are known to have erupted in the Holocene epoch; these include Eldgjá, source of the largest lava eruption in human history.

Volcanic systems and volcanic zones of Iceland

Holocene volcanism in Iceland is mostly to be found in the Neovolcanic Zone, comprising the Reykjanes Volcanic Belt (RVB), the West Volcanic Zone (WVZ), the Mid-Iceland Belt (MIB), the East Volcanic Zone (EVZ) and the North Volcanic Zone (NVZ). Two lateral volcanic zones play a minor role: Öræfi Volcanic Belt (ÖVB) and Snæfellsnes Volcanic Belt (SVB). Outside of the main island are the Reykjanes Ridge (RR), as part of the Mid-Atlantic Ridge to the southwest and the Kolbeinsey Ridge (KR) to the north. Two transform zones are connecting these volcano-tectonic zones: the South Iceland Seismic Zone (SISZ) in the south of Iceland and the Tjörnes Transform Zone (TFZ) in the north.

The island has around 30 active volcanic systems, comprising each volcano-tectonic fissure systems and many of them also a central volcano (mostly in the form of a stratovolcano, sometimes of a shield volcano with a magma chamber underneath). Thirteen volcanic systems have hosted eruptions since the settlement of Iceland in AD 874.

Of these 30 active volcanic systems, the most active is Grímsvötn. Over the past 500 years, Iceland’s volcanoes have produced a third of the total global lava output.

Important eruptions

See also : List of volcanic eruptions in Iceland


Hekla has erupted more than 20 times in recorded history. It was known to medieval Europeans as the Gate of Hell; that reputation persisted into the 19th century.

Laki/Skaftáreldar 1783-84

The most deadly volcanic eruption of Iceland’s history was the so-called Skaftáreldar (fires of Skaftá) in 1783. The eruption was in the crater row Lakagígar (craters of Laki) southwest of Vatnajökull glacier. The craters are a part of a larger volcanic system with the subglacial Grímsvötn as a central volcano. Roughly a quarter of the Icelandic population died because of the eruption. Most died not because of the lava flow or other direct effects of the eruption but from indirect effects, including changes in climate and illnesses in livestock in the following years caused by the ash and poisonous gases from the eruption. The eruption is thought to have erupted the largest quantity of lava from a single eruption in historic times.[citation needed]

Eldfell 1973

Eldfell is a volcanic cone on the east side of Heimaey which formed during an eruption in January 1973. The eruption happened without warning, causing the island’s population of about 5,300 people to evacuate on fishing boats within a few hours. Importantly, the progress of lava into the harbour was slowed by manual spraying of seawater. One person died, and the eruption resulted in the destruction of homes and property on the island.[citation needed]

Eyjafjallajökull 2010

The eruption under Eyjafjallajökull in April 2010 caused extreme disruption to air travel across western and northern Europe over a period of six days in April 2010. About 20 countries closed their airspace to commercial jet traffic and it affected approximately 10 million travellers.

The eruption had a volcano explosivity index of 4, the largest known from Eyjafjallajökull. Several previous eruptions of Eyjafjallajökull have been followed soon afterwards by eruptions of the larger volcano Katla, but after the 2010 eruption, no activity occurred at Katla.

Grímsvötn 2011

The eruption in May 2011 at Grímsvötn under the Vatnajökull glacier sent thousands of tonnes of ash into the sky in a few days, raising concerns of a repeat of the travel chaos seen across northern Europe.[citation needed]

The craters of Grábrók

Bárðarbunga 2014–2015

Bárðarbunga is a stratovolcano and is roughly 2,000 metres (roughly 6,560 feet) above sea level in central Iceland. This makes it the second highest mountain in Iceland. Its 2014-2015 eruption was Iceland’s largest in 230 years. The eruption started on August 17, 2014 and lasted for 180 days, Following a major earthquake swarm, multiple lava fountain eruptions began in Holuhraun. The lava flow rate was between 250 and 350 cubic metres per second and came from a dyke over 40 km long. An ice-filled subsidence bowl over 100 square kilometres in area and up to 65 metres deep formed as well. There was very limited ash output from this eruption unlike numerous glacial eruptions which are common in Iceland. The primary concern with this eruption was the large plumes of sulphur dioxide (SO2) in the atmosphere which adversely affected breathing conditions across Iceland, depending on wind direction. The volcanic cloud was also transported toward Western Europe in September 2014.

2021 Fagradalsfjall volcanic eruption

Fagradalsfjall 2021

Following a three-week period of increased seismic activity, an eruption fissure developed near Fagradalsfjall, a mountain on the Reykjanes Peninsula. Lava flow from a 200-meter fissure was first discovered by an Icelandic Coast Guard helicopter on March 19, 2021 in the Geldingadalur area near Grindavík, and within hours the fissure had grown to 500 meters in length.

Structure of lava fields

Pāhoehoe (helluhraun) lava fields in Iceland

ʻAʻā (apalhraun) field in Iceland

The smooth flowing basaltic lava pāhoehoe is known in Icelandic as helluhraun [ˈhɛtlʏˌr̥œiːn]. It forms smooth surfaces that are quite easy to cross. More viscous lava forms ʻaʻā flows, known in Icelandic as apalhraun [ˈaːpalˌr̥œiːn]. The loose, broken, sharp, spiny surface of an ʻaʻā flow makes hiking across it difficult and slow.

See also


External links

By topic

Source: Volcanism of Iceland

Video about The Icelandic Volcanoes Are Related To Plate Tectonics Because

Iceland's Volcanic World | National Geographic

Question about The Icelandic Volcanoes Are Related To Plate Tectonics Because

If you have any questions about The Icelandic Volcanoes Are Related To Plate Tectonics Because, please let us know, all your questions or suggestions will help us improve in the following articles!

The article The Icelandic Volcanoes Are Related To Plate Tectonics Because was compiled by me and my team from many sources. If you find the article The Icelandic Volcanoes Are Related To Plate Tectonics Because helpful to you, please support the team Like or Share!

Rate Articles Volcanism of Iceland

Rate: 4-5 stars
Ratings: 4110
Views: 65591428

Search keywords The Icelandic Volcanoes Are Related To Plate Tectonics Because

1. Iceland Volcanism
2. Icelandic Volcanoes
3. Icelandic Volcanic Eruptions
4. Icelandic Volcanic Activity
5. Icelandic Volcanic Hazards
6. Icelandic Magma
7. Icelandic Magma Chambers
8. Icelandic Geothermal Activity
9. Icelandic Plate Tectonics
10. Icelandic Hot Spots
#Volcanism #Iceland