Iceland Volcano Eruption
Iceland Volcano Eruption
Volcanic eruptions are not uncommon in Iceland because of its location on the mid-Atlantic ridge, where the North American and Eurasian tectonic plates meet. Iceland has a high level of geothermal activity, leading to various volcanic events over time.
If a volcano has recently erupted in Iceland, please refer to the latest news sources for the latest information about the specific event, including the location, nature of the eruption, effects on surrounding areas, and any Reaction or mitigation. Actions taken by the authorities
In the region's Fugradalsafjal volcanic system, lava fountains erupt spectacularly from 500- and 750-meter-long fissures in the ground. Volcanic activity in the area lasted for six months this year, prompting thousands of Icelanders and tourists to visit the site.
In March 2021
In March 2021, lava fountains erupted spectacularly from a fissure in the ground measuring between 500 and 750 meters long in the region's Fagradalsfjall volcanic system.
On August 3, 2022
On August 3, 2022, a volcano erupted in Iceland's Reykjavik peninsula. The eruption occurred in the Fagradalsfjall volcanic system, which had been dormant for over 6,000 years.
Fagradalsfjall volcanic system, Iceland
It was preceded by a series of earthquakes, and fountains of lava erupted from fissures 500 and 750 meters long in the ground. The eruption lasted for six months, and the lava flow covered an area of about 4.7 square kilometers.
Lava fountains erupting from a fissure in the ground in Fagradalsfjall, Iceland
The eruption was a major tourist attraction, with thousands of people visiting the site to watch the lava flow and breathe in the sulfur fumes. However, the eruption also had negative effects on the environment, with volcanic ash and gases polluting the air and water.
Tourists watching the lava flows in Fagradalsfjall, Iceland
The eruption of the Fagradalsfjall volcano was a reminder of the power of nature and the importance of being prepared for natural disasters. It is also a reminder of the importance of protecting the environment, as volcanic eruptions can significantly affect air and water quality.
Latest "Iceland Volcano Eruption
No volcano has erupted in Iceland since the eruption of Fagradalsfjall volcano on August 3, 2022. However, scientists are still monitoring the Fagradalsfjall volcanic system for signs of future activity.
On November 11, 2023, the Icelandic Meteorological Office (IMO) issued a warning that a new volcanic eruption is likely in the Reykjanes peninsula. The IMO said there has been a significant increase in seismic activity in the region, and that the ground is deteriorating.
The IMO evacuated a small town, Grindavik, which is located near the Fugradasfjal volcano. However, the explosion did not occur, and the IMO lifted the evacuation order on 12 November.
The IMO said it is still possible that a volcano could erupt in the Reykjanes peninsula in the near future. IMO is closely monitoring the situation and will provide updates as needed.
Here is a link to the latest information from the IMO on the Reykjanes Peninsula:
[IMO website link] https://www.imo.im/
Important Note: Please note that this is a developing situation, and information may change.
The slant of volcanoes in Iceland
| Name | Elevation | Coordinates | Last eruption | VIEW | Notes | |
|---|---|---|---|---|---|---|
| (m) | (ft) | |||||
| Askja | 1516 | 4974 |  65.03°N 16.75°W |
1961 | 5 | |
| Bárðarbunga | 2005 | 6515 | 64.64°N 17.56°W |
2014–2015 | ||
| Brennisteinsfjöll | 626 | 2054 | 63.92°N 21.83°W |
1341 (± 1 year) | 2 | |
| Eldfell | 279 | 915 | 63.43°N 20.25°W |
1973 | 3 | A volcanic cone on the island of Heimaey |
| Eldgjá | ca 800 | ca 2625 | 64.24°N 18.37°W |
934 | 6 | A large eruptive fissure in connection with Katla |
| Esjufjöll | 1760 | 5774 | 64.27°N 16.65°W |
1927 | ||
| Eyjafjallajökull | 1666 | 5466 | 63.63°N 19.62°W |
2010 | 4 | |
| Fagradalsfjall | 385 | 1263 | 63.89°N 22.27°W |
2023 | 0 | Eruptions in 2021, 2022, and 2023. Usually considered part of Krýsuvík. |
| Fremrinámur | 939 | 3081 | 65.43°N 16.65°W |
800 BC (± 300 years) | ||
| Grensdalur | 497 | 1631 | 64.02°N 21.17°W |
dormant | Active during Pleistocene | |
| Grímsnes | 214 | 702 | 64.03°N 20.87°W |
~3500 BC | 3 | |
| Grímsvötn | 1725 | 5659 | 64.42°N 17.33°W |
2011 | 4 | |
| Hekla | 1491 | 4892 | 63.98°N 19.70°W |
2000 | 3 | |
| Helgafell | 227 | 745 | 63.43°N 20.26°W |
3950 BC (± 300 years) | Vestmannaeyjar island of Heimaey | |
| Hengill | 803 | 2634 | 64.18°N 21.33°W |
150 AD (± 75 years) | 2 | |
| Herðubreið | 1682 | 5518 | 65.18°N 16.34°W |
dormant | Active during Pleistocene | |
| Hofsjökull | 1782 | 5846 | 64.85°N 19.53°W |
dormant | Active during Holocene | |
| Holuhraun | 778 | 2553 | 64.84°N 16.83°W |
2015 | Part of the Bárðarbunga fissure system | |
| Hrómundartindur | 540 | 1772 | 64.07°N 21.20°W |
10,000 BC | ||
| Hveravellir | 1360 | 4462 | 64.75°N 19.98°W |
950 AD ± 50 years | 6 | Central volcano of the eastern Langjökull system |
| Hverfjall | 420 | 1378 | 65.36°N 16.53°W |
~500 BC | Part of the Krafla fissure system | |
| Jólnir | 70* | 230* | 63.30°N 20.63°W |
1966 | This vent of Surtsey has since eroded to below-sea-level | |
| Katla | 1512 | 4961 | 63.63°N 19.05°W |
1918 | ||
| Kerlingarfjöll | 1488 | 4882 | 64.63°N 19.32°W |
dormant | Active during Holocene | |
| Kolbeinsey Ridge | 5 | 16 | 66.67°N 18.50°W |
1755[1] | ||
| Kollóttadyngja | 1177 | 3825 | 65.22°N 16.55°W |
unknown | ||
| Krafla | 650 | 2133 | 65.73°N 16.78°W |
1984 | 4 | |
| Krakatindur | 300 | 984 | 63.55°N 19.30°W |
unknown | ||
| Krýsuvík | 379 | 1243 | 63.93°N 22.10°W |
probably ~1340 | 2 | |
| Kverkfjöll | 1920 | 6299 | 64.65°N 16.72°W |
1968 | 1 | |
| Laki | 1725 | 5606 | 64.06°N 18.22°W |
1783-84 | 6 | Part of Grímsvötn fissure system |
| Loki-Fögrufjöll | 1570 | 5151 | 64.48°N 17.80°W |
1910 | ||
| Ljósufjöll | 988 | 3241 | 64.87°N 22.23°W |
960 AD (± 10 years) | 3 | |
| Lýsuhóll | 540+ | 1772+ | 64.87°N 23.25°W |
dormant | Active during Holocene | |
| Öræfajökull | 2119 | 6952 | 64.00°N 16.65°W |
1727 | 5 | |
| Prestahnúkur | 1386 | 4504 | 64.60°N 20.60°W |
7550 BC (± 500 years) | Central volcano of western Langjökull system | |
| Reykjanes | 230 | 755 | 63.88°N 22.50°W |
1879 | ||
| Reykjaneshryggur | -80 | -262 | 63.67°N 23.33°W |
1970 | ||
| Snæfellsjökull | 1448 | 4751 | 64.80°N 23.78°W |
200 AD (± 150 years) | 2 | |
| Surtsey | 174 | 571 | 63.30°N 20.62°W |
1963 | In the Vestmannaeyjar islands | |
| Theistareykjarbunga (Þeistareykjarbunga) |
564 | 1850 | 65.88°N 16.83°W |
750 BC (± 100 years) | ||
| Thórðarhyrna (Þórðarhyrna) |
1660 | 5446 | 64.12°N 17.0°W |
1910 | 4 | |
| Thórólfsfell (Þórólfsfell) |
574 | 1883 | 63.72°N 19.67°W |
unknown | ||
| Thríhnákagígur (Þríhnákagígur) |
550 | 1804 | 63.99°N 21.7°W |
2 BC | ||
| Tindfjallajökull | 1463 | 4800 | 63.78°N 19.57°W |
dormant | Active during Holocene | |
| Torfajökull | 1259 | 4131 | 63.92°N 19.17°W |
1477 | 3 | |
| Trölladyngja | 1468 | 4816 | 64.89°N 17.25°W |
~2980 BC | ||
| Tungnafellsjökull | 1535 | 5036 | 64.73°N 17.92°W |
dormant | Active during Holocene | |
| Vatnafjöll | 1235 | 4052 | 63.92°N 19.67°W |
750 AD (± 1000[dubious – discuss] years) | ||
