Nombre |
Elevación (m) |
Elevación (ft) |
Coordenadas |
Última erupción |
IEV |
Notas |
Askja |
1516 | 4974 | 65.03, -16.75 (Askja) | 1961 | 5 | |
Bárðarbunga |
2005 | 6515 | 64.64, -17.56 (Bárðarbunga) | 2015 | | |
Brennisteinsfjöll |
626 | 2054 | 63.92, -21.83 (Brennisteinsfjöll) | 1341 (± 1 año) | 2 | |
Eldfell |
279 | 915 | 63.43, -20.25 (Eldfell) | 1973 | 3 | Isla Vestmannaeyjar de Heimaey |
Sistema de fisuras Eldgjá |
ca 800 | ca 2625 | 64.24, -18.37 (Eldgjá) | 934 | 6 | |
Esjufjöll |
1760 | 5774 | 64.27, -16.65 (Esjufjöll) | 1927 | | |
Eyjafjallajökull |
1666 | 5466 | 63.63, -19.62 (Eyjafjallajökull) | 2010 | 4 | |
Fagradalsfjall |
385 | 1263 | 63.89, -22.27 (Fagradalsfjall) | 2021 |
|
Actualmente en erupción |
Fremrinámur |
939 | 3081 | 65.43, -16.65 (Fremrinámur) | 800 a. C. (± 300 años) | | |
Grensdalur |
497 | 1631 | 64.02, -21.17 (Grensdalur) | Inactivo | | Activo durante el Pleistoceno |
Grímsnes |
214 | 702 | 64.03, -20.87 (Grímsnes) | ~3500 a. C. | 3 | |
Grímsvötn |
1725 | 5659 | 64.42, -17.33 (Grímsvötn) | 2011 | 4 | |
Hekla |
1491 | 4892 | 63.98, -19.70 (Hekla) | 2000 | 3 | |
Hengill |
803 | 2634 | 64.18, -21.33 (Hengill) | 90 d. C. (± 100 años) | 2 | |
Herðubreið |
1682 | 5518 | 65.18, -16.34 (Herðubreið) | Inactivo | | Activo durante el Pleistoceno |
Hofsjökull |
1782 | 5846 | 64.85, -19.53 (Hofsjökull) | Inactivo | | Activo durante el Holoceno |
Hrómundartindur |
540 | 1772 | 64.07, -21.20 (Hrómundartindur) | 10000 a. C. | | |
Hverfjall |
420 | 1378 | 65.36, -16.53 (Hverfjall) | ~500 a. C. | | |
Hveravellir |
1360 | 4462 | 64.75, -19.98 (Hveravellir) | 950 d. C. ± 50 años | 6 | |
Jólnir |
70* | 230* | 63.30, -20.63 (Jólnir) | 1966 | | Este respiradero del Surtsey, desde entonces, se ha erosionado por debajo del nivel del mar |
Katla |
1512 | 4961 | 63.63, -19.05 (Katla) | 1918 | 5 | Normalmente entra en erupción después de una erupción del Eyjafjallajökull |
Kerlingarfjöll |
1488 | 4882 | 64.63, -19.32 (Kerlingarfjöll) | Inactivo | | Activo durante el Holoceno |
Kolbeinsey |
5 | 16 | 66.67, -18.50 (Kolbeinsey) | 1999[1] | | |
Kollóttadyngja |
1177 | 3825 | 65.22, -16.55 (Kollóttadyngja) | Desconocido | | |
Krafla |
650 | 2133 | 65.73, -16.78 (Krafla) | 1984 | 4 | |
Krýsuvík |
379 | 1243 | 63.93, -22.10 (Krýsuvík) | ~1340 | 2 | |
Krakatindur |
300 | 984 | 63.55, -19.30 (Krakatindur) | Desconocido | | |
Kverkfjöll |
1920 | 6299 | 64.65, -16.72 (Kverkfjöll) | 1968 | 1 | |
Laki |
1725 | 5606 | 64.06, -18.22 (Laki) | 1783-84 | 6 | |
Langjökull |
1360 | 4462 | 64.75, -19.98 (Langjökull) | 925 d. C. (± 25 años) | | |
Loki-Fögrufjöll |
1570 | 5151 | 64.48, -17.80 (Fögrufjöll) | 1910 | | |
Ljósufjöll |
988 | 3241 | 64.87, -22.23 (Ljósufjöll) | 960 d. C. (± 10 años) | 3 | |
Lýsuhóll |
540+ | 1772+ | 64.87, -23.25 (Lýsuhóll) | Inactivo | | Activo durante el Holoceno |
Öræfajökull |
2119 | 6952 | 64.00, -16.65 (Öræfajökull) | 1727 | 5 | |
Prestahnúkur |
1386 | 4504 | 64.60, -20.60 (Prestahnúkur) | 7550 a. C. (± 500 años) | | |
Reykjanes |
230 | 755 | 63.88, -22.50 (Reykjanes) | 1879 | | |
Reykjaneshryggur |
-80 | -262 | 63.67, -23.33 (Reykjaneshryggur) | 1970(?) | | |
Skjaldbreiður |
1060 | 3480 | 64°24′36″N 20°45′44″O | Desconocido | | |
Snæfellsjökull |
1448 | 4751 | 64.80, -23.78 (Snæfellsjökull) | 200 d. C. (± 150 años) | 2 | |
Surtsey |
174 | 571 | 63.30, -20.62 (Surtsey) | 1963 | | Islas Westman
Isla Vestmannaeyjar |
Theistareykjarbunga |
564 | 1850 | 65.88, -16.83 (Theistareykjarbunga) | 750 d. C. (± 100 años) | | |
Thordarhyrna |
| | 64.12, -17.0 (Thordarhyrna) | 1910 | 4 | |
Thórólfsfell |
574 | 1883 | 63.72, -19.67 (Thórólfsfell) | Desconocido | | |
Tindfjallajökull |
1463 | 4800 | 63.78, -19.57 (Tindfjallajökull) | Inactivo | | Activo durante el Holoceno |
Tjörnes fracture zone |
—150 | —500 | 66.30, -17.10 (Tjörnes) | 1868 | | |
Torfajökull |
1259 | 4131 | 63.92, -19.17 (Torfajökull) | 1477 | 3 | |
Tungnafellsjökull |
1535 | 5036 | 64.73, -17.92 (Tungnafellsjökull) | Inactivo | | Activo durante el Holoceno |
Vatnafjöll |
1235 | 4052 | 63.92, -19.67 (Vatnafjöll) | 750 d. C. (± 1000 años) | | |