Torfajökull
| Torfajökull | |
|---|---|
Torfajökull | |
| Highest point | |
| Elevation | 1,281 m (4,203 ft) |
| Coordinates | 63°55′00″N 19°10′00″W / 63.91667°N 19.16667°W |
| Dimensions | |
| Area | 450 km2 (170 sq mi) |
| Geography | |
Torfajökull Geological features near the Torfajökull volcanic system (red outlines) - In particular note that the Bárðarbunga volcanic system is also emphasised as the last two Torfajökull rhyolites (877 and 1477 CE) were erupted simultaneous with Veidivötn (Bárðarbunga) basalts (Light violet shading). Legend
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Geological features near the Torfajökull volcanic system (red outlines) - In particular note that the Bárðarbunga volcanic system is also emphasised as the last two Torfajökull rhyolites (877 and 1477 CE) were erupted simultaneous with Veidivötn (Bárðarbunga) basalts (Light violet shading). Legend
| |
| Location | Iceland |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Stratovolcano |
| Last eruption | March 1477 |
Torfajökull (Icelandic for "Torfi's glacier"; Icelandic pronunciation: [ˈtʰɔrvaˌjœːkʏtl̥] ⓘ) is a rhyolitic stratovolcano, with a large caldera (central volcano) capped by a glacier of the same name and associated with a complex of subglacial volcanoes. Torfajökull last erupted in 1477 and consists of the largest area of silicic extrusive rocks in Iceland. This is now known to be due to a VEI 5 eruption 55,000 years ago.