Tindfjallajökull
Tindfjallajökull | |
---|---|
Highest point | |
Elevation | 1,462 m (4,797 ft) |
Coordinates | 63°48′N 19°35′W / 63.8°N 19.58°WCoordinates: 63°48′N 19°35′W / 63.8°N 19.58°W |
Geography | |
Location | Iceland |
Parent range | Mid-Atlantic Ridge |
Geology | |
Mountain type | Stratovolcano |
Last eruption | Possibly Holocene |
Tindfjallajökull (Icelandic pronunciation: [ˈtʰɪntˌfjatlaˌjœːkʏtl̥]) is a stratovolcano in the south of Iceland.[1] It has erupted rocks of basaltic to rhyolitic composition, and a 5-km-wide caldera was formed during the eruption of the 54,000-year-old Thórsmörk Ignimbrite. It is capped by a glacier of 19 km².[2] Its highest peak is Ýmir [ˈiːmɪr̥] (1462m),[2][3] which takes its name from the giant Ýmir of Norse mythology. The most recent eruption was at an unknown time in the Holocene.[1]
The name means "Tindfjöll glacier". Tindfjöll ([ˈtʰɪntˌfjœtl̥], "peak mountains") is a ridge that extends to the south of the glacier.
The rivers that flow from the glacier are Hvítmaga to the north-east, Gilsá to the south, Þórólfsá to the south-west, Valá to the north-west and Blesá to the north. Hvítmaga, Gilsá and Þórólfsá drain into Markarfljót while Valá and Blesá drain into Eystri Rangá.
See also[]
- List of volcanoes in Iceland
- Glaciers of Iceland
- Volcanism of Iceland
References[]
External links[]
- Tindfjallajökull in the
- Map of the area
Wikimedia Commons has media related to Tindfjallajökull. |
- Stratovolcanoes of Iceland
- Holocene volcanoes
- Southern Region (Iceland)
- East Volcanic Zone of Iceland
- Glaciers of Iceland
- Subglacial volcanoes of Iceland
- Calderas of Iceland
- Central volcanoes of Iceland
- Glacier stubs
- Iceland geography stubs