Torfajökull
Sign in to saveTorfajökull (Icelandic for "Torfi's glacier"; ) 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.
Key facts
- Mountain.name
- Torfajökull
- Mountain.photo
- File:Landmannalaugar 1 Iceland zoom.jpg
- Mountain.photo_caption
- Torfajökull
- Mountain.elevation_m
- 1,281
- Mountain.map
- Iceland
- Mountain.map_size
- 200
- Mountain.label_position
- right
- Mountain.location
- Iceland
- Mountain.type
- Stratovolcano
- Mountain.age
- Pleistocene
- Mountain.last_eruption
- March 1477
- Mountain.mapframe
- no
- Mountain.map_caption
- 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).
- Glacier.name
- Torfajökull
- Glacier.type
- Glacier
- Glacier.location
- Iceland
- Glacier.area
- .
- Glacier.status
- Retreating
via Wikipedia infobox
Described at
Icelandic Volcanoes
icelandicvolcanoes.is →Link to a page describing this subject · 2,681 chars · not written by Vinony
Wikidata facts
- Elevation
- 1190
- Image
- Landmannalaugar 1 Iceland zoom.jpg
Show 3 more facts
- Commons category
- Torfajökull
- Commons gallery
- Torfajökull
- described at URL
- icelandicvolcanoes.is//?volcano=TOR
Sources (2)
via Wikidata · CC0
~8 min read
Article
11 sectionsContents
- Geography
- Volcano
- Geology
- Seismic Activity
- Eruptions
- Glaciers
- Naming
- See also
- Notes
- References
- External links
Torfajökull (Icelandic for "Torfi's glacier"; ) 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.
== Geography == The volcano is located north of Mýrdalsjökull and south of Þórisvatn Lake, Iceland. To its south-west is the volcano and glacier of Tindfjallajökull and almost directly to its west is the volcano of Hekla. Adjacent to the southern edge of its glacier of Torfajökull it has a peak of but the south-eastern caldera margin also extends to the glacier of Kaldaklofsjökull which is on the western slopes of a peak called Háskerðingur that is high. Laufafell dome at is at the north-western edge of the Torfajökull volcanic system and almost halfway between Hekla and the glacier of Torfajökull.
On the map
4 mapped locations
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