 | This article needs additional citations for
verification. (August 2021) |
| Hverfjall | |
|---|---|
 The Hverfjall crater from the south | |
| Highest point | |
| Elevation | 420 m (1,380 ft) |
| Coordinates | 65°36′00″N 16°53′00″W / 65.60000°N 16.88333°W |
| Geography | |
| Location | Iceland |
| Geology | |
| Mountain type | Tephra cone, tuff ring volcano |
| Last eruption | 2500 BP |
Hverfjall (Icelandic pronunciation: [ˈkʰvɛrˌfjatl̥] ; also known as Hverfell [ˈkʰvɛrˌfɛtl̥]) is a tephra cone or tuff ring volcano in northern Iceland, to the east of Mývatn.
It erupted in 2500 BP in the southern part of the Krafla fissure swarm. [1] The crater is approximately 1 km in diameter. [2]
Tephra has been carried from Hverfjall all over the Mývatn area. A landslide apparently occurred in the south part of the crater during the eruption, which accounts for the disruption to the round shape of the mountain.[ citation needed] During the Age of Settlement, lava flowed from Svörtuborgir [ˈsvœr̥tʏˌpɔrcɪr̥], at the southern end of Námafjall [ˈnauːmaˌfjatl̥], around Hverfjall, which was nearly engulfed by the lava. At the same time an eruption occurred in the slopes above the valley of Hlíðardalur [ˈl̥iːðarˌtaːlʏr̥].[ citation needed]
The rim of the crater is only accessible by two paths, from the northwest and south. It is strictly forbidden to use other routes in ascent or descent.
- ^ The Hverfjall fissure eruption Archived 2011-07-28 at the Wayback Machine Accessed 29 October 2008
- ^ Rough Guide on Hverfjall[ permanent dead link] Accessed 29 October 2008
Media related to
Hverfjall at Wikimedia Commons
| International | |
|---|---|
| Geographic | |
 | This Iceland location article is a stub. You can help Wikipedia by expanding it. |
| This article needs additional citations for
verification. (August 2021) |
| Hverfjall | |
|---|---|
|
The Hverfjall crater from the south | |
| Highest point | |
| Elevation | 420 m (1,380 ft) |
| Coordinates | 65°36′00″N 16°53′00″W / 65.60000°N 16.88333°W |
| Geography | |
| Location | Iceland |
| Geology | |
| Mountain type | Tephra cone, tuff ring volcano |
| Last eruption | 2500 BP |
Hverfjall (Icelandic pronunciation: [ˈkʰvɛrˌfjatl̥] ; also known as Hverfell [ˈkʰvɛrˌfɛtl̥]) is a tephra cone or tuff ring volcano in northern Iceland, to the east of Mývatn.
It erupted in 2500 BP in the southern part of the Krafla fissure swarm. [1] The crater is approximately 1 km in diameter. [2]
Tephra has been carried from Hverfjall all over the Mývatn area. A landslide apparently occurred in the south part of the crater during the eruption, which accounts for the disruption to the round shape of the mountain.[ citation needed] During the Age of Settlement, lava flowed from Svörtuborgir [ˈsvœr̥tʏˌpɔrcɪr̥], at the southern end of Námafjall [ˈnauːmaˌfjatl̥], around Hverfjall, which was nearly engulfed by the lava. At the same time an eruption occurred in the slopes above the valley of Hlíðardalur [ˈl̥iːðarˌtaːlʏr̥].[ citation needed]
The rim of the crater is only accessible by two paths, from the northwest and south. It is strictly forbidden to use other routes in ascent or descent.
- ^ The Hverfjall fissure eruption Archived 2011-07-28 at the Wayback Machine Accessed 29 October 2008
- ^ Rough Guide on Hverfjall[ permanent dead link] Accessed 29 October 2008
Media related to
Hverfjall at Wikimedia Commons
| International | |
|---|---|
| Geographic | |
|
| This Iceland location article is a stub. You can help Wikipedia by expanding it. |