| Snæfell | |
| Elevation M: | 1833 |
| Location: | Iceland, East Iceland |
| Coordinates: | 64.7974°N -15.56°W |
| Coordinates Ref: | [1] |
| Type: | Stratovolcano |
| Last Eruption: | 207,000 ± 10,000 years ago |
| Map: | Iceland |
Snæfell (in Icelandic pronounced as /ˈsnaiːˌfɛtl̥/, "snow mountain") at high, is an ice-capped stratovolcano located in the north-east part of Vatnajökull National Park, Iceland. While it has been dormant in the Holocene, it is now known to have had repose times of over 100,000 years between eruptions, so it cannot be assumed to be extinct.
The mountain is the tallest subaerial stratovolcano in Iceland, at, and is immediately east of the Hálslón Reservoir of the Kárahnjúkar hydroelectric project and north of the Vatnajökull glacier with its Eyjabakkajökull tongue. Its ice-cap contains the following glaciers, from north clockwise:
It is the border between the municipalities of Múlaþing and Fljótsdalshreppur so the western slopes are in Múlaþing and the eastern in Fljótsdalshreppur. It is SW of Egilsstaðir by "road".
Snæfell is the northernmost central volcano in Iceland's off-rift Öræfi volcanic belt, which is regarded by some as an eastern flank zone to the northern volcanic zone. Mostly Snæfell was formed under ice cover. In addition to the main mountain, the Snæfell volcanic system has a series of fissures and smaller subglacial eruptive features, oriented in a south-west to north-east direction (27°), almost parallel to the active northern volcanic zone, which is to its west. The associated fissure swarm, which was not recognised by earlier authors, has now been mapped to be long.
The basal tholeiitic basalt sheet bedrock age on which the volcano is built, is between 2.5 to 1.8 million years old and can be easily distinguished from the current volcano's magma source which is transitional alkalic, with no evidence of admixture with continental crust, as some had postulated might be the case. Recent work has suggested that the Upptyppingar subglacial volcano to its west has compositional similarities to Snæfell which helps the argument for a flank zone concept. Snæfell compositions have been studied in some detail as they help to understand mantle plume characteristics that may be related to the Iceland hotspot, and magma evolution.
The oldest basalt of the volcano has been dated at 1350 ± 28, basalt at the summit is 256 ± 28 ka and there are multiple samples between these ages, with for example trachyandesite at 466 ± 40 ka. These are K–Ar ages and near summit rhyolite with a previous K–Ar age of 253 ± 6 ka was subsequently re-dated by the more accurate 40Ar–39Ar method to 207 ± 10 ka. The magma involved in the formation of the mountain must have come from mantle sources and uranium–lead dating of zircon is consistent with these datings. The magma has been found to have had residence times of between 100,000 to 200,000 years between eruptions, which is much longer than for other Icelandic volcanoes and means previous suspicions that the volcano might only be dormant, are more likely to be the case.
There is some hydrothermal activity at the periphery of the Snæfell volcano.
Access to the mountain is usually via Skriðuklaustur, a Vatnajökull National Park service centre, and when the park is open in summer via the F909 road that accesses the northern Brúarjökull and Eyjabakkajökull regions of Vatnajökull with a car park at the Snæfellsskáli ranger hut. The mountain top with its good views requires climbers to have special equipment and skills.[2]