Rauðhólar (Vesturdalur) is a small chain of volcanoes within the Askja or the Fremrinámur volcanic systems in the north of Iceland.[1]
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They are located at the lower course of the river Jökulsá á Fjöllum, around 25 km from Öxarfjörður fjord and at the same time near Vesturdalur in Jökulsárgljúfur National Park next to the Hljóðaklettar (the echo cliffs).
Geology
editHljóðaklettar and Rauðhólar
editThe latter vents and Rauðhólar build together a small volcanic chain,[2] consisting of eruption fissures which were active 11.000 years ago. Some of the fissures crossed the river. The river destroyed the craters of Hljóðaklettar and only remnants were left standing, dikes, volcanic plugs, sills and lava flows. The erosion started with phreatomagmatic explosions during the eruption series, when water and magma met, but there was also steady fluvial erosion afterwards, incl. many big jökulhlaup. The volcanic edifices of Rauðhólar on the other hand were just opened in the direction of the river, but left intact.[3]
Jökulhlaups of Jökulsá á Fjöllum
editScientists are still discussing the exact data of the Holocene volcanogenic jökulhlaups of Jökulsá á Fjöllum, but it is possible to show the sedimentary record of no less than 16 jökulhlaups in Vesturdalur.[4]
Magmatic plumbing system
editThe magmatic plumbing system of Rauðhólar was exposed by erosion, so that a.o. the feeder dike can be seen and analyzed whereby the geologist A. Gudmundsson saw a connection between the dike and a normal fault (re)activated by the dike movements.[5] as this is still a location on the active Icelandic rift zone. Other scientists refer to the type of volcanoes as scoria cones which in this case expose a rather complicated plumbing system connected to repeated intrusions.[6]
Visitor attraction
editThe region with its very unusual rock formations is also a visitor attraction with many hiking trails, a camping area nearby and some simple facilities.[7] The road has newly been upgraded (in 2020).
The Vesturdalur valley and its rock formations are part of Jökulsárgljúfur National Park, today integrated in the bigger Vatnajökull National Park.
External sources
edit- Friese, N., Bense, F.A., Tanner, D.C. et al. From feeder dykes to scoria cones: the tectonically controlled plumbing system of the Rauðhólar volcanic chain, Northern Volcanic Zone, Iceland. Bull Volcanol 75, 717 (2013). https://doi.org/10.1007/s00445-013-0717-2
References
edit- ^ Ásta Rut Hjartardóttira, Páll Einarsson and Haraldur Sigurdsson: The fissure swarm of the Askja volcanic system along the divergent plate boundary of N Iceland. Bulletin of Volcanology 2009. Retrieved 28 July 2020. , see map p. 37
- ^ For the exact positions on a map see p.3 in: I. Galindo and A. Gudmundsson: Basaltic feeder dykes in rift zones. In: Nat. Hazards Earth Syst. Sci., 12, 3683–3700, 2012 https://www.nat-hazards-earth-syst-sci.net/12/3683/2012/ doi:10.5194/nhess-12-3683-2012 Retrieved 28 July 2020.
- ^ Snæbjörn Guðmundsson: Vegavísir um jarðfræði Íslands. Reykjavík 2015, p. 141
- ^ See p. 138: Greta Hoe Wells: Timeline Reconstruction of Holocene jökulhlaups along the Jökulsá á Fjöllum Channel, Iceland. B.A. Thesis at University of Texas, Austin 2016. Retrieved 28 July 2020.
- ^ I. Galindo and A. Gudmundsson: Basaltic feeder dykes in rift zones. In: Nat. Hazards Earth Syst. Sci., 12, 3683–3700, 2012 https://www.nat-hazards-earth-syst-sci.net/12/3683/2012/ doi:10.5194/nhess-12-3683-2012 Retrieved on 28 July 2020.
- ^ Friese, N., Bense, F.A., Tanner, D.C. et al. From feeder dykes to scoria cones: the tectonically controlled plumbing system of the Rauðhólar volcanic chain, Northern Volcanic Zone, Iceland. Bull Volcanol 75, 717 (2013). https://doi.org/10.1007/s00445-013-0717-2 Retrieved 28 July 2020.
- ^ Vatnajökulsþjoðgarður. Jökulsárgljúfur. (Official website) Retrieved 28 July 2020.