Torfajökull
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Angel Peak
NW Rauðfossafjöll
SE Rauðfossafjöll
Námshraun
Hrafntinnusker
Dalakvísl
Subglacial Torfajökull eruptions
Postglacial Torfajökull eruptions
Rhyolite
Tholeiite
Mixed rhyolite-tholeiite
Alkali basalt
Other features
Torfajökull glacier
Caldera rim
Boundary of Veiðivötn system
Fissures/faults
Laugahraun
Torfajökull is special because it is Iceland's largest rhyolitic centre and contains Iceland's largest geothermal field. Most volcanic centres contain a little bit of rhyolite, usually 10%. There are only two volcanic centres that have considerably more than 10%; Kerlingarfjöll has 25%, but Torfajökull is 80% rhyolite! Consequently Torfajökull accounts for about a third of Icelandic rhyolite. It is because of the rhyolite that Torfajökull has beautiful orange mountains (see Landmannalaugar and other pages). The large geothermal field means that there are many hot streams and pools in Torfajökull. There is one that you can bathe in at Landmannalaugar. There are other places where puddles boil and there are plenty of fumaroles (sulphurous steam vents) too. This creates some very atmospheric (and occasionally smelly) scenery.
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