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Torfajökull 

The map below is interactive; click on text in purple for more information.

 

Note, more text will be become purple as my website grows, so watch this space!

Angel Peak

NW Rauðfossafjöll

SE Rauðfossafjöll

Námshraun

Hrafntinnusker 

Dalakvísl 

Subglacial Torfajökull eruptions

Ring fracture rhyolites

Older rhyolites

Edifices relating to my PhD

 

Postglacial Torfajökull eruptions

Rhyolite

Tholeiite

Mixed rhyolite-tholeiite

Alkali basalt

 

Other features

Torfajökull glacier

Caldera rim

Boundary of Veiðivötn system

Fissures/faults

Landmannalaugar campsite

 

 

 

 

 

 

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. 

 

 

If you have any comments or questions, please post them on the bottom of the page or contact me

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