The highway back to Selfoss village
The landscape around the Hekla volcano
Going close to the Hekla volcano
Sleeping Hekla volcano
Driving along endless lava fields
The highway no. 1 passing the Hoffellsjökull glaci…
Svínafellsjökull Glacier Tongue
Natural ice sculptures in foreground
More ice pieces on the Jökulsárlón beach
Natural ice sculpture on the black beach of Jökuls…
Ice rocks on the black beach
Tour amphibian vehicles for a Jökulsárlón excursio…
Walk along the Vatnajökull glacier
Vatnajökull Icecap
Höfn
Vatnajökull Icecap, the view from Höfn
The harbour in Höfn
The harbour in Höfn
Graffiti painting on a house wall in Reykjavik
The Hekla volcano and its eruption history
Climbing on the lava hills
Beside the highway no. 1
Svartifoss (The Black Waterfall)
The Old Harbour of Reykjavik
Reykjavik skyline under heavy weather
Minke whale shows its backside
On the way to the Blue Lagoon
The Blue Lagoon
The Blue Lagoon outside
A walk in the Skaftafell nationalpark
Glacial lake in Skaftafell
Glacial branch of the Glacier Vatnajokull
Lakes from the Svinafellsjökull glacier
The Svinafellsjökull glacier
The run-out of the Svinafellsjökull glacier
Svinafellsjökull lakes
Way to the Svinafellsjökull glacier
The view to the Svinafellsjökull glacier
Two German youngsters missing since one year
The Skeiðará river flows into a glacial lake
The Skeiðará river at the end of the Svinafellsjök…
Coming closer to the Svinafellsjökull glacier
The glacier and the river end in the lake
The big glacial lake
Heavy weather clouds came on the way back
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Hot springs near Reykjavik
Hot springs are found all over Iceland, but they are rare in the eastern basalt area. There are about 250 low-temperature geothermal areas with a total of about 800 hot springs. The average temperature of their water is 75° Celsius. The largest hot spring in Iceland, Deildartunguhver, has a flow of 150 liters of boiling water per second. Some of the hot springs are spouting springs or geysers. Springs charged with carbon dioxide are to be found in some districts, mainly in Snaefellsnes, but have not yet been utilized. Since the last Hekla eruption, springs rising from under the new lava have also been found to be charged with carbon dioxide.
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