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Landscape (2035)

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The rig at the top of Hellutindar Mountain with a view to Kleifa
The rig at the top of Hellutindar Mountain with a view to Kleifa Sveifluháls or Austurháls is 395 m high palagonite rigg in Reykjanesfjallgarð, west of Kleifarvatn. Steep hammers are down to Kleifarvatn. On the south and east site of the neck are high geothermal areas mainly at Krísuvík. The highest peaks at Sveifluháls are Hellutindar, Stapatindar og Miðdegishnúkar.
On the top of Sólheimajökull Glacier
On the top of Sólheimajökull Glacier The glacier snout Solheimajokull is the southwestern outlet of the Myrdalsjokull icecap. It is about 8 km long and 1-2 km wide. River Jokulsa discharges it, and is sometimes called “The Stinking River” because of its emission of sulphuric acid from sub-glacial high temperature areas. The glacier advanced about 900 metres during the last few centuries, but retreated greatly from 1930 to 1964. In the nineties it advanced and almost managed to cover the Jokulhaus hill
Hlíðarvatn in Ice and snow
Hlíðarvatn in Ice and snow Hliðarvatn is a good fishing lake on the Reykjanes Peninsula
Hlíðarvatn in Ice and snow
Hlíðarvatn in Ice and snow Hliðarvatn is a good fishing lake on the Reykjanes Peninsula
Near Seltún at Krísuvík. Geothermal Area - Steaming hot river
Near Seltún at Krísuvík. Geothermal Area - Steaming hot river The geothermal area Krýsuvík is situated on the Reykjanes peninsula in Iceland. It is in the south of Reykjanes in the middle of the fissurezone on the Mid-Atlantic Ridge which traverses Iceland Krýsuvík consists of several geothermal fields, such as Seltún. Here solfataras, fumaroles, mud pots and hot springs have formed, the soil is coloured. Sulphuric water and gases have created colorful deposits, the soil is colored in green, yellow and red colors. Visitors can wonder at hissing solfataras, fumaroles and boiling mud pots, where the soil is mixed with acid. . Sulphur deposits were mined in 1722 – 1728 and in the 19th century.
Seltún at Krísuvík. Geothermal Area - Steaming hot springs in
Seltún at Krísuvík. Geothermal Area - Steaming hot springs in The geothermal area Krýsuvík is situated on the Reykjanes peninsula in Iceland. It is in the south of Reykjanes in the middle of the fissurezone on the Mid-Atlantic Ridge which traverses Iceland Krýsuvík consists of several geothermal fields, such as Seltún. Here solfataras, fumaroles, mud pots and hot springs have formed, the soil is coloured. Sulphuric water and gases have created colorful deposits, the soil is colored in green, yellow and red colors. Visitors can wonder at hissing solfataras, fumaroles and boiling mud pots, where the soil is mixed with acid. . Sulphur deposits were mined in 1722 – 1728 and in the 19th century.
Seltún at Krísuvík. Geothermal Area - Beautiful, Steamy Smell
Seltún at Krísuvík. Geothermal Area - Beautiful, Steamy Smell The geothermal area Krýsuvík is situated on the Reykjanes peninsula in Iceland. It is in the south of Reykjanes in the middle of the fissurezone on the Mid-Atlantic Ridge which traverses Iceland Krýsuvík consists of several geothermal fields, such as Seltún. Here solfataras, fumaroles, mud pots and hot springs have formed, the soil is coloured. Sulphuric water and gases have created colorful deposits, the soil is colored in green, yellow and red colors. Visitors can wonder at hissing solfataras, fumaroles and boiling mud pots, where the soil is mixed with acid. . Sulphur deposits were mined in 1722 – 1728 and in the 19th century.
Fjallabak nyrðri. Reserve region in the Highlands of Iceland
Fjallabak nyrðri. Reserve region in the Highlands of Iceland Fjallabak Nature Reserve was established in 1979. The Nature reserve is 47.000 hectares and is over 500 meters above see level. The land is mountainous, sculptured by volcanoes and geothermal activity, covered by lavas, sands, rivers and lakes. The Fjallabak region takes its name from the numerous wild and rugged mountains with deeply incised valleys, which are found there. The topography of the Torfajokull, central volcano found within the Fjallabak Nature Reserve, is a direct result of the region being the largest rhyolite area in Iceland and the largest geothermal area (after Grimsvotn in Vatnajokull).
Hellutindar at Sveifluháls with a view over Kleifarvatn Lake
Hellutindar at Sveifluháls with a view over Kleifarvatn Lake Sveifluháls or Austurháls is 395 m high palagonite rigg in Reykjanesfjallgarð, west of Kleifarvatn. Steep hammers are down to Kleifarvatn. On the south and east site of the neck are high geothermal areas mainly at Krísuvík. The highest peaks at Sveifluháls are Hellutindar, Stapatindar og Miðdegishnúkar.
Two palagonite stones and Hellutindar Mountain in the background
Two palagonite stones and Hellutindar Mountain in the background Sveifluháls or Austurháls is 395 m high palagonite rigg in Reykjanesfjallgarð, west of Kleifarvatn. Steep hammers are down to Kleifarvatn. On the south and east site of the neck are high geothermal areas mainly at Krísuvík. The highest peaks at Sveifluháls are Hellutindar, Stapatindar og Miðdegishnúkar.