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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
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.
Syðri Háganga and the river Kaldakvísl in the Highlands of Ic
Syðri Háganga and the river Kaldakvísl in the Highlands of Ic The Hágöngur high-temperature area in Central-Iceland is considered to represent one of the larger geothermal areas in Iceland
Lambaskarð pass in the Highlands of Iceland. At Dómadalsleið
Lambaskarð pass in the Highlands of Iceland. At Dómadalsleið Lambaskarð is a saddle within South Iceland and is nearby to Sauðleysur, Herbjarnarfell and Sátubarn. Lambaskarð has an elevation of 584 metres.
Gilsfjörður, Westfjords, Iceland.
Gilsfjörður, Westfjords, Iceland. Gilsfjörður, Westfjords, Iceland. Gilsfjörður is a fjord within Westfjords and is nearby to Nónsker, Króksfjarðarmúli and Garpsdalsfjall.
Cold day in the Highlands of Iceland
Cold day in the Highlands of Iceland Cold day in the Highlands of Iceland
Twilight in the Sprengisandur Highlands of Iceland
Twilight in the Sprengisandur Highlands of Iceland Sprengisandur is an ancient pass - during the time of the Icelandic Free State (ca. 930–1265) it was one of the several important north-south routes that connected remote regions of the island to the Plains of the Parliament, Þingvellir, where the yearly parliament, Alþingi, was held each year at midsummer. In the sagas of Icelanders it is often called simply Sandr "Sand" or Sandleið, "Sand trail". At its southern end, it was joined with another such route, Fjallabaksvegur nyrðri, running west from Landmannalaugar mountain hot springs area.
Road to Highlands of Gæsavötn in wintertime
Road to Highlands of Gæsavötn in wintertime Road to Gæsavötn, Highlands of Iceland in winter time