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K - Ö Geothermal (180)

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Kerlingarfjöll, Geothermal area in the highlands
Kerlingarfjöll, Geothermal area in the highlands Kerlingarfjöll (1,477 m (4,846 ft)) is a mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area. And indeed, they are part of a large volcano system of 100km² (38.6 square mile). The volcanoes of the range are tuyas. The earth is shimmering red in this area because of the volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.
Sogaselsdalur in the mountain of Reykjanes
Sogaselsdalur in the mountain of Reykjanes Sogaselsdalur in the mountains of Reykjanes is an old almost cooled down geothermal valley where you still can see all the clay on the hill side. It’s not recommended to walk in the valley itself as the clay gets stuck under your sole. This is a beautiful hidden Gem. Reykjanes. Iceland
Kerlingarfjöll, Geothermal area in the highlands
Kerlingarfjöll, Geothermal area in the highlands Kerlingarfjöll (1,477 m (4,846 ft)) is a mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area. And indeed, they are part of a large volcano system of 100km² (38.6 square mile). The volcanoes of the range are tuyas. The earth is shimmering red in this area because of the volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.
Kerlingarfjöll, Geothermal area in the highlands
Kerlingarfjöll, Geothermal area in the highlands Kerlingarfjöll (1,477 m (4,846 ft)) is a mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area. And indeed, they are part of a large volcano system of 100km² (38.6 square mile). The volcanoes of the range are tuyas. The earth is shimmering red in this area because of the volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.
Stórihver, Engjahver or Austurengjaver in Reykjanes Peninsula.
Stórihver, Engjahver or Austurengjaver in Reykjanes Peninsula. The thermal area of Austurengjar extends from east of Lake Grænavatn to Lake Kleifarvatn in the north. Hot springs, mud pots, and fumaroles are scattered sparsely over the area. The largest and most powerful hot spring, called Austurengjahver, Engjahver, or Stórihver, is located east of Lake Grænavatn in about 1,6 km walk from the parking lot where a sign leads you on to the right trail.
Stórihver, Engjahver or Austurengjaver in Reykjanes Peninsula.
Stórihver, Engjahver or Austurengjaver in Reykjanes Peninsula. The thermal area of Austurengjar extends from east of Lake Grænavatn to Lake Kleifarvatn in the north. Hot springs, mud pots, and fumaroles are scattered sparsely over the area. The largest and most powerful hot spring, called Austurengjahver, Engjahver, or Stórihver, is located east of Lake Grænavatn in about 1,6 km walk from the parking lot where a sign leads you on to the right trail.
The Veins of Landmannalaugar Highlands
The Veins of Landmannalaugar Highlands Landmannalaugar is a place in the Fjallabak Nature Reserve in the Highlands of Iceland. It is at the edge of Laugahraun lava field, which was formed in an eruption around the year 1477. It is known for its natural geothermal hot springs and surrounding landscape.
Landmannalaugar Highlands
Landmannalaugar Highlands Landmannalaugar is a place in the Fjallabak Nature Reserve in the Highlands of Iceland. It is at the edge of Laugahraun lava field, which was formed in an eruption around the year 1477. It is known for its natural geothermal hot springs and surrounding landscape
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.