Your Shopping Cart is empty.
Search
All files
Category
K - Ö Geothermal
Keywords
Photo
Advanced search
Photo Filters
Categories

K - Ö Geothermal (172)

 Flow
 Auto paging
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).
Laugafell geothermal oases hot pool
Laugafell geothermal oases hot pool The Laugafell geothermal pool is located on the northwestern slopes of Laugafell Mountain. The area is an oasis in the barren land between Hofsjökull Glacier and Vatnajökull Glacier. The Laugafell pool is rather large and measures around 17×7 meters in diameter and from 0.5-1.5 meters in depth. The temperature in the pool is pretty consistent at around 36 °C and 50-70 people can bathe in the pool simultaneously. Just above the main pool you will find a very small pool that can only fit one person at a time. The small pool is called Þórunnarlaug, or Thorunn’s pool.
One of the Hidden Waterfall at Landmannalaugar Highlands
One of the Hidden Waterfall at 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. All the #PHOTOS you need from #Iceland More than 8.000 #Professional high resolution photos http://www.icestockphotos.com
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.
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