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Sky Lagoon

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Sky Lagoon is a geothermal spa in southwestern Iceland . It is located at Kársnes Harbour, Kópavogur ,

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12-494: Sky Lagoon is primarily heated by geothermal energy. Natural hot water that comes from a great depth below the Earth's surface feeds the geothermal pool. which keeps the water temperature at approximately 38 to 40 °C (100 to 104 °F). Snæfellsjökull (a glacier-capped volcano) and Keilir mountain are visible from Sky Lagoon. The spa is a competitor of the nearby Blue Lagoon . Construction of Sky Lagoon began in early 2020 and

24-504: A Czechoslovak-Icelandic science party discovers an ancient alien outpost in the cave system under Snæfellsjökull. It also figures prominently in the novel Under the Glacier (1968) by Icelandic Nobel laureate Halldór Laxness . Snæfellsjökull is the setting and subject of "Lava and Ice" (episode 2) of Wireless Nights , Jarvis Cocker 's BBC Radio 4 and podcast series. The campaign "Snæfellsjökul fyrir forseta" proposed Snæfellsjökul as

36-523: Is a 700,000-year-old glacier -capped stratovolcano in western Iceland. It is situated on the westernmost part of the Snæfellsnes peninsula. Sometimes it may be seen from the city of Reykjavík over Faxa Bay , at a distance of 120 km (75 mi). The mountain is one of the most famous sites of Iceland, primarily due to the novel Journey to the Center of the Earth ( 1864 ) by Jules Verne , in which

48-531: Is also associated with a fissure field that last erupted to the west forming the Væjuhraun lava flow as already mentioned. To the east of Snæfellsjökull this fissure field last erupted between 5 and 8 thousand years ago. This eruption formed the 18 km (6.9 sq mi) Búðahraun lava field from the crater Búðaklettur, south-west of Búðir . This is part of the Snæfellsjökull volcanic system which in turn

60-517: Is part of the Snæfellsnes volcanic belt (Snæfellsnes volcanic zone). This is an area of renewed intra-plate volcanism in the North American Plate, with rocks no older locally than 800,000 years, that overlay an extinct rift zone that produced the more than 5 million years old crustal basement tholeiitic flood basalts of the Snæfellsnes peninsula. The Snæfellsjökull volcanic system has

72-515: The last central volcano eruption. This main eruption had been explosive and originated from the summit crater. It is dated to about 200  CE, and was also associated with the eruption of viscous lava that covered 30 km (12 sq mi). In all three large, perhaps up to VEI 4 plinian rhyolitic eruptions have occurred during the Holocene producing tephra . These occurred about 1800, 4000 and 8500 years ago. Snæfellsjökull

84-408: The potential for lava flows, explosive tephra eruptions (e.g. air traffic during a major rhyolitic eruption), tsunami generation (perhaps one flank collapse has occurred historically) and Jökulhlaups . In summer, the saddle near the summit can be reached easily by walking, although the glacier's crevasses must be avoided. Several tour companies run regular guided walks during the season. Reaching

96-576: The protagonists find the entrance to a passage leading to the center of the Earth on Snæfellsjökull. The mountain is part of Snæfellsjökull National Park (Icelandic: Þjóðgarðurinn Snæfellsjökull ). Snæfellsjökull was visible from an extreme distance due to an arctic mirage on 17 July 1939. Captain Robert Bartlett of the Effie M. Morrissey sighted Snæfellsjökull from a position some 536 to 560 kilometres (289–302 nmi) distant. In August 2012,

108-457: The summit crater and have produced felsic material, with pumice from the two most recent major eruptions being alkaline trachyte trending in composition close to rhyolite . Lower-flank craters have produced basaltic lava flows with classic basalt composition. The latest flank eruption was of 0.11 km (0.0264 cu mi) of basaltic material in the 4.5 km (1.7 sq mi) Væjuhraun lava flow and occurred shortly after

120-495: The summit was ice-free for the first time in recorded history . The icecap area had been 16 km (6.2 sq mi) in 1946, 14 km (5.4 sq mi) in 1999 reducing to 10–11 km (3.9–4.2 sq mi) in 2008. The stratovolcano , which is the only large central volcano in its part of Iceland, has many pyroclastic cones on its flanks. Upper-flank craters produced intermediate to felsic materials. Several holocene eruptions have originated from

132-455: The true summit requires technical ice climbing. Snæfellsjökull serves as the entrance to the subterranean journey in Jules Verne 's classic science fiction novel, Journey to the Center of the Earth (1864). It is also featured in the 1960s Blind Birds trilogy by Czech SF writer Ludvík Souček , loosely inspired by Verne's work. While trying to discern whether Verne actually visited Iceland,

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144-591: Was completed in 2021. The design was inspired by the Icelandic geography and uses grey-blues, deep greens, whites and creams to copy the landscape. Some elements of Sky Lagoon were inspired by Icelandic nature and heritage, such as the turfhouse, turf walls and plunge pool. Elements of the facility include a cave tunnel entrance to a hot springs soaking pool and a cold plunge. Sn%C3%A6fellsj%C3%B6kull Snæfellsjökull ( Icelandic pronunciation: [ˈs(t)naiːˌfɛlsˌjœːkʏtl̥] , snow- fell glacier )

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