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Eldvörp Crades
Eldvörp Crades Eldvörp is a row of scoria and spatter cones formed in the Reykjanes Fires 1210-1240 AD in the Svartsengi volcanic system. The craters lie in a NE-SW trending row, extending from the south coast about 10 km inland, with the north end 2 km west of the Blue Lagoon. The lava emitted from the crater row is one of the most voluminous Holocene lava flows on the Reykjanes Peninsula, covering c. 20 km2.
Blue Lagoon Spa
Blue Lagoon Spa Blue Lagoon Spa - Reykjanes - Iceland
View over Sveifluháls rig, Arnarvatn and Kleifarvatn Lakes with
View over Sveifluháls rig, Arnarvatn and Kleifarvatn Lakes with View over Sveifluháls rig, Arnarvatn and Kleifarvatn Lakes with Miðdegishnjúk mountain in the middle, Reykjanes, South West Iceland.
Eldvörp - Still hot after more than 800 years
Eldvörp - Still hot after more than 800 years Eldvörp is a row of scoria and spatter cones formed in the Reykjanes Fires 1210-1240 AD in the Svartsengi volcanic system. The craters lie in a NE-SW trending row, extending from the south coast about 10 km inland, with the north end 2 km west of the Blue Lagoon. The lava emitted from the crater row is one of the most voluminous Holocene lava flows on the Reykjanes Peninsula, covering c. 20 km2.
Eldvörp - Still hot after more than 800 years
Eldvörp - Still hot after more than 800 years Eldvörp is a row of scoria and spatter cones formed in the Reykjanes Fires 1210-1240 AD in the Svartsengi volcanic system. The craters lie in a NE-SW trending row, extending from the south coast about 10 km inland, with the north end 2 km west of the Blue Lagoon. The lava emitted from the crater row is one of the most voluminous Holocene lava flows on the Reykjanes Peninsula, covering c. 20 km2.
Eldvörp craters - Still hot after 800 years
Eldvörp craters - Still hot after 800 years Eldvörp is a row of scoria and spatter cones formed in the Reykjanes Fires 1210-1240 AD in the Svartsengi volcanic system. The craters lie in a NE-SW trending row, extending from the south coast about 10 km inland, with the north end 2 km west of the Blue Lagoon. The lava emitted from the crater row is one of the most voluminous Holocene lava flows on the Reykjanes Peninsula, covering c. 20 km2.
Northern lights over Gerðistangaviti lighthouse
Northern lights over Gerðistangaviti lighthouse Northern lights over Gerðistangaviti lighthouse. Reykjanes. Iceland
Northern lights over Gerðistangaviti lighthouse
Northern lights over Gerðistangaviti lighthouse Northern lights over Gerðistangaviti lighthouse. Reykjanes. Iceland
Bessastaðir. The official residence of the President of Iceland
Bessastaðir. The official residence of the President of Iceland After the slaying of Snorri Sturluson in September 1241, Bessastaðir was claimed by the King of Norway. Thereafter it became a Royal stronghold and the dwellings of the King's highest-ranking officers and officials in Iceland. It resisted an attack by Turkish slave raiders in July 1627. In the late 18th century Bessastaðir was changed into a school for a few years and until 1944 when it was donated to the President it was a common farm. The location is named after Sigurður Jónasson Bessastaðir who bought the estate in 1940 and donated it in 1941.
Stóriburkni - Dryopteris filix-mas
Stóriburkni - Dryopteris filix-mas Eldvorp is a 10 km long crater row to the northwest of Grindavik. It has several big craters with extensive thermal activity within and outside one of them, where a great deal of steam of about 280°C escapes. In older days, women from Grindavík baked bread in the warm steam and took the trail called "Brauðstígur" or Breadtrail up there from Grindavík.