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Eldvörp (14)

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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.
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.
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.
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.
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.
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.
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.
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.