Rafn Sig,-
Eldvörp Crades in winter
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.
Discover Wild Iceland offers wide variety of exciting and private day tours, photo tours, Photo workshop tours and Wedding Photography tours - all year round.
All our tours are operated by highly experienced guides and professional photographers.
Eldvörp Crades in winter
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.
Discover Wild Iceland offers wide variety of exciting and private day tours, photo tours, Photo workshop tours and Wedding Photography tours - all year round.
All our tours are operated by highly experienced guides and professional photographers.