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Moss (6)

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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.
South shore
South shore Moss on the South shore Iceland
South shore
South shore Moss on the South shore Iceland
The green moss in Iceland
The green moss in Iceland Picture from Þakgil. Up in the mountayns you will find this green moss