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  • Eldvörp Crades in winter

    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.
  • Eldvörp Crades in winter twilight

    Eldvörp Crades in winter twilight

    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 in winter

    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.
  • Driftwood in the bottom of Bitrufjörður. Westfjords - #Iceland

    Driftwood in the bottom of Bitrufjörður. Westfjords - #Iceland

    Bitrufjörður is in north-western Iceland, connected to the rest of Iceland by a 10 km wide isthmus between Gilsfjörður (Gilsfjordur) and Bitrufjörður (Bitrufjordur). Iceland's Western Fjords are very mountainous. The long, stunningly beautiful coastline – about half of Iceland’s total shoreline, is indented with dozens of fjords carved by intense glaciation. The shore is infinitely varied, changing with the seasons, lying on the mystical border between different worlds. Seals bask on the rocks, huge colonies of seabirds are seen and the king of the skies, the white-tailed eagle, watching over.
  • White frost on the moss - #Iceland.

    White frost on the moss - #Iceland.

    White frost is a solid deposition of ice which forms directly from water vapour contained in air. White frost forms when there is a relative humidity above 90% and a temperature below −8 °C (18 °F) and it grows against the wind direction, since air arriving from windward has a higher humidity than leeward air, but the wind must not be strong or it damages the delicate icy structures as they begin to form. White frost resembles a heavy coating of hoar frost with big, interlocking crystals, usually needle-shaped.
  • White frost on the moss - #Iceland.

    White frost on the moss - #Iceland.

    White frost is a solid deposition of ice which forms directly from water vapour contained in air. White frost forms when there is a relative humidity above 90% and a temperature below −8 °C (18 °F) and it grows against the wind direction, since air arriving from windward has a higher humidity than leeward air, but the wind must not be strong or it damages the delicate icy structures as they begin to form. White frost resembles a heavy coating of hoar frost with big, interlocking crystals, usually needle-shaped.
  • Keilir Volcano in the hoarfrost moss - #Iceland.

    Keilir Volcano in the hoarfrost moss - #Iceland.

    Keilir is a hyaloclastite mountain. It was created during subglacial eruptions during the ice age. It´s shape makes it distinctive and according to geologists, it probably is a crater plug. In spite of its steep slopes, it is not too difficult to climb, and the view from its top on a fine day is to be remembered. Keilir is the most distinctive landmark of Reykjanes and a symbol of the Reykjanes peninsula. On top of the mountain is a concrete table with a view direction map on a metal plate.
  • Aurora at Reykjanes Peninsula - Iceland

    Aurora at Reykjanes Peninsula - Iceland

    Snorrastaðatjarnir at Reykjanesskagi, Southwest Iceland. A popular recreational area. Pounds, rich of vegetation and important resting place for migration birds.
  • Moon Rays with Northern lights at Reykjanes Peninsula - #Iceland

    Moon Rays with Northern lights at Reykjanes Peninsula - #Iceland

    Snorrastaðatjarnir at Reykjanesskagi, Southwest Iceland. A popular recreational area. Pounds, rich of vegetation and important resting place for migration birds.
  • At Hengill Geaothermal area

    At Hengill Geaothermal area

    Hengill volcano is situated in the southwest of Iceland, to the south of Þingvellir. The volcano covers an area of about 100 km². The volcano is still active, evidenced by its numerous hot springs and fumaroles, but the last eruption occurred approximately 2,000 years ago.

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