Goodbye Geiranger

Geiranger fjord, Norway

Twisted

Trollstigen mountain road, near Åndalsnes, in Romsdalen. Norway. The road twists through 11 hairpin bends as it climbs up to Stigrøra (858 metres above sea level). In some parts it's cut into the mountain and others are built on top of stone walls. An impressive bridge carries it across the Stigfossen waterfall.

The red cabin

Traditional norwegian red cabin by Oldevatnet Lake. Norway.

Grass roofs

Grass roof houses in the heart of the Norwegian Fjords, Lovatnet, Loen, Norway.

Ice abyss

Briksdalsbre Glacier, Norway.

Peaceful Olden

Olden, Norway.

Turquoise valley

Panoramic view of Kjenndal Valley, Norway. The beauty of this place hides the tragic history of Mount Ramnefjellet rock avalanches.

Turquoise mirror

Kjenndal Valley, Norway. The beauty of this place hides the tragic history of Mount Ramnefjellet rock avalanches. Much of the valley was devastated from two rockfall slides (one in 1905 and one in 1936) that created huge waves that swept with them most of the houses and vegetation.

From the fjord to the top

Loen from the top of Mt Hoven, Norway. The village of Loen is located in the inner part of the Nordfjord region and the lake Lovatnet is located just to the southeast of it.

Geirangerfjord views 3

Geiranger, Norway.

Geirangerfjord views 2

The impressive Geirangerfjord from Dalsnibba, Norway.

Geirangerfjord views 1

The deep blue waters of Geirangerfjord. View from Dalsnibba. Norway.

Arctic dream

Panoramic view of Reine, Lofoten Islands, Norway.

Arctic village

Winter evening in Horn, Lofoten.

The photographer

A photographer contemplating the landscape in Skagsanden beach, Lofoten, Norway.

Arctic green dream

Northern lights over Reine, Lofoten Islands, Norway.

51/52 - Green Explosion

Aurora at Uttakleiv Beach, Lofoten, Norway. An aurora, also known as polar lights or northern lights, is a natural light display in the sky, predominantly seen in the Arctic and Antarctic regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere, where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity.

Aurora Mirror 2

Aurora Borealis at Skagsanden beach, Lofoten Island, Norway. An aurora, also known as polar lights or northern lights, is a natural light display in the sky, predominantly seen in the Arctic and Antarctic regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere, where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity.

Arctic night 2

Aurora at Uttakleiv Beach, Lofoten, Norway.

Aurora Mirror

Aurora Borealis at Skagsanden beach, Lofoten Island, Norway. An aurora, also known as polar lights or northern lights, is a natural light display in the sky, predominantly seen in the Arctic and Antarctic regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere, where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity.

52/52 - The Moon and the Aurora

Aurora Borealis at Skagsanden beach, Lofoten Island, Norway.

Dreamy Aurora

Aurora Borealis at Skagsanden beach, Lofoten Island, Norway.

Arctic night

Aurora at Uttakleiv Beach, Lofoten, Norway. An aurora, also known as polar lights or northern lights, is a natural light display in the sky, predominantly seen in the Arctic and Antarctic regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere, where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity.