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Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018 - 19:25

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Halsnøy

Halsnøy

19.12.2018 - 21:15

Hadde ikkje Hardangerfjordbreen mot slutten av istida rykt fram over fjordbotnen, ville Halsnøy ikkje eksistert som éi øy, men som mange småøyar. Breen skuva framfor seg så mykje leire frå havbotnen at Brattåsen, Toftåsen, Landåsen og Svartaberg vart samla i eitt landområde.

Elias Fiigenschoug’s painting of Halsnøy monastery , 1656

Halsnøy Monastery

19.06.2018 - 16:12

Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.

Kvinnherad Church

Kvinnherad Church

19.06.2018 - 16:12

The stately Kvinnherad Church with its characteristic profile set out against the mighty Malmangernuten in the background, gives you a rare feeling of being present in a historic landscape as you come around Nes and face the well-kept houses at the Skåla farm. The church at Skåla is one of four “fjordungskirker” (one of four main district churches) and this farm was the centre of this coastal administration district.

Langhaugane, Ulvanosa in the background.

Langhaugane

03.01.2019 - 16:52

Skorpo (Svein Nord)

Skorpo

29.03.2018 - 11:25

Skorpo - Polished by glaciers and meltwater

Ølve

Ølve

04.01.2019 - 15:57

Ølve has a special soil type. Here one finds an extra hard clay soil. This is especially noticed by those who work with excavating for building foundations and the like. Often it is necessary to use especially big digging machines and sometimes even dynamite in order to break up the compact masses. The reason for this is the growth of the glaciers toward the end of the Ice Age: The clay, that was first deposited in front of the glacier, came under great pressure when the glacier later grew and slid out over the clay.

Detail from smokehouse, Arnatveit, Bergen

Arnatveit

12.06.2018 - 19:24

On the farm of Arnatveit, high up on the slope above the highway, an old smokehouse remains standing in the courtyard of the main farm property, in the place of the old common courtyard. Today this farm lies at the outskirts of a large housing estate. Most of the farmland of the other farm properties has been sold to benefit the city’s need of sites for the new community of Arna.

Bryggen

Bryggen

26.09.2018 - 19:14

In the 1300s Bergen was a trading centre of European dimension. The town is thought to have had around 7000 inhabitants and was the largest and most important in the country. In a European context it was an average size town. At this time the most tightly built town area was still mostly east of Vågen from Holmen in the north to Vågsbotn in the south. Already in medieval times, latest in the 1340s, this area was called Bryggen.

Domkirken

Domkirken

12.06.2018 - 19:08

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