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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.

Stained glass painting in “Målabuo”.

Gjerde

19.06.2018 - 16:19

The Halsnøy Boat

19.06.2018 - 16:25

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.

The circular buckle from Hatteberg, Kvinnherad

Hatteberg

13.03.2018 - 20:51

Chest from Huglo, painted in 1820 by Gunder Gundersen Handeland

Skorven

19.06.2018 - 16:17

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

Geithidleren, Årsand, Kvinnherad

Årsand

19.06.2018 - 16:10

Below a south facing, steep rock at Årsand, there is one of the strangest ancient relics in the whole of Hordaland. The jutting rock wall forms a shallow flagstone – Geithilderen. Parts of the rock wall are covered by a light lime crust and on the crust figures have been painted in golden and rusty red colours.

Fra Blåmanen mot Vardegga og Ulriken.

Vidden

07.12.2018 - 14:19

Langavatnet, Åsane (Svein Nord)

Åsane

05.12.2018 - 18:44

Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.

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