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This is what the northernmost part of the fishing village might have looked like in Viking times

Hjartøy

19.05.2018 - 19:53

This little mountain in the picture sticks up because the layers are tilted on their sides.

Toftøyna

27.03.2019 - 15:07

Blomvågen 1851.

Blomvågen

07.12.2018 - 11:48

"One of the big scientific sensations", was the title in the Bergens Times newspaper on the 22nd of November, 1941. It was the geologist Isal Undås who had been interviewed by the newspaper. He thought that he had discovered a 120 000 year old whale bone, remains of life from before the last Ice Age.

Tveita

Tveitabotn

31.03.2018 - 19:25

Maters Fjord with Holmedalsberget in the background.

Holmedalsberget

19.06.2018 - 16:22

If you want to be on your own for a long day in a magnificent deciduous forest in demanding terrain, then HOLMESDALSBERGET is the right place. This is a big forested area by Matres Fjord in the southwestly part of Kinnherad. Here, we find one of the largest deciduous forests in Hordaland. The forest stretches over several kilometres.

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.

Skorpo (Svein Nord)

Skorpo

29.03.2018 - 11:25

Skorpo - Polished by glaciers and meltwater

From Ingahogg.

Ingahogg

20.12.2018 - 12:19

At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.

Langhaugane, Ulvanosa in the background.

Langhaugane

03.01.2019 - 16:52

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.

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