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Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018

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.

Fjelberg

Fjelberg

19.06.2018

The beautiful vicarage on the Fjelberg Island lies a few minutes walk up from the fjord, in a compact enclosure with the church south of the main building and the bishop’s residence to the north; a rare harmonic cluster.

Gildrehola

Gildrehola

12.03.2018

Halsnøy

Halsnøy

19.12.2018

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.

Kvinnherad Church

Kvinnherad Church

19.06.2018

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

Skålafjøro

Skålafjøro

21.11.2018

Skorpo (Svein Nord)

Skorpo

29.03.2018

Skorpo - Polished by glaciers and meltwater

Sunde, Kvinnherad

Sunde

19.06.2018

In 1852 Haktor Thorsen erected two large warehouses on one of his farms in Sunde and started trading and salting herring. This was the start of an industrial adventure that made Sunde into one of the first industrial communities in Kvinnherad.

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019

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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