• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Fjelberg

Fjelberg

19.06.2018 - 16:10

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.

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.

Ænes, Kvinnherad

Ænes

19.06.2018 - 16:11

Ænes has been one of the prosperous farms at the Mauranger Fjord in medieval times. At the time of Harald Gilles, around 1130, we hear of GAUT at Ænes. The noble families around the Hardanger Fjord were prominent in the political sphere from early on, and it is obvious that the fine and openly situated farm at Ænes was also a good place for a Church.

Nils Hertzber’s watercolour from 1829 gives us an impression of the burial site with the menhirs at Årbakkesanden.

Årbakka- The prehistoric site

19.06.2018 - 17:47

The prehistoric site at Årbakkasanden with menhirs and burial mounds has been visited, described and illustrated by many learned researchers through the last 350 years. All the same, we still know very little of this unique cultural monument.

Gildrehola

Gildrehola

12.03.2018 - 12:53

Seim

19.06.2018 - 16:23

Skorpo (Svein Nord)

Skorpo

29.03.2018 - 11:25

Skorpo - Polished by glaciers and meltwater

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.

Espevik

Espevik

03.01.2019 - 15:26

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

The walls in the boathouse in Hopssundet are built of red granite from Reksteren.

Hopssundet

01.05.2018 - 16:39

Pages