• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018 - 14:03

Hammarsland, Fusa

Hammarsland

30.03.2018 - 08:42

Mjånes, Fusa

Mjånes

16.06.2018 - 14:06

The Hellands scree

Møshovd

06.12.2018 - 10:30

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Gamalt postopneri, Øpstad i Fusa

Øpstad

16.06.2018 - 14:10

The post house at Øpstad stands out in the landscape. An ochre yellow house with a loft and a white-painted house in Swiss style with ochre edgings, bears witness to a well preserved house from the 1800s, nearest neighbour to the beautiful old vicarage. In the Øpstad hamlet there was a post office for more than a hundred years, until the 1970s. Today it is possible to walk the old post road across the mountain to Strandvik, as part of “Den Stavangerske Postvei” (The post road to Stavanger).

The oldest farmyard at Fryste or Frøystein.

Frøystein

27.05.2018 - 15:48

The farm Frøystein by the Ulvik fjord is commonly called Fryste. In 1614 the name was written Frøstemb – an obvious Danish influence – and the form Frøsten was used up until the land register in 1886 and 1907. It is probable that the name of the farm originally was Frystvin; a vin-name. Thus it has no connection with neither Frøy (Norse fertility god) nor stein (stone).

Glacial river plain at Lake Klevavatnet.

Rallarvegen

04.12.2018 - 14:30

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

On the trail toward Kyrkjedøri, a half hour walk from Finse station, we find these small ridges

Trail toward Kyrkjedøri

04.12.2018 - 15:04

Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.

Pages