• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Sculptures in the bedrock

Herand- geologi

11.12.2018 - 14:12

Hereiane. Jonahornet in the background.

Hereiane

26.05.2018 - 16:24

At Hereiane on warm summer days one you can walk barefoot up the hill from the fjord all the way up to 400 metres elevation. The naked, furrowed bedrock often causes travellers who see it from the north side of the fjord to wonder. Why does it look like this, and why is there so little that grows here? It is a long way to the heavy metal industry in Ålvik and Odda, and there hasn’t been a forest fire in modern times.

Indre Vikane

Indre Vikane

26.05.2018 - 16:24

The boathouses at Svåsand.

Svåsand

26.05.2018 - 16:28

Down by the fjord at Svåsand, close to the main highway, there is a long row of boathouses, one of the well-preserved, older boathouse locations along the Hardanger fjord. It is the farms at Svåsand that have their boathouses here, four main farms with origins far back in time.

Halnelægeret.

Halne

26.05.2018 - 11:25

At Halnefjorden, a few hundred metres east of Halne mountain lodge, lie the remains of two stone sheds – Halnelægeret. Some generations ago the cattle drovers stopped here in the summer; they were the cowboys of their time. But Halnelægeret already had a long history before the cattle drovers came.

Skytjedalen in Eidfjord.

Skytjedalen

03.01.2019 - 14:57

Støle church

Støle church

18.06.2018 - 20:27

The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.

Lyse Monastery, reconstruction

Lyse Monastery

16.06.2018 - 15:56

Varghola

Vargavågen

13.03.2018 - 21:35

Geologist William Helland-Hansen examining a quartz conglomerate in the Ulven Syncline on one of the hills by the north west end of Lake Ulvenvatnet.

Ulven

03.01.2019 - 15:16

In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.

Pages