• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

The bridge at Mørkhølen

Mørkhølen

13.12.2018 - 08:48

Tysse

Tysse

18.03.2018 - 08:08

As early as 1862 Svein L.Røsseland started a country store and lodging house at Ytre Tysse, and later on he became steamship agent and the first post office manager in Samnanger. However, the decisive change came when F.Mathiessen started A/S Samnanger Uldvarfabrik (woollen factory) in 1886.

Goltasund bridge and Goltasundet

Goltasundet

16.06.2018 - 17:34

For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.

The Salting shed at Trælevika.

Trellevik

16.06.2018 - 17:35

St. Ludvig.

Tyssøy

16.06.2018 - 17:36

B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.

Boathouses in Breiviksunde

Breiviksundet

24.06.2018 - 15:33

Ulevn Camp around 1915.

Ulven camp

16.06.2018 - 16:03

Varghola

Vargavågen

13.03.2018 - 21:35

Lysekloster

Lysekloster- Mushroom flora

05.12.2018 - 08:05

The area around Lysekloster is one of the most popular places in Hordaland for picking mushrooms. The large variety of mushrooms probably stems from the varied, old, cultural landscape which has a lot of open grazing areas and several types of fir- and deciduous forests.

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