• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Langfoss (Alf Adriansen)

Langfoss

29.03.2018 - 11:48

Botnavatnet

Botnavatnet

29.03.2018 - 12:00

Today there are only a few farmers that grow potatoes in Fitjar.

Fitjar- potatoes

19.12.2018 - 18:18

The deep agricultural soils in Fitjar are found especially in the area between Lake Storavatnet and Breivika. The many stonewalls in the area reflect that the earth probably was full of stones and stone blocks. The stones that couldn't be dug out had also a function: they stored heat that helped to grow potatoes.

From Grønafjellet toward Kattnakken.

Grønafjellet

19.06.2018 - 16:06

Mountain plants with their beautiful, colourful flowers are common in high altitude areas in Norway. On the coast there are not so many of them. But, here and there one nonetheless finds mountain plants, and this makes some coastal mountainsides a little bit different. Perhaps the growth on these mountainsides gives us a little glimpse of a distant past?

Smedholmen, Fitjar

Smedholmen

30.03.2018 - 20:10

From Helland toward the end of the valley with the Skrikjo waterfall.

Opedal

03.12.2018 - 13:53

Ullensvang

Ullensvang church

27.05.2018 - 15:28

Ullensvang church, situated beside the vicarage, in idyllic surroundings on the headland just inside Lofthus municipality, is mentioned for the first time in written sources in 1309. At that time the present Gothic stone church must have been new. Judging by the style in the western portal and the eastern chancel windows, the church must have been built around 1300 or just before, probably by builders from Bergen influenced by the English Gothic style.

From Kinsekvelven river toward Lakes Kinsevatnet and Veivatnet.

Veivatnet

27.05.2018 - 15:29

From Kinsekvelven river and inward to Lake Veivatnet, we can wander through one of Hardangervidda's many fertile areas. A number of finicky plants grow here, and there are plenty of birds and fish. We can thank a lime rich soil for the diversity.

Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.

Skånevik- moraine

06.03.2019 - 14:58

In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.

Pages