• 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.

Etne and the Etne delta around 1900.

Etnedeltaet

18.06.2018 - 20:23

During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.

Langfoss (Alf Adriansen)

Langfoss

29.03.2018 - 11:48

Boat engines, Norwegian Engine Museum in Skånevik

Skånevik- Norwegian engine museum

25.04.2018 - 21:25

Fykse

Fykse

29.03.2018 - 11:55

«Gygraræve»

Fyksesundet

29.03.2018 - 11:55

Rockslide at Mundheim in the spring of 1997

Mundheim

26.05.2018 - 16:36

At Mundheim there is a dangerous stretch of the highway. The mountainside has given way several times in this area. Typically, it happens in the spring, when the frost has loosened its grip.

Rindarne moraine

29.03.2018 - 11:56

Boys fishing from the river at Steinsdalsfossen

Steinsdalsfossen

29.03.2018 - 11:56

Øvsthusfossen, or Steinsdalsfossen waterfall, as it is called today, attracts tourists by the thousands, and always has done as long as there have been tourists in Norway, since the early 1800s.

The waterfall at the top of Tokagjelet

Tokagjelet

03.12.2018 - 09:55

There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.

Pages