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Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018 - 14:03

Holdhus church, Fusa

Holdhus church

16.06.2018 - 14:04

The old church at Holdhus is one of the oldest timbered churches left in the west of Norway. The new church at Eide, built in 1889, replaced the church location from the Middle Ages. As the small, tarred church lies today, in the hilly landscape at Holdhus, it was taken over by the Society for the Preservation of Norwegian Ancient Monuments, who obtained title to the property in 1900 from Hans Holdhus.

The man from Holmefjord

Holmefjord

06.12.2018 - 16:28

Even though we know of several hundred burial places from the Stone Age in Hordaland, we do not often hit on the Stone Age Man himself. But there are a few.

Hopslia

Hopslia

16.06.2018 - 14:05

Some of the giant trees in Hopslia north of Holme Fjord are as much as thirty metres high. Elm and ash are the most common, basswood somewhat rarer. Relatively soft bedrock, good growing conditions and enough light, help them to thrive just here.

The Hellands scree

Møshovd

06.12.2018 - 10:30

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

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.

Rembesdalsskåka and the lower part of Demmevatnet, from Tresnuten. Demmevass cabin is visible to the left in the picture.

Simadalen

29.11.2018 - 16:02

On the 10th of August, 1937, over half of the agricultural land in Simadalen was submerged by the river. The damage to roads and houses was also catastrophic. This was the most destructive flood ever recorded in Hordaland.

Sysendammen

Sysendammen

18.03.2018 - 07:59

Kjerringafjellet

Bergsdalen

13.12.2018 - 15:03

The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.

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