- Remove Smallholdings filter Smallholdings
- Remove Radøy, frå 2020 del av nye Alver kommune. filter Radøy, frå 2020 del av nye Alver kommune.
- Remove Maritime environments filter Maritime environments
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Churches filter Churches
- Remove Eidfjord filter Eidfjord
- Remove Fusa, frå 2020 ein del av nye Bjørnafjorden kommune filter Fusa, frå 2020 ein del av nye Bjørnafjorden kommune
- Remove Vaksdal filter Vaksdal
- Remove Arkitektur filter Arkitektur
- Remove Metamorphic rocks filter Metamorphic rocks
- Remove Stone age filter Stone age
Holdhus church
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.
Holmefjord
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.
Halne
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.
Fosnstraumen
At the southern end of the bridge between Radøy and Fosnøy archaeologists found an unusual Stone Age settlement. There was a thick “cultural layer” here with the remains of the waste dumps of a hunting people. The place was called Kotedalen. Here they came, one group after the other, and settled for some weeks, some months, or maybe years before they went on, leaving the settlement deserted. Time after time it happened. At least 16 settlement phases have been identified, stretching over 5,500 years.
Vågenes
On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.
Bergsdalen
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.