University of Bergen- Remove Small landforms filter Small landforms
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- Remove Sund, frå 2020 del av nye Øygarden kommune filter Sund, frå 2020 del av nye Øygarden kommune
- Remove Granvin, frå 2020 del av nye Voss herad filter Granvin, frå 2020 del av nye Voss herad
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- Remove Masfjorden filter Masfjorden
Skjervet- river theft
At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.
Tyssøy
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.
Matrehola
On a large gravel terrace in Matredalen (the Matre valley), a couple of kilometres from the coastal settlement Matre, lies Storseterhilleren, at the end of a large stone block that came rushing down from the mountain. The Matre river runs just over 100 metres to the east of the cave.
Øvre Folkedal
Folkedal, which today is like a small “detour” from the main highway, was in the Middle Ages centrally situated in one of the most important roads between Hardanger and Voss. This is the road that Olav Haraldsson travelled in 1023, when he came from the royal farm at Avaldsnes for a meeting with the Voss inhabitants about the new belief. The road passes across the mountain pasture Krossaset and down Bordalen to Vangen.
