University of Bergen- Remove Small landforms filter Small landforms
- Remove Churches filter Churches
- Remove Late glacial filter Late glacial
- Remove Monastery filter Monastery
- Remove Samnanger filter Samnanger
- Remove Precipitation filter Precipitation
- Remove Granvin, frå 2020 del av nye Voss herad filter Granvin, frå 2020 del av nye Voss herad
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.
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
Storegraven
The first mention of Granvin church in written sources is in 1306, but the church location must be far older than this. The farm Storegraven is centrally situated at Granvinsvatnet, by the important traffic artery between Hardanger and Voss, where the road takes off to Ulvik.
Ådland
Ådland, innermost in the Samnanger Fjord is an old church centre and transport centre; a nodal point in the transport from sea to land. The white painted church standing today, was built in 1851, but there were two older churches here in former centuries.
Kvitingen
Few other places in Hordaland, or even the whole country, get as much rain as in the Samnanger mountains. The mountains here simply attract wetness. The weather station on Kvitingen has continuous measurements all the way back to 1900, and the measurements have documented several records for the county. The station is therefore much used as a reference for the rainfall in western Norway.
