University of Bergen- Remove Small landforms filter Small landforms
- Remove Middle age filter Middle age
- Remove Eidfjord filter Eidfjord
- Remove Large landforms filter Large landforms
- Remove Tysnes filter Tysnes
- Remove Currents and tides filter Currents and tides
- Remove Igneous rocks filter Igneous rocks
- Remove Ullensvang, frå 2020 del av nye Ullensvang kommune. filter Ullensvang, frå 2020 del av nye Ullensvang kommune.
- Remove Rock carvings filter Rock carvings
- Remove Granvin, frå 2020 del av nye Voss herad filter Granvin, frå 2020 del av nye Voss herad
Kinsarvik
Kinsarvik has probably been a centre for the inner Hardanger districts back in prehistory. History tells us that in medieval times there was a marketing place, a “kaupang”, here; a connecting point in the communications between east and west. There were supposedly around 300 residents here but the place was likely wiped out in a great fire.
Måbødalen- geology
The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.
Hårteigen
Hårteigen, «the grey signpost», as the name suggests, is a landmark for mountain hikers on the western plateau. The piece of mountain is also a monument for the mighty rock layers that once covered the entire plateau.
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.
