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![From the old road along the Åkrafjord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_190_akrafjord_veg_2_150.jpg?itok=0G_IOg6S)
![Vollom](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_14.jpg?itok=RhEa2l84)
Vollom
On Vollom, northwest of Seim, we find the only natural beech forest in Western Norway, which is also the most northerly of its type in the world. Beech grows also many other places in the county, but these trees are totally lacking in history compared with those of Vollomskogen Forest.
![Toward Støle and Sørheim, 1920.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/terassen.jpg?itok=1OuuZEj5)
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
![Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/skanevik_endret_til_rgb.jpg?itok=KfKszhQ9)
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.
![Ringedalsfossen innermost in Skjeggedalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_397-1.jpg?itok=3KoWBQlp)
![The mountain farm Øyna in Reinsnos.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_399-1x.jpg?itok=xrSyoFMA)
Reinsnos
The mountain settlement Reinsnos is situated at nearly 700 metres above sea level at the end of the Reinsnos lake; an entry point to the Hardanger plateau.
![Vegane gjennom den tronge og bratte Måbødalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_407-1.jpg?itok=jN0RFHBc)
![Foglefonna and Sandvikedalen with Hardangerjøkulen in the distance.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_40.jpg?itok=QkNKWy9j)
Mosnes
The permanently-protected Mosneselva River, with its meltwater from Folgefonna, runs out into Åkra Fjord by the roadless and uninhabited Mosnes. Those who once lived here were forced to surrender to the ravages of Nature. In the autumn of 1962 there was a flood so great that the people were driven from their farms.
![The sites show the longhouse, a smaller “old folk’s house” and a hayshed.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/3151.jpg?itok=c_m0Rz1s)
Lurekalven
Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.
![English Yew tree i Langebudalen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_247_barlind_etne_150.jpg?itok=JDhAo7PB)