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![Potholes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_31.jpg?itok=W2LZyIpN)
![Skjervet toward the east. Jørdre Farm up to the left.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_32.jpg?itok=HGK8HMBs)
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.
![St. Ludvig.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_274-4s.jpg?itok=gXvooPsW)
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.
![Boat bow of oak shaped like an animal head.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_223-4.jpg?itok=6Y1lzt5t)
![Ådlandsstova, as it stood at Nedre Ådland, Stord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_209-2_sk_414.jpg?itok=cG31Cib5)
Ådlandsstova
The Ådland house is one of the biggest medieval houses still existing in West Norway. It is constructed from unusually large, hard fir wood, beautifully oval-cut. One story links the cottage to the Gildeskålbakken at Orninggård (Lower Ådland); thus indicating that the cottage has been the medieval banqueting hall. The building has been dated back to the 13-1400s by carbon dating.
![Huglo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_27.jpg?itok=9cCQ5yAR)
Huglo
The majority of Huglo is bare rock. A bit of dwarf pine forest is the only vegetation able to put down roots. Along the west- and east sides, to the contrary, the landscape is unusually green and lush. The reason lies both in the bedrock and in the ice that covered the area 12 000 years ago.
![Baldellia](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_30.jpg?itok=cgEojqGU)
Ådlandsvatnet
Plants that grow in and beside water have to be prepared for marked and rapid changes in their living conditions. They must be able to tolerate living under water without drowning, and getting totally dried out without whithering. Many swamp plants are well adapted to these kinds of changes.
![Stordfjella mountain towards the south.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_38.jpg?itok=IY1GTmKU)
Kattnakken–Stovegolvet
The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.
![Folkedal](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_367-4.jpg?itok=88ZF6fTB)
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.