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![Moraine ridges, Fruo.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_22a.jpg?itok=V9Vy57R6)
Fruo
At Fruo, nature has built its own little "Chinese wall ". Some kilometers south of the Vøringsfossen waterfall, there are a number of moraine ridges, the longest and most notable of their kind in Hordaland.
![The Eidfjord terrace as seen from Lægreid, presumably in the early 1900s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_36.jpg?itok=_A8sZyMW)
Hæreid- geology
The Eidfjord terrace is a gigantic ridge that reaches up more than one hundred metres from the city centre in Eidfjord. It serves as a powerful natural monument left behind by the ice when it retreated.
![Sketch showing the process of formation of an esker.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/skisse.jpg?itok=dTA78127)
![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.
![Storegraven and Granvin church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_365-4.jpg?itok=t9act0tk)
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.
![Glacial river plain at Lake Klevavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_32.jpg?itok=duW0R_ur)
Rallarvegen
They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.
![The cross church from 1710](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_359-3_0.jpg?itok=a4Vem1vB)
![Landrovågen, the 1980's.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_283-bu.jpg?itok=xIOX5Ooi)
Landro
Landro has been the largest estate on Sotra, including 15 farms with reasonable conditions for agriculture. Their boathouses have had an excellent harbour in Landrovågen. Landro thus has been a good basis for the combination of agriculture and fishing.
![Flatekvål](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_29.jpg?itok=FmtrpVtP)
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.