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![Glacier fall at Bondhusbreen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_41.jpg?itok=R53rfaSZ)
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
![Fjelberg](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_193_z.jpg?itok=b8s1jJSH)
Fjelberg
The beautiful vicarage on the Fjelberg Island lies a few minutes walk up from the fjord, in a compact enclosure with the church south of the main building and the bishop’s residence to the north; a rare harmonic cluster.
![Kvinnherad Church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_198_x.jpg?itok=yh2bEzjf)
Kvinnherad Church
The stately Kvinnherad Church with its characteristic profile set out against the mighty Malmangernuten in the background, gives you a rare feeling of being present in a historic landscape as you come around Nes and face the well-kept houses at the Skåla farm. The church at Skåla is one of four “fjordungskirker” (one of four main district churches) and this farm was the centre of this coastal administration district.
![Ænes, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_199-2.jpg?itok=F9NXUgeu)
Ænes
Ænes has been one of the prosperous farms at the Mauranger Fjord in medieval times. At the time of Harald Gilles, around 1130, we hear of GAUT at Ænes. The noble families around the Hardanger Fjord were prominent in the political sphere from early on, and it is obvious that the fine and openly situated farm at Ænes was also a good place for a Church.
![Rembesdalsskåka and the lower part of Demmevatnet, from Tresnuten. Demmevass cabin is visible to the left in the picture.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_491.jpg?itok=eg8SNPfS)
Simadalen
On the 10th of August, 1937, over half of the agricultural land in Simadalen was submerged by the river. The damage to roads and houses was also catastrophic. This was the most destructive flood ever recorded in Hordaland.
![Sysendammen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_37.jpg?itok=ibwv5qBG)
![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)
![Dale power station](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_333-4xx.jpg?itok=Y26ZxQM5)
Dale power station
In 1923 Bergenshalvøens Kommunale Kraftselskap (BKK) expropriated large areas for power plants and development of hydropower started soon afterwards. Dale power station with the two first aggregates, each of 14 MW was put into operation on 17 November 1927. In the supply reservoir in Storefossen 5152 cubic metres of concrete were cast, and a modern and well-equipped power station was built.
![A silled lake at Ekse](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_23.jpg?itok=FFeLX3xo)
Eksingedalen- hydropower development
Water discharge at the outlet of the Ekso into Eidsfjord was halved after the big hydropower development in the mountainous area between Modalen and Eksingedalen and further southward toward Evanger in the 1960s, 70s and 80s. In an attempt to amend the changed environmental conditions in the waterway the developer built 35 small dams in the river.
![Boatshed](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_335-3.jpg?itok=egD0W5wD)