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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.
Gullbrå
From written sources we know that the farm Gullbrå was in use early in the 1600s. The Apostolic church in Bergen owned land here that it rented out, but even early in the 1600s some of the land was in private ownership. Eksingedalen then belonged to Modalen parish, which was under Hamre parish. In 1723 the Apostolic church still had properties here, and Ivar and Lars were farmers.
Færavåg
The main house at Færavåg was built in 1599. History tells us that a German came to Færavåg and built the house. He divided the land between his two sons. They in turn divided it between their two sons, thus there were four equal holdings on the farm. And it is said that all households lived in the same house. They each stayed in their own corner around the fire in the middle of the floor.
Godøysund
The old hostelry centres were strategically placed with good harbours and anchoring conditions where people travelled. GODØYSUND, or Gøysundet, as it was called, was in the middle of Tysnes Parish, with easy access from the sea, also for the local population. Gøysundet is amongst the oldest hostelries in Sunnhordland.
Klinkholmen
Kubbervik, or Vikjo as it was known colloquially, must have been established as a trading post under the farm of Håland some time around 1600. The reason for this was probably the thriving trade on Scotland. Every year ships from the islands in the west came to buy lumber in Bårsund. Vikjo was the harbour in use, as the place is ideally situated on the route through Bårsund, the sound between Reksteren and Tysnesøy.
Nedrevåge
Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.