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Engevikhavn
The guesthouse activity in Engevik in the 1700s could not have been very extensive. But a hundred years later a trading and guesthouse centre developed on a piece of land called Engevikhavn. This is the place where Segelcke had obtained licence to operate an inn and guesthouse business in 1729.
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.
Holmeknappen
If you come by sea to Bergen and come up the Herdle Fjord, the yellow ochre marine shed at Holmeknappen is a well known landmark to starboard as you come close to the little shore settlement. In olden days Holmenknappen served important functions as a centre for a wide hinterland of the surrounding farms, warehouse, landing point, country store and later a steamer quay, a hotel (1896) and a dairy (1909). But today Holmeknappen is no longer a focal point. Transport and commercial routes have changed the old pattern
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.