220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.
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.
The richest seabird localities in Bjørna Fjord are FLUØYANE, a group of small and medium-sized islets just east of the entrance to Våge. Here, we see many different nesting birds, but there is the danger that overgrowth will become an obstacle for nesting here in the future. On one of the islands, the environmental protection authority has promised to step in and help the birds.
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.