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Engesund
For more than 350 years Engesund has been a place for hostelries and trading in the Fitjar islands. The place is centrally placed in the shipping lane, with a sheltered harbour close to the exposed Selbjørnsfjorden. Engesund was once part of the great network of historical stopover places on the coast.
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
Frekhaug
Frekhaug has been a large farm with well-off owners through many generations. The main house, a two storey building with a hipped roof, must have been erected about 1780.
Færøysund
The old trading post lies at the sound between Stord and Færøy in Langenuen. There was a country store and steamship forwarding agent up to 1964. The trade was then moved over to the new ferry harbour of Sandvikvåg.
Grønafjellet
Mountain plants with their beautiful, colourful flowers are common in high altitude areas in Norway. On the coast there are not so many of them. But, here and there one nonetheless finds mountain plants, and this makes some coastal mountainsides a little bit different. Perhaps the growth on these mountainsides gives us a little glimpse of a distant past?
Kjelstraumen
If you take the sea route north you have several options. The various routes have been dealt with in history, and through the Middle Ages the traffic increased as well as the trading with Nordland in fish and herring, feather and down. One of the central routes passes through Kjelstraumen, in the sound between Ulvøy and Bakkøy. This has been a place for a guesthouse since 1610, with Royal Letter of Privilege, part of the large network of trading post and guesthouse locations along the coast.
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.