Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.
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.
Skorpo - Polished by glaciers and meltwater
There is still a lot of ore in the abandoned mines on Varaldsøy Island. If today's prices and availability of ore continue, it is doubtful whether the mines will resume operation. But, the pyrite is there, if the market should return. On Varaldsøy Island one finds at least nine mines and prospect pits, that for the most part date back to the latter part of the 1800s.
On the farm of Arnatveit, high up on the slope above the highway, an old smokehouse remains standing in the courtyard of the main farm property, in the place of the old common courtyard. Today this farm lies at the outskirts of a large housing estate. Most of the farmland of the other farm properties has been sold to benefit the city’s need of sites for the new community of Arna.
In the 1300s Bergen was a trading centre of European dimension. The town is thought to have had around 7000 inhabitants and was the largest and most important in the country. In a European context it was an average size town. At this time the most tightly built town area was still mostly east of Vågen from Holmen in the north to Vågsbotn in the south. Already in medieval times, latest in the 1340s, this area was called Bryggen.
Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.