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Golta- Long house
In the years between the wars a major registration of houses and house costumes, house construction methods, fireplaces and forms of housing clusters was started in West Norway – an ambitious mapping of everything that came under the name “Registration of Culture and Geography in West Norway”. One of the places of which material was gathered in 1938 was an old multi-room house at Golta; new and interesting material for the researchers from the Historical Museum, but well known within the local building tradition through several generations.
Goltasundet
For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.
Tyssøy
B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.
Hjelmo
On the farm Hjelmo, furthest north in Øygarden, in the innermost part of a long bay, there is a fine boatshed collection with a church beside it. From times immemorial this has probably been the fish-shed location for these farm units and this was also the landing place for the churchgoers.
Lyse chapel
The small white-painted chapel with the red brick tiled roof just south of the monastery ruins at Lyse was built in 1663 as a local chapel for the monastery estate, following the takeover of the property by the District Recorder (Stiftskriver) Niels Hanssøn Schmidt two years previously. The chapel, with its harmonic proportions, lies in the cultural landscape beside the grand monastery estate, witness to a time gone by. But even today, there is a tradition of high mass on the 2nd day of Ascension in Lyse Chapel.
Ulven
In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.
Sandviksfjellet
On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.