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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.
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.
Skogsøyna
There isn't much forest on Skogsøyna today, but that there is, has been planted. There is not much wildlife, either. But, quite a lot of birds pass by Skogsøyna during migration time. Ther is no other place along the coast where you can better observe the seabird migrations.
Fedje bog
The wild rabbit is really native to Northwest Africa, but the Ancient Romans introduced them to large parts of Europe. Not to Norway, rightly enough: the population on Fedje originated from 3-4 pairs that were brought here from the Shetland Isles in 1875, making this their first residence in the country.
Hellisøy
Hellisøy lighthouse was lit for the first time in 1855. The characteristic red cast-iron tower with two white belts is 33m high and a light height of 46m above high tide.
Holmengrå
Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.