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Helleland
The old “recorder residence” at Helleland has been both residence for the district recorder and officer’s residence. The main building, which came under protection in 1924, was built in 1764 by the curate Christian Heiberg. When he was appointed parish priest in Jølster, he sold the farm to the state employee Geelmuyden, who resold the farm to Hans De Knagenhielm in 1774. He was the head of “Søndre Hardangerske kompani” (a local army division).
Hop- Thomas Erichsens Minde
From the 1500s Hop was noble estate for the law speaker in Bergen and Gulen judicial districts. Several of the law speakers were of noble descent, such as Hans Hansen Lillienskiold and Niels Knagenhielm. The beautiful main building, still standing, was erected by the Bergen merchant Thomas Erichsen in 1793-95. He also established a magnificent garden with an 800 metres long linden avenue reaching down to the stone boathouse at Hop harbour.
Herdla farm
Numerous finds show that the settlement at Herdla goes back to prehistoric times, and the large estate at Herdla has enjoyed a central place in the nation’s history since High Middle Ages. As Ask, Herdla was part of the country estate Harald Hårfagre took over as he took command of the west of Norway.
Hesthamar
Hesthamar, some kilometres north of Utne, is one of the oldest residences for a district recorder in the country. In 1637, barely 50 years after the office of the district recorder was established in 1591, the local people bought this residence from the bailiff Lauritz Johnsen on Torsnes. From 1659 the district recorders lived here, intermittently, up to 1790. This is when Helleland at Lofthus became a “recorder” farm.
Finnås
At Flintaneset by Finnåsvika, in the centre of the municipality, we find the most beautiful and best preserved igneous rocks in western Norway. We must go to Hawaii or Island to find as fine structures as at Bømlo.
Siggjo
Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.
Urangsvågen-Rubbestadneset
In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.