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).

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.

Kinso

Ferstad

Ferstad is well worth a visit. The farm lies on a little hillock south of Lekven: a beautiful official residence from the 1700s.

Civil Servants in Small Societies 1650 – 1850

Lysekloster- The monks and nature

Lysekloster was the largest agricultural property in the country when it was phased out during the Reformation in 1537. In its prime this cloister encompassed two-thirds of all the farms in Os. The monks introduced and cultivated new plant species and it was probably they who stocked the waters with fish not indigenous to the area. This legacy from the Middle Ages has left a lasting mark.

Oselva

Oselvo is the biggest waterway on the Bergen peninsula, with sources in Gullfjellet and Sveningen. There is a fall of only 60 metres along the entire stretch from Samdalsvatnet Lake to the sandbank in Fusafjorden. It is rare to see a river like this in western Norway. There is salmon along this entire section of the Oselvo river.

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.

Rambjøra

In Sanddalen and Helldalsåsen the building of houses has increased dramatically. Where there eariery was grazing land, hundreds of families now live. Not far away, lies Rambjøra as an oasis in the built up area.