- Remove Smallholdings filter Smallholdings
- Remove Archaeological findings filter Archaeological findings
- Remove Museum filter Museum
- Remove Large landforms filter Large landforms
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.
Fitjar- the King's farm
In front of Fitjar Church there is a memorial stone, sculpted by Anne Grimdalen and erected in 1961, for the thousand-year memorial of one of the most dramatic events in Norway’s history, the Battle of Fitjar. This was the place where Norway’s king, Håkon the Good, suffered his fatal injury in the fight with Eirik’s sons, probably in the year 961.
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
Rimsvarden
Rimsvarden lies high and unencumbered, an enormous stone mound on the highest top with a wide view of the Fitjar rural community. With its 30 meters across and almost 4 meters high, this is one of the largest prehistoric burial relics existing in Hordaland.
Årskog
Årskog farm is situated in a typical coastal landscape in a gentle terrain that slopes down from the outlying heaths down towards the fjord. The farm steading exists as it was in the 1800s. In 1980 the two brothers, Lars and Olai Årskog donated the farm with all its contents of tools and interior decoration, for museum purposes.
Huglo
The majority of Huglo is bare rock. A bit of dwarf pine forest is the only vegetation able to put down roots. Along the west- and east sides, to the contrary, the landscape is unusually green and lush. The reason lies both in the bedrock and in the ice that covered the area 12 000 years ago.