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![Halnelægeret.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_409-2.jpg?itok=hEx5mouW)
Halne
At Halnefjorden, a few hundred metres east of Halne mountain lodge, lie the remains of two stone sheds – Halnelægeret. Some generations ago the cattle drovers stopped here in the summer; they were the cowboys of their time. But Halnelægeret already had a long history before the cattle drovers came.
![Rembesdalsskåka and the lower part of Demmevatnet, from Tresnuten. Demmevass cabin is visible to the left in the picture.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_491.jpg?itok=eg8SNPfS)
Simadalen
On the 10th of August, 1937, over half of the agricultural land in Simadalen was submerged by the river. The damage to roads and houses was also catastrophic. This was the most destructive flood ever recorded in Hordaland.
![Skytjedalen in Eidfjord.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/011.jpg?itok=YAgcsVmd)
![Sysendammen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_37.jpg?itok=ibwv5qBG)
![The Nottveit farms are situated without road access at Mofjorden.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_330-1z.jpg?itok=vG7SLFkx)
Nottveit
In one of the frame-built haysheds at Nottveit, at holding No. 3, we discover that several of the staves have a medieval look, with large dimensions and carefully rounded edges. According to tradition, it was the farms Nottveit and Mostraumen that supplied the timber for the stave church at Mo, and it is not unlikely that these farms received the old timber in return when the new church was erected there in 1593.
![Steinslandsstølen around 1950.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_331-_2.jpg?itok=4EWYkknE)
Stølsheimen
The large mountain area between Modalen, the Voss communities and Sogn is one of the finest mountain pasture areas in West Norway. In older times this area was called Steinslandsheimen, in our times it has acquired the name Stølsheimen. Power development and protection interests have been opposed here. The core area of Stølsheimen has now been protected as a landscape protection area, while some of the oldest mountain farms have been flooded. A register in the 1970s comprised almost 40 mountain farm settlements in the central area of Stølsheimen, belonging to Modalen, Høyanger and Vik municipalities.
![Bergesfjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_31.jpg?itok=i9o6PSWe)
![One of the employee's homes.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_7.jpg?itok=g8bMYKUS)
Lykling- gold
During the summer of 1979 a rock was found at Lykling in Bømlo that contained 450 grams of gold, and at the end of the 1980s a great many gold samples were laid out for sale. In the old mining area there are still gold miners hunting for the precious metal. But, the big adventure stories are a thing of the past.
![The church at Moster, as drawn by Johan Meyer in 1897.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_206-2.jpg?itok=SGdrZdqC)
Moster- The old church
Moster is mentioned as a church site already in the time of Olav Tryggvason. According to the sagas the king is supposed to have laid the foundations for the first church at Moster when he came there in 995. That building would have been a stave church - the church standing there today – a stone church with a nave and narrower, straight chancel – was probably founded around 1100. In 1874 a new church was built at Moster. Then the old church was bought by The Society for the Preservation of Norwegian Ancient Monuments, which is still the owner.
![Siggjo from the south. (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_52.jpg?itok=ZLhD-gho)
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.