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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.
![Nedre Helland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_1.jpg?itok=J9xuc7pb)
Nedre Helland- skred
Many still remember when the avalanche struck Nedre Helland, on the 14th of August, 1953 14:30 o'clock. All of the buildings at one of the farms and the main house on the neighbouring farm were destroyed. The one woman who was inside a building escaped, frightened but unharmed. The same with the others who lived at Nedre Helland; everyone was a safe distance from the avalanche.
![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.
![Otterstadstølen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_4.jpg?itok=yFY5zoII)
Otterstadstølen
Otterstadstølen lies in an idyllic grassy plain surrounded by rich forest, but also with high mountains close by. The mountainsides are steep and typical of this part of the county. The same cannot be said about the forest. This spruce forest has been able to develop freely for hundreds of years. Otherwise in the county, only Voss has spruce forest.
![Steinslandsvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_466.jpg?itok=Wx0aw3W7)
![The rectory at Finnes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_203_finnas_1_150.jpg?itok=MjLf1y2s)
![From a soapstone quarry at Lykling](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_268_lykling_kleber_2_150.jpg?itok=F7bjH3TA)
![The old limestone quarry is today rebuilt and become Moster Amfi.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_206-3a.jpg?itok=US4hTVFq)
![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.