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![The stave church in Røldal](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_55-1.jpg?itok=s4rVLQ2e)
Røldal
The stave church in Røldal was one of the key pilgrimage churches in West Norway. The church was probably built between 1250 and 1350, and in the high Middle Ages Røldal was the most important destination for pilgrims in the country beside the Nidaros cathedral. It was the crucifix that attracted people to midnight mass on midsummer night. That was when it excreted its miraculous sweat.
![The rock paintings in Grødalshaug, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_234-x.jpg?itok=3teSxvuP)
Grødalshaug
At the bottom of Vargavågen on Halhjem lies Grødalshaug, a 30 metres high rocky outcrop between the bay and a moist valley cleft. On the south side of the rock is a steep rock cliff facing the valley, the bog and the stream. On this rock face we find rock carvings from the Bronze Age.
![Lyse chapel, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_238-1.jpg?itok=QUOPChLG)
Lyse chapel
The small white-painted chapel with the red brick tiled roof just south of the monastery ruins at Lyse was built in 1663 as a local chapel for the monastery estate, following the takeover of the property by the District Recorder (Stiftskriver) Niels Hanssøn Schmidt two years previously. The chapel, with its harmonic proportions, lies in the cultural landscape beside the grand monastery estate, witness to a time gone by. But even today, there is a tradition of high mass on the 2nd day of Ascension in Lyse Chapel.
![Hetlefloten i Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/723.jpg?itok=iwhgEn9w)
![Geologist William Helland-Hansen examining a quartz conglomerate in the Ulven Syncline on one of the hills by the north west end of Lake Ulvenvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_31.jpg?itok=kdZe21Du)
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.
![From](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_312_vaksinen_ulven_150.jpg?itok=P4DdHVu-)