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![Skreien](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_21.jpg?itok=H25GT68d)
![Hetlefloten i Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/723.jpg?itok=iwhgEn9w)
![Raudlia](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_28.jpg?itok=88h0oT36)
![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-)
![Villelia](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_13.jpg?itok=9i20fr7T)
![Rosendals Mountain (Jan Rabben)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/256.jpg?itok=o54SuV1X)
Melderskin
MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.
![This little mountain in the picture sticks up because the layers are tilted on their sides.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/oygard_21.jpg?itok=ugcTumKb)
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