Os valley

Raudlia

Ulvensletta

Skånevik- moraine

In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.

Rådalen

"...it would not be of any particular economical interest to support the planting of forest as the forest that can be cultivated will leave much to be desired in the way of growth potential." These words stem from the economist that at the end of the 1800s was sent to Stend to inspect the planned reforestation in person. The pioneer G.A.Wilson put the economist's words to shame. The spruce that was planted in Rådalen in the period 1867–1869 became a landmark. No other stand of forest in Scandinavia can boast more trees per unit area.

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.

Vossagran

How did the spruce tree get to Voss? Did the seed or small spruce plants get help from people, for example, to make it here unscathed? Nobody knows.