The village of Etne

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

Kyrping

The trading post down by the fjord at Kyrping does not belong to the oldest group of trading posts from the 1600s and 1700s. It was only after the liberalisation of the trading legislation that trade was established here.

Langfoss

Skånevik- the trading post

There are only two buildings left of the old trading and guesthouse settlement in Skånevik. They are in the centre, close to the main road passing through the settlement. The other buildings that belonged to the place, the lodging house (“Holteriet”), the bakery, the courthouse, the boathouse and the sea house with the store, were pulled down in the last century.

Huglo

The majority of Huglo is bare rock. A bit of dwarf pine forest is the only vegetation able to put down roots. Along the west- and east sides, to the contrary, the landscape is unusually green and lush. The reason lies both in the bedrock and in the ice that covered the area 12 000 years ago.

Hystad- burial mounds

The biggest collection of prehistoric burial relics in Stord is to be found in Hystadmarka. There are still 16 burial mounds and two stone rings visible here; finds that span from the Bronze Age to the Viking Age in time.

Hystad- the black alder forest

One of the biggest black alder forests in the country is in Hystadmarkjo. Along the well prepared trail through the forest you can experience an exceptional nature with an unusual abundance of exuberant plant species. But what has laid the foundation for this richness?

Kåravika

Leirvik- The trading post

Already in the Middle Ages the good harbour at Leirvik provided a connecting point. Here was a court of law, and a guesthouse was established here in the 1600s. But Leirvik never achieved the status of a trading post or a ship-loading place. In the census of 1865 parts of the farms Nordre Bjelland, Leirvik and Orninggård are mentioned as the “Coastal district of Lervig”. And the community grew around the old guesthouse location early in the 1800s.

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.