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.

Gjerde church

Grindheim church

The first church at Grindheim was a stave church with a free-standing steeple. The church was first mentioned in 1326, but was probably built long before this time.

Støle church

The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.

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.

Søvik

Os valley

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.

Sæbøtunet

When you come into the well-tended farm steading at Sæbø just above Etne centre, you get the impression of a Sunnhordland farm from well before the time of the tractor; from the time of the horse and the scythe. The hamlet at Sæbø, one of the farms neighbouring to Gjerde, was taken over by Sunnhordland Folk Museum in 1938.