Manger

Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.

Vågenes

On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.

Ystebøtræet

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.

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.

Aga

The grand farm Aga on the west side of Sørfjorden, came under protection in 1937, when the agricultural reform threatened to disperse the old clustered settlement. “Lagmannsstova”, named after the “lagmann” (law speaker) Sigurd Brynjulfsson, was already protected in 1924; one of the authentic profane wooden buildings from the Middle Ages still standing. All the same it is the farmyard itself that is the key cultural monument.

Jåstad

The farm Jåstad, situated a few kilometres north of Agatunet, must have been a grand farm in medieval times. Torolf on Jåstad is mentioned as arbitration moderator in 1293, and in the vaulted corridor at Lyse Kloster Sigurd, farmer at Jåstad, and his wife Sigrid – the king’s kinswoman - are buried.

Kinsarvik

Kinsarvik has probably been a centre for the inner Hardanger districts back in prehistory. History tells us that in medieval times there was a marketing place, a “kaupang”, here; a connecting point in the communications between east and west. There were supposedly around 300 residents here but the place was likely wiped out in a great fire.

Opedal

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.