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.

Bergsdalen

The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.

Hana

Skreien

Moster- The old church

Moster is mentioned as a church site already in the time of Olav Tryggvason. According to the sagas the king is supposed to have laid the foundations for the first church at Moster when he came there in 995. That building would have been a stave church - the church standing there today – a stone church with a nave and narrower, straight chancel – was probably founded around 1100. In 1874 a new church was built at Moster. Then the old church was bought by The Society for the Preservation of Norwegian Ancient Monuments, which is still the owner.

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.

Onarheim

Hamlagrø

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.