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Dalskarvatnet–Dyvikvågen
Many of the fossils one finds on Stord are related to fossils of the same age found in North America. Scientists thinks this indicates that the bedrock on Stord was much nearer to America at that time than today.
Einstapevoll- slates
“On the country of Wallestrand…the rock almost everywhere appears to be of a slate-like substance, be it at the seashore, on the farms or in their distant fields”.
Espevik
220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.
In Memory of Fartein Valen
“Fartein Valen is the key figure within newer Norwegian music. Not by way of being more popular than other younger composers, but because he aims at things higher, which he is fully confident of being able to reach since he commands all techniques. But there is a price to pay for reaching above the ordinary, and there is a price to pay for demanding more than the ordinary from the listeners. This is something Valen has experienced”.
Ingahogg
At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.
Kattnakken–Stovegolvet
The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.