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![Dalskarvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_46.jpg?itok=Alucy1eG)
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.
![Stordfjella mountain towards the south.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_38.jpg?itok=IY1GTmKU)
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.
![Frå kopargruvene på Tveit.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/tveit_gruve.jpg?itok=hjvhdIKa)
![Einstapevoll](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sveio-11.jpg?itok=kzXzvNHZ)
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”.