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.

Storsøya Island

On Storsøya Island, English ivy grows nearly everywhere. It creeps along the ground and climbs all the way to the top of the tree trunks. Together with holly, the trees of juniper, yew and an unusual pine forest keep the island green the whole year 'round.

Ådlandsstova

The Ådland house is one of the biggest medieval houses still existing in West Norway. It is constructed from unusually large, hard fir wood, beautifully oval-cut. One story links the cottage to the Gildeskålbakken at Orninggård (Lower Ådland); thus indicating that the cottage has been the medieval banqueting hall. The building has been dated back to the 13-1400s by carbon dating.

Einstapevoll- the farm

Einstapevoll (from einstape: “bregne” (fern)) lies on the west side of the Tittelsnes peninsula. Up to 1831 the farm was a vicarage belonging to Stord parish. The priests had leasing rights. Land rent and other fees from the farm was part of their salaries.

Haugsbø

The single unit farm without a road to it, Haugsbø, is situated on the east side of the Tittelsnes peninsula facing Ålfjorden. As far back as the Middle Ages the farm has probably belonged to Stord Parish, up to the 1800s. In 1590 it was thought to be abandoned, but in 1601 Mickel Hougsbøe paid a tithe on the farm.

Hopsfjellet

On June 2nd, 1992, a big forest fire broke out in Sveio. The fire started southeast of Hopsfjellet. In a strong wind the flames spread quickly northward. Houses on the other side of the highway were threatened, but escaped unscathed. The burned area, which is easily visible about a 5 minute's drive south from the tunnel at the triple- junction, was made into a nature reserve in 1998. The intention was to ensure that the re-establishment of plant- and animal life would take place without disturbance.

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.

Espevikpollen

Færavåg

The main house at Færavåg was built in 1599. History tells us that a German came to Færavåg and built the house. He divided the land between his two sons. They in turn divided it between their two sons, thus there were four equal holdings on the farm. And it is said that all households lived in the same house. They each stayed in their own corner around the fire in the middle of the floor.

Hopssundet