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![Geologists from all over the world come to study the veined bedrock (the dark stripe in the picture) at Spildepollen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sund_9.jpg?itok=Guc62QqZ)
Spildepollen
The oceanic crust of the North Sea was subjected to a lot of stretching both in Permian and Triassic times, and later in the Jurassic. This stretching resulted in the North Sea collapsing in and also to large faults forming west of Hordaland and on the mainland. Austefjorden in Sund follows one of these faults.
![Deportations from Tælavåg 30 April 1942.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_277-2x-1.jpg?itok=E8EZwkL_)
Tælavåg
Tælavåg has a significant place in the history of the German occupation in WWII. The small community by the sea, where for centuries people had made a living from farming and fishing in harmony with the natural resources, in 1942 became the victim of German reprisals without their equal in Norwegian war history. The collection of war histories in Tælavåg provides us with a close-up of the dramatic events.
![St. Ludvig.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_274-4s.jpg?itok=gXvooPsW)
Tyssøy
B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.
![Skrivargarden in “”Kåravikjo”.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_210-2.jpg?itok=sQdjqHps)
![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.
![Coat of arms, Orning](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_209-1.jpg?itok=48LepR7r)
![The main building at Huglo, Stord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_213-3_futastovo213.jpg?itok=JflzRyZ3)
Sørhuglo
The tax collector’s farm at Sørhuglo is one of the many farms for state employees in Hordaland. According to history, “Futastovo” was built by the tax collector Gram in the second half of the 17th century. In 1943 the building was moved to Sunnhordland Folk Museum.
![Ådlandsstova, as it stood at Nedre Ådland, Stord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_209-2_sk_414.jpg?itok=cG31Cib5)
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.
![Boat bow of oak shaped like an animal head.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_223-4.jpg?itok=6Y1lzt5t)
![Espevik](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_15.jpg?itok=xW8eH-Lu)
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.