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![The long house at Golta, Sund](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_276-1.jpg?itok=qlke6iyO)
Golta- Long house
In the years between the wars a major registration of houses and house costumes, house construction methods, fireplaces and forms of housing clusters was started in West Norway – an ambitious mapping of everything that came under the name “Registration of Culture and Geography in West Norway”. One of the places of which material was gathered in 1938 was an old multi-room house at Golta; new and interesting material for the researchers from the Historical Museum, but well known within the local building tradition through several generations.
![Goltasund bridge and Goltasundet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_276_goltasundet_150.jpg?itok=1CBSE3io)
Goltasundet
For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.
![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.
![The Salting shed at Trælevika.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_275-4.jpg?itok=20MdCbWg)
![Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_18.jpg?itok=PD2tmRI1)
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
![Strandflat and scree by land](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_14.jpg?itok=4i8IcPpe)
![Smedholmen, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_219-_bu.jpg?itok=RVN_WnRB)
![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.
![Bordalsgjelet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_33.jpg?itok=xPd4kUeG)
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
![The mighty scree by Langeland Farm](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_53.jpg?itok=_aFa06qZ)
Teigdalen
It is not surprising that there are several folk tales connected to the large and unusual scree deposit that is found at Langeland, uppermost in Teigdalen. It is said that folk have been taken into the mountains by these stone blocks and have come back and told about how the wood nymphs live. It is also said that packs of thieves hid here in the old days, both themselves and the treasures they had stolen.