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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)
![View in over Mostraumen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_16.jpg?itok=GnR34JLO)
Mostraumen
Until 1743 the people from Modal had to wait for a flood in MOSTRAUMEN before they could draw their boats up the river current, and then row back across Lake Movatnet. But, that year the flood opened a free passageway all the way to Mo. Hordaland had gained a new tidal waterway.
![Under the grass fields lie large quantities of sand and gravel.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_24.jpg?itok=e4ePAE19)
Nedre Helland- Sand Quarries
The three spades in the municipal coat of arms for Modalen are sand spades. Sand quarrying has brought income and employment. As much as 70,000-80,0000 tonnes of sand and gravel left the municipality each year since the turn of the millennium, to be used as cementing sand. Why is Modalen endowed with so much sand?
![Mo with the Otterstad farm in the background early in the 1900s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_329-1_0.jpg?itok=JUVMdLHq)
Otterstad
Tthe Otterstad farms lie in the innermost part of Mofjorden, on the northwest side of the river. The row of stave-built boatsheds that belong to the farm were probably constructed a little after the middle of the 1800s. Both here and on the Mo side, the boatsheds were important storage places at the seashore; wood and other farm products intended for the town; corn and merchandise in return.
![Otterstadstølen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_4.jpg?itok=yFY5zoII)
Otterstadstølen
Otterstadstølen lies in an idyllic grassy plain surrounded by rich forest, but also with high mountains close by. The mountainsides are steep and typical of this part of the county. The same cannot be said about the forest. This spruce forest has been able to develop freely for hundreds of years. Otherwise in the county, only Voss has spruce forest.
![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.
![Today there are only a few farmers that grow potatoes in Fitjar.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_22.jpg?itok=avXiCbey)
Fitjar- potatoes
The deep agricultural soils in Fitjar are found especially in the area between Lake Storavatnet and Breivika. The many stonewalls in the area reflect that the earth probably was full of stones and stone blocks. The stones that couldn't be dug out had also a function: they stored heat that helped to grow potatoes.