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![Blomvågen 1851.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/oygard_25.jpg?itok=at3JP7DM)
Blomvågen
"One of the big scientific sensations", was the title in the Bergens Times newspaper on the 22nd of November, 1941. It was the geologist Isal Undås who had been interviewed by the newspaper. He thought that he had discovered a 120 000 year old whale bone, remains of life from before the last Ice Age.
![Bronze keys and remains of a wooden stick from Døso.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_234-1_b.jpg?itok=EoET9UiR)
![The power station at Gåssand, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_237-1-1.jpg?itok=kDd6e2yS)
Gåssand
The 28th November 1914 was a day to remember for the Os inhabitants. This was the day they could turn the switch on the wall and have electric light in their houses. It was like opening the door on the future when the power station at Gåssand was put into operation.
![Stone quarry in Kollevågen, 1922](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/askoy_21.jpg?itok=Xnws-T7D)
![Sandy beach to the west of Kallsøyna, outermost Valen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_353_herdla_150.jpg?itok=XcEOtEry)
Herdla – glacial deposits
The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.
![This is what the northernmost part of the fishing village might have looked like in Viking times](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_288-4.jpg?itok=mGnXIxYE)
![Lysøen, Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_240_hs.jpg?itok=Kqvzn50I)
Lysøen
Lysøen, this fairytale castle with its Russian-inspired onion dome on the corner turret, stands as a reminder of the diversity of the period called Historicism and a monument to a versatile artist; a key figure in the Norwegian National Romanticism.
![Hetlefloten i Os](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/723.jpg?itok=iwhgEn9w)
![Frostrøyk i Osdalføret.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/os_15_b_0.jpg?itok=LqTqmgE7)
Søfteland
If you drive between Søfteland and Ulven on a clear spring morning, or an evening in late autumn, you are advised to be careful on the turns. The temperature on the road can fall to under 0 °C here long before other places in the municipality. On clear, still nights the earth's surface chills quite a bit. In exposed areas a layer of cold air develops very near the ground and the road surface can easily chill to below freezing.
![Toftestallen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_13.jpg?itok=zrSHKUwq)
Toftestallen
The large coastal waves that crash down on the islands west in the sea gather their energy from storms and winds all the way out in the North Atlantic Ocean. The most common place of origin is nonetheless the North Sea. When these waves break over the skerries and islets along the shore, or on the rocky outermost islands, their energy is released. This takes the form of turbulence in the water and sea spray up on land. Can the enormous energy contained in the waves be exploited?