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Vinnesleira
Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.
Øpstad
The post house at Øpstad stands out in the landscape. An ochre yellow house with a loft and a white-painted house in Swiss style with ochre edgings, bears witness to a well preserved house from the 1800s, nearest neighbour to the beautiful old vicarage. In the Øpstad hamlet there was a post office for more than a hundred years, until the 1970s. Today it is possible to walk the old post road across the mountain to Strandvik, as part of “Den Stavangerske Postvei” (The post road to Stavanger).
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?
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.