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![Potholes by the Koldals River](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fokllk.jpg?itok=MZgPWao9)
Eikelandsosen
"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"
![The trading post of Engevikhavn, Fusa](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-243-3.jpg?itok=WaEdeaKO)
Engevikhavn
The guesthouse activity in Engevik in the 1700s could not have been very extensive. But a hundred years later a trading and guesthouse centre developed on a piece of land called Engevikhavn. This is the place where Segelcke had obtained licence to operate an inn and guesthouse business in 1729.
![Gjønavatnet and Kikedalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_320_kikedalen_150.jpg?itok=mWd_BFbm)
![The trading store at Holsund is now in the Horda Museum.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_247-xx.jpg?itok=osh8ymrJ)
![The Hellands scree](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_15.jpg?itok=lTDOoMCW)
![Skjelbreid terrace](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_27.jpg?itok=xBptoHjz)
Skjelbreid
On the east side of Lake Skjelbreidvatnet, clearly visible along the road from Eikelandsosen, we notice a farm on a terrace above a grassy hill. The hill has the form of a broad shield; Skjelbreid (" Broad Shield") is the name of the farm.
![Sundvor, Fusa](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_242-3.jpg?itok=Q9j0Y-ci)
![Vinnesleira](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_3.jpg?itok=XFQuYzaF)
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.
![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.
![Strusshamn at the beginning of the 1800s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_269-2-3.jpg?itok=GGmjJiOc)
Strusshamn
On the south side of Askøy, just west of Bergen, lies Strusshamn. The sheltered bay is one of the best harbours in Byfjorden, on the route south. At the time of the sailing ships the harbour could be full of vessels from Bergen and abroad, lying in wait for favourable wind. Old anchoring rings from 1687 bear witness to this. Strusshamn was a quarantine harbour for ships that came sailing in with the yellow pest flag flying.