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![Ask mot Herdlefjorden og Holsnøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/askoy_18.jpg?itok=31Vc89f-)
Ask- jordbær
Strawberry-growing on Askøy flourished in the beginning of the last century. When gardener Samson Eik took in the type "Seierherren" from Rosendal in 1909 for growing strawberries on Hop, it appeared that the soil and climate in this area was perfect for the mass production of strawberries.
![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.
![Midtvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fjell_27.jpg?itok=816BuZcP)
Fjell river network
There are many river networks out by the coast and they tend to be small and unassuming. The farmer has relied upon the watercourses to run his mill and saw, and it may be that the trout have given him a good source of food in years when the ocean fish failed. In our time, these river networks are being rediscovered for their value in recreation and outdoor life, and several places, tourist trails have been built in order to fully enjoy them.
![Botnavatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_20.jpg?itok=q4QcNNrR)
![Whitefish](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_3.jpg?itok=BdQyPUBu)
![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.
![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.
![Bømoen toward the north.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_52.jpg?itok=mV3IWyRp)
![From Hamlagrøhornet one sees a division between the fertile phyllite and the naked Precambrian basement rock types in the landscape](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_55.jpg?itok=WKuDCDHt)
Hamlagrø
The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.