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![Grunnosen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_17.jpg?itok=YXEI98_B)
![Lyngoksen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/austr_16.jpg?itok=FU0ZNly2)
![The farms on Toska lie on moraine soils from the Herdla moraine.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_21.jpg?itok=Zzbp7oRx)
Toska
The peat bogs on Toska have been mined for peat since 1946, when the island got electricity. In this treeless coastal landscape, peat was the most important source of energy, and this took quite a toll on the bogs.
![Garnets at Vågenes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_6.jpg?itok=atL5iY_1)
Vågenes
On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.
![Fløksand - Tidal flats](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/meland_13.jpg?itok=XFwGTS7i)
![Eclogite bedrock at Ådnefjellet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/meland_21.jpg?itok=W8PmuPzd)
Eldsfjellet
The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.
![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)
![Archaeological fins from the sites at Risøya.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_276-2.jpg?itok=hxoLOQ5s)
![St. Ludvig.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_274-4s.jpg?itok=gXvooPsW)
Tyssøy
B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.
![The combination building at Nordvik.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_250-2.jpg?itok=CxcVlWaV)