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![Kjerringafjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_31.jpg?itok=iFmhzSNw)
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
![Ekso ved Eidslandet, Eidsfjorden i bakgrunnen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/ekso2.jpg?itok=A_Azq5ry)
Ekso
In the late 1800s, Ekso was known among the nobility in England as having among the best salmon rivers. In summer the Lords could haul in big fish of up to 25 kg. In return, the townsfolk were paid for fishing rights, lodging and local assistance.
![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.
![Hana](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_56.jpg?itok=xl5rWX0M)
![Hellandsfossen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/modal_28.jpg?itok=CXBrp1mg)
![Hellisøy lighthouse, Fedje](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_309-2a.jpg?itok=j0svJC8o)
Hellisøy
Hellisøy lighthouse was lit for the first time in 1855. The characteristic red cast-iron tower with two white belts is 33m high and a light height of 46m above high tide.
![Holmengrå](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fedje_18.jpg?itok=sUXXEBb1)
Holmengrå
Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.
Litlandsvatnet
Large quantities of nickel ore have been mined from Litlandsvatnet, between Lonevågen and Hosanger. The discovery was made in 1875. During the period of operation from 1882 to 1945, 4170 tonnes of pure nickel were extracted from 462 000 tonnes of ore, a large production by Norwegian standards.
![Lonelva](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ost_10.jpg?itok=Zq5z_a93)
Lonelva
It is said that the salmon populations with the largest and the smallest salmon in the world both come from the waters that run out into the fjord system around Osterøy. Vosso is supposed to have the largest spawning salmon to be found in any river, whereas Lonelva is said to have the smallest.
![Lindåsosane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_16.jpg?itok=VlK-dXup)
Lure Fjord
Both Lure Fjord and Lindåsosane to the inside give good living conditions for rare marine organisms: jellyfish, shellfish and fish. These include animals that migrated in after last the Ice Age, when the sea level was higher. Eventually, as the land rose, some of these populations became isolated.