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![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.
![The marine shed at Hollmeknappe, Meland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_296-1_0.jpg?itok=bMReCI2n)
Holmeknappen
If you come by sea to Bergen and come up the Herdle Fjord, the yellow ochre marine shed at Holmeknappen is a well known landmark to starboard as you come close to the little shore settlement. In olden days Holmenknappen served important functions as a centre for a wide hinterland of the surrounding farms, warehouse, landing point, country store and later a steamer quay, a hotel (1896) and a dairy (1909). But today Holmeknappen is no longer a focal point. Transport and commercial routes have changed the old pattern
![Nedre Helland](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mo_1.jpg?itok=J9xuc7pb)
Nedre Helland- skred
Many still remember when the avalanche struck Nedre Helland, on the 14th of August, 1953 14:30 o'clock. All of the buildings at one of the farms and the main house on the neighbouring farm were destroyed. The one woman who was inside a building escaped, frightened but unharmed. The same with the others who lived at Nedre Helland; everyone was a safe distance from the avalanche.
![Mo with the Otterstad farm in the background early in the 1900s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_329-1_0.jpg?itok=JUVMdLHq)
Otterstad
Tthe Otterstad farms lie in the innermost part of Mofjorden, on the northwest side of the river. The row of stave-built boatsheds that belong to the farm were probably constructed a little after the middle of the 1800s. Both here and on the Mo side, the boatsheds were important storage places at the seashore; wood and other farm products intended for the town; corn and merchandise in return.
![Steinslandsvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_466.jpg?itok=Wx0aw3W7)
![Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_18.jpg?itok=PD2tmRI1)
Fitjarøyane
If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.
![Strandflat and scree by land](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_14.jpg?itok=4i8IcPpe)
![Smedholmen, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_219-_bu.jpg?itok=RVN_WnRB)
![The fields have been affected by many landslides](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ull_12.jpg?itok=UmE0Qwae)
![Hårteigen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ull_26.jpg?itok=3IkRLl38)
Hårteigen
Hårteigen, «the grey signpost», as the name suggests, is a landmark for mountain hikers on the western plateau. The piece of mountain is also a monument for the mighty rock layers that once covered the entire plateau.