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![A zone with nuggets from the inner earth.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/auste_26.jpg?itok=6s7Qo0xH)
![Cross-leaved heath (Akvarell: Miranda Bødtker)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/auste_3.jpg?itok=LlH8ouMq)
![Bergesfjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_31.jpg?itok=i9o6PSWe)
![The lobster park in Espevær](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bomlo_39.jpg?itok=QWK2IaA7)
![Siggjo from the south. (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_52.jpg?itok=ZLhD-gho)
Siggjo
Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.
![The eider population at Bømlo has increased sharply during the last decade.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fuuugler.jpg?itok=gor6FPw4)
![Urangsvågen-Rubbestadneset](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/bo_51.jpg?itok=TOAhYhRU)
Urangsvågen-Rubbestadneset
In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.
![Etne and the Etne delta around 1900.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_2.jpg?itok=bfLAQc7X)
Etnedeltaet
During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.
![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)