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![The defensive refuge at Borgåsen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh-etne-2_img_1.jpg?itok=9l2JAuTi)
Borgåsen
In Etne there are no less than four defensive refuges. They are all situated in strategic positions, so that they have served as places of refuge and protection for central parts of the district
![Toward Støle and Sørheim, 1920.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/terassen.jpg?itok=1OuuZEj5)
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
![Boat engines, Norwegian Engine Museum in Skånevik](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_189_motormuseum_1_150.jpg?itok=CDwNdWQJ)
![Botnavatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_20.jpg?itok=q4QcNNrR)
![The Battle of Fitjar from Erik Werenskiold pen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_214-2_ny.jpg?itok=_9eechIK)
Fitjar- the King's farm
In front of Fitjar Church there is a memorial stone, sculpted by Anne Grimdalen and erected in 1961, for the thousand-year memorial of one of the most dramatic events in Norway’s history, the Battle of Fitjar. This was the place where Norway’s king, Håkon the Good, suffered his fatal injury in the fight with Eirik’s sons, probably in the year 961.
![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.
![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.
![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)
![Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/skanevik_endret_til_rgb.jpg?itok=KfKszhQ9)
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.