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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.
![Stordalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/stordalen_endret_til_rgb.jpg?itok=nn6EunGo)
Stordalen
When the Etne water system was protected in 1994, preservation of the cultural landscape in Stordalen Valley was a a main objective. This is a valley with an exceptional abundance of Different types of plants and animals. In the grey alder forest in Stordalen there are more bird species than in most other places, in fact, denser than one tends to find in a tropical rainforest.
![Botnagrenda](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_369-_2.jpg?itok=9FLr126Z)
Botnen
Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.
![Nestunet by Nesvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_378_x.jpg?itok=TEDlV-ov)
Nes
The farm Nes lies directly inside Mundheim on a forested headland in the fjord between Mundheimsvika and Bondesundet, a farm with an attractive and well-kept cultural landscape.
![The décor from the Skogasel house](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_376-2.jpg?itok=QmBEEr5T)
![Dwelling house and store from the Øystese hamlet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_370-1.jpg?itok=7m6cFMFJ)
![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.