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![Sculptures in the bedrock](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/jondal_23.jpg?itok=fS00QTt-)
![The boathouses at Svåsand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_383-2.jpg?itok=KK04JZW2)
Svåsand
Down by the fjord at Svåsand, close to the main highway, there is a long row of boathouses, one of the well-preserved, older boathouse locations along the Hardanger fjord. It is the farms at Svåsand that have their boathouses here, four main farms with origins far back in time.
![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.
![Botnavatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_20.jpg?itok=q4QcNNrR)
![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.
![Liarbø, Fitjar](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_216-3_liarbo216a.jpg?itok=4A2LYm0f)
![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.
![Landskapsdraget sørover langs Krokavatnet og Bjørndalsvida i Etnefjella følgjer Etneforkastinga](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/krokavatnetjpg.jpg?itok=NDr7ckOt)
Krokavatnet
On Sunday the 29th of January, 1989, at 17:38 o'clock, Etna shook. The earthquake, with its epicentre ca. 9 kilometres south of Etne centre, had a strength of 4.2 on the Richters scale. This could be felt over large parts of West Land, especially in the areas around Åkra, Etne, Hardanger Fjord and Sauda Fjord. The earthquake was the largest that has ever been measured in Hordaland.