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![From Ingahogg.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvinnherad.jpg?itok=dmrfeaRp)
Ingahogg
At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.
![From Upper Musland toward Geitadalen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_48.jpg?itok=PG7RknzF)
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.
![Ground up bedrock in the Valen Fault, seen under a microscope.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_31.jpg?itok=Hhx1ihCW)
![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.
![Rimbareidtjørna](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fi_15.jpg?itok=TrTU29bZ)
Rimbareid- Vestbøstad
At nesting time you cannot avoid hearing the calls of the curlew or the snipe along the narrow road through the cultural landscape from Rimbareid to Vestbøstad. And on late summer evenings, the intense song of the sedge warbler rings out over the two characteristic tarns in the area.
![Iglatjødno](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_44.jpg?itok=MRGFOnX6)
![Lake Tveitavatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_42.jpg?itok=AqtnVja2)
Tveitavatnet
It is difficult to imagine that a plant can grow at the same place for many thousands of years: Climate and local environment change. Different species grow up and die out. Nonetheless, some plants get established, but don't manage to spread into new areas, because the climate is at the edge of what they can tolerate. Great fen-sedge is just such a plant.
![Baldellia](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_30.jpg?itok=cgEojqGU)
Ådlandsvatnet
Plants that grow in and beside water have to be prepared for marked and rapid changes in their living conditions. They must be able to tolerate living under water without drowning, and getting totally dried out without whithering. Many swamp plants are well adapted to these kinds of changes.
![Leech (Jan Rabben)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_9.jpg?itok=6mOcgRc5)