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![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_366_x.jpg?itok=bWyHW2Im)
Kjerland
On the farms Kjerland and Røynstrond, east of the river that flows into the fjord, we find many decorative painters who belong to the so-called sòlekistemålarane in Hardanger: Knut and Mikkjel Røynstrand and Johannes Jonsson Kjærland.
![The contrast between phyllite and Precambrian basement is clearly visible at Lussand.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_27.jpg?itok=knbu7uIk)
Lussand- geology
Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.
![Storegraven and Granvin church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_365-4.jpg?itok=t9act0tk)
Storegraven
The first mention of Granvin church in written sources is in 1306, but the church location must be far older than this. The farm Storegraven is centrally situated at Granvinsvatnet, by the important traffic artery between Hardanger and Voss, where the road takes off to Ulvik.
![Gjerde church at Etne](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_186_y.jpg?itok=6BRujecm)
![Grindheim church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_188_yzx.jpg?itok=aRPBqArF)
Grindheim church
The first church at Grindheim was a stave church with a free-standing steeple. The church was first mentioned in 1326, but was probably built long before this time.
![Støle church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_187_stole_kyrkje_150.jpg?itok=QkdeOeRd)
Støle church
The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.
![Dalskarvatnet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_46.jpg?itok=Alucy1eG)
Dalskarvatnet–Dyvikvågen
Many of the fossils one finds on Stord are related to fossils of the same age found in North America. Scientists thinks this indicates that the bedrock on Stord was much nearer to America at that time than today.
![Stordfjella mountain towards the south.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/stord_38.jpg?itok=IY1GTmKU)
Kattnakken–Stovegolvet
The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.
![The quartz quarry in the mountainside above Kvalvikane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ull_27.jpg?itok=zyI9-mbt)
Kvalvikane
In Ålvik quartz has long been used to produce ferro-silicon. The quartz was collected from the other side of the fjord, from the mountainside above Kvalvikane.
![Ullensvang](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_393-1.jpg?itok=d1meAEuf)
Ullensvang church
Ullensvang church, situated beside the vicarage, in idyllic surroundings on the headland just inside Lofthus municipality, is mentioned for the first time in written sources in 1309. At that time the present Gothic stone church must have been new. Judging by the style in the western portal and the eastern chancel windows, the church must have been built around 1300 or just before, probably by builders from Bergen influenced by the English Gothic style.