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![Glacier fall at Bondhusbreen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_41.jpg?itok=R53rfaSZ)
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
![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)
![Fjøsanger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_49.jpg?itok=x0vBKTNz)
Fjøsanger
Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.
![Norwegian Sagebrush](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/jondal_3.jpg?itok=fj-tqk5a)
Jonstein
When high school student Arne Handegard collected plants for a herbarium in 1962, he didn’t know what kind of rarity he had pressed into his notebook. 30 years later he attended a botanical lecture, where a picture was shown of a plant he recognized: “Norwegian Sagebrush, which in Norway is only found in a large area of Dovre and in Trollheimen, and in a little area in Ry county”. Arne Handegard raised his hand: “That plant grows on Mt. Jonstein in Jondal”.
![Gjønavatnet and Kikedalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_320_kikedalen_150.jpg?itok=mWd_BFbm)
![The Hellands scree](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_15.jpg?itok=lTDOoMCW)
![The saw tooth pattern is clearly visible from Skora Mountain southwards toward Tellnes and Skogsvågen.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fjell_26.jpg?itok=JF-ZMEUU)
Haganes
The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.
![Fantasy drawing of the animal life that reigned when the Bjorøy layer was deposited during the younger part of the Jurassic Period.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_35.jpg?itok=VWoic2L9)
Vatlestraumen
There are coal bits hidden in the sand under Vatlestraumen. These remains from a geological layer from the Jurassic Period were discovered when the undersea Bjorøy Tunnel was built in 1994. Oil- and gas reservoirs in the Troll Field in the sea west of Hordaland are from the same time. It is, nonetheless, quite surprising to find bedrock from dinosaur time inside of the outer islands of western Norway. On the Scandinavian mainland north of Denmark, there are only a very few places where one f inds rock from this time in earth history.
![The sites show the longhouse, a smaller “old folk’s house” and a hayshed.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/3151.jpg?itok=c_m0Rz1s)
Lurekalven
Lurekalven is an unpopulated island of heather moor which is a part of the wilderness belonging to the five farms on Ytre Lygra. Between the two islands there is only a small sound. As late as the 1920s, milking cows were rowed over the sound from Lygra in summer – a form of farming that was adapted to the coastal landscape.
![Romarheimsdalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_33.jpg?itok=VKAH_TBc)