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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.
![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)
![Gjønavatnet and Kikedalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_320_kikedalen_150.jpg?itok=mWd_BFbm)
![Vøringsfossen waterfall and the Upper Måbødalen Valley, as seen from the viewpoint at Hotel Fossli.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_27.jpg?itok=N8nsqBs2)
Måbødalen- geology
The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.
![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.
![Fossen cliff](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/sam_11.jpg?itok=VQQxhF23)
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
![Romarheimsdalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_33.jpg?itok=VKAH_TBc)
![The farms on Toska lie on moraine soils from the Herdla moraine.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_21.jpg?itok=Zzbp7oRx)
Toska
The peat bogs on Toska have been mined for peat since 1946, when the island got electricity. In this treeless coastal landscape, peat was the most important source of energy, and this took quite a toll on the bogs.
![Langfoss (Alf Adriansen)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/etne_32.jpg?itok=bIoehHDD)