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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.
![Gjuvsland (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/navn.jpg?itok=npdQFont)
![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.
![Kjerringafjellet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_31.jpg?itok=iFmhzSNw)
Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
![Flatekvål](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_29.jpg?itok=FmtrpVtP)
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.
![Drawing of how it might have looked at Straume 7000 years ago.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/vaksdal_32.jpg?itok=LfWFLsDG)
Skipshelleren
For vel 7000 år sidan var Straume ein av dei beste – om ikkje den beste – veideplassen i Hordaland. Steinalderfolket som busette seg ved Skipshelleren, skjøna truleg ikkje kor heldige dei var. Mellom dei opptil 2 meter tjukke dyngjene med stein og bein som arkeologar grov fram i 1931–32, fann dei reiskapar og avfall frå fangst og matstell. Frå dette materialet har arkeologane stava seg fram til livet ved straumen.
![Kårstad, Veafjorden](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_336_zz.jpg?itok=A1-9xe5P)
![Anne and Reidar Skorpen during the hay harvest.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/tysnes_14.jpg?itok=REkmXQvq)
Ånuglo
Take a tour to Ånuglo on a warm summer's day. You can anchor up in Skipavågen and go exploring along the beach. Or, you can find giant holly trees and ivy inland on the island. If you take a trip to the small farms on the west side - one of which is still in operation - you can experience colourful flower meadows from a time most dream of, but few can still remember.
![Botnagrenda](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_369-_2.jpg?itok=9FLr126Z)
Botnen
Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.
![Nestunet by Nesvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/kvh_378_x.jpg?itok=TEDlV-ov)
Nes
The farm Nes lies directly inside Mundheim on a forested headland in the fjord between Mundheimsvika and Bondesundet, a farm with an attractive and well-kept cultural landscape.