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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.
![Vinnesleira](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_3.jpg?itok=XFQuYzaF)
Vinnesleira
Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.
![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.
![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.
![Rekvesøyane](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_23.jpg?itok=AaNmW0ie)
Rekvesøyane
The sediment that was deposited from the river Dyrvo has created the fan-shaped delta Rekvesøyane. The bit of land farthest out toward the water gets periodically flooded, especially during snow melt and after periods of much rain.
![Rockslide at Mundheim in the spring of 1997](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_3.jpg?itok=M0w_nyFl)
Mundheim
At Mundheim there is a dangerous stretch of the highway. The mountainside has given way several times in this area. Typically, it happens in the spring, when the frost has loosened its grip.
![Buardalen and Buarbreen before 1880.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/odda_27.jpg?itok=6wyvqy1Z)
Buardalen Valley
Buarbreen glacier was one of the first destinations during the period of increasing tourism in Odda in the 1800s. Foreigners came by the thousands, mostly Englishmen and Germans, to the magnificent landscape in front of the glacier. Back at the hotel in Odda they could enjoy drinks containing ice from the glacier.