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![Potholes](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/gra_31.jpg?itok=W2LZyIpN)
![Brekkhus](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_342_brekkhus_150.jpg?itok=TjykXKlw)
![The Ostra chests are easily recognisable with their characteristic style.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_327-1.jpg?itok=x-fr2TBj)
Mjøsvågen
Around Mjøsvågen here is still a compact marine use area. Some of the buildings are common boathouses, but most of them also house small enterprises and workshops. This is where the farmers from Øvsthus, Mjøs, Hole and other farms have supplemented their meagre incomes as smiths, brass moulders, clog makers, chest builders and decorative painters.
![Grytøyrelva](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/nv_482.jpg?itok=xhxzmzEq)
![Opo](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/odda_32.jpg?itok=X8hRVGS1)
![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.
![The icefall from Folgefonna calves out in Lake Juklavatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/jondal_10.jpg?itok=iERB9CRo)
Folgefonna
The glacier is not only white – it is full of colour. The colours have several sources: glacial flour, desert dust, or living algae. And the light refraction in the ice creates cool, bluish nuances – a masterpiece of the interaction between cold and light.
![The waterfall at the top of Tokagjelet](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvam_49.jpg?itok=OJAJPjRK)
Tokagjelet
There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.
![The soil tongues below Jomfrunuten.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_36.jpg?itok=aOfkkEth)
Jomfrunuten
Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.
![Vosso between Evangervatnet and Bolstadfjorden.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/voss_34.jpg?itok=OZVJPGrh)
The Vosso river network
The Vosso is Hordaland's main artery, she has never run more richly than in our times, and no other river in western Norway carries so much water. The increase in the amount of water comes mainly from hydropower development, due to the transfer of water from other water systems. Climate change can also be a reason that the Vosso carries more water than before.