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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.
![Halsnøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_15.jpg?itok=mn2F8JKB)
Halsnøy
Hadde ikkje Hardangerfjordbreen mot slutten av istida rykt fram over fjordbotnen, ville Halsnøy ikkje eksistert som éi øy, men som mange småøyar. Breen skuva framfor seg så mykje leire frå havbotnen at Brattåsen, Toftåsen, Landåsen og Svartaberg vart samla i eitt landområde.
![Elias Fiigenschoug’s painting of Halsnøy monastery , 1656](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_192-1.jpg?itok=9VO9I-NR)
Halsnøy Monastery
Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.
![Skorpo (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_49.jpg?itok=i4VQIqsW)
Skorpo
Skorpo - Polished by glaciers and meltwater
![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.
![Ølve](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/landstet.jpg?itok=1EeuuxMs)
Ølve
Ølve has a special soil type. Here one finds an extra hard clay soil. This is especially noticed by those who work with excavating for building foundations and the like. Often it is necessary to use especially big digging machines and sometimes even dynamite in order to break up the compact masses. The reason for this is the growth of the glaciers toward the end of the Ice Age: The clay, that was first deposited in front of the glacier, came under great pressure when the glacier later grew and slid out over the clay.
![Skjelbreid terrace](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/fusa_27.jpg?itok=xBptoHjz)
Skjelbreid
On the east side of Lake Skjelbreidvatnet, clearly visible along the road from Eikelandsosen, we notice a farm on a terrace above a grassy hill. The hill has the form of a broad shield; Skjelbreid (" Broad Shield") is the name of the farm.
![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.
![Moraine ridges, Fruo.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_22a.jpg?itok=V9Vy57R6)
Fruo
At Fruo, nature has built its own little "Chinese wall ". Some kilometers south of the Vøringsfossen waterfall, there are a number of moraine ridges, the longest and most notable of their kind in Hordaland.
![The Eidfjord terrace as seen from Lægreid, presumably in the early 1900s.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/eid_36.jpg?itok=_A8sZyMW)
Hæreid- geology
The Eidfjord terrace is a gigantic ridge that reaches up more than one hundred metres from the city centre in Eidfjord. It serves as a powerful natural monument left behind by the ice when it retreated.