Holsund

Odland

The auger smithies in Odland and Fosse were amongst those which had the largest production of augers in the period between the Wars. Martinus Fosse built a smithy in 1877, and this was in operation right up to the 1980s - one of the centres for auger production in Meland. In 1930 yet another smithy was built here. There was a smithy at Fossesjøen as early at the 18th century, and at the end of the 19th century they went over to auger smithing. There is still a market for hand-forged augers.

Valestrandsfossen- tanning industry

Valestrand became a centre for the tanning industry in Osterøy; one of the old crafts that has developed into a local industry with many places of work. From the 1870s ever more ventures were started. Many of the large sea houses we see today around the bay have been places for tanning and leather enterprises.

Evanger

Evanger (from Old Norse ålvangr, “vang”, “voll” (field) where the horses may graze) is the place where the river from Vangsvatnet, the Voss watercourse, runs out into Evangervatnet. From here Teigdalen valley runs to the north, towards Eksingedalen, and from here there is a short distance to Bergsdalen in the south.

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

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.

Langhaugane

Skorpo

Skorpo - Polished by glaciers and meltwater

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

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.