Håhaugsteinen

Huse

The farm Huse is situated on a broad terrace in the valley above the church and the commons ground in Kinsarvik. Huse is one of the largest farms in Kinsarvik. The house from the Middle Ages, still standing at Huse today, probably from the middle of 1200, is joined on to a house in the Swiss style from around 1890. This house, with a smoke-vent in the roof, bears witness of a grand old farm and of the chieftain’s power in early medieval times.

Utne

When sergeant Peder Larsen Børsem from Strandebarm was “demobilised” in 1721, following the large Nordic War, he married the Bergen lady Elisabeth Schrøder and settled as innkeeper at Utne with a letter of privilege from the county governor dated 29 October 1722.

Årekol

Grødalshaug

At the bottom of Vargavågen on Halhjem lies Grødalshaug, a 30 metres high rocky outcrop between the bay and a moist valley cleft. On the south side of the rock is a steep rock cliff facing the valley, the bog and the stream. On this rock face we find rock carvings from the Bronze Age.

Sandviksfjellet

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

Frette

Isdalen

The valley on the inside of the Svartediks dam, a five minutes' bus ride from Bergen centre, is often referred to by Bergen folk as Isdalen ("Ice Valley") - justifiably, since the area could have been described in textbooks for its ice-carved land forms. The glacier's polishing over ca. 40 ice ages has created a magnificient landscape. The original ice valley climbs up behind Ulriken at the end of Svartediket.

Hårteigen

Hårteigen, «the grey signpost», as the name suggests, is a landmark for mountain hikers on the western plateau. The piece of mountain is also a monument for the mighty rock layers that once covered the entire plateau.

Melderskin

MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.