• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Kvamskogen, toward the north.

Kvamskogen

02.12.2018 - 20:57

The different bedrock types that got shoved in over Hordaland in Cambro-Silurian times still remain, layer by layer, almost like a cake. But at Kvamskogen the cake has been turned upside down.

Hunter carvings

Vangdal

27.05.2018 - 15:02

At Salthamaren in Vangdalsberget it is thought that salt was burned some time in history, and deep layers of coal in the ground show that fire has been made up here several times. But they were hardly salt-burners, the first people who stopped here. Some of them carved figures into the rock. On top of the rocky outcrop, furthest out on the cliff, a group of Stone Age hunters carved animal figures. More than 1,500 years later Bronze Age farmers drew ship figures at the foot of the rock. Both these works of art - some of the oldest in Hordaland – are still visible, carved in the rock at Salthamaren.

Vesoldo

Vesoldo

27.05.2018 - 15:02

Folds are to be found everywhere in the remains of the Caledonian mountain chain. Some were formed during the collision with Greenland, others stem from the time when the mountain chain collapsed. Few can compare with the giant fold that remains in the mountain area around Tørvikenuten, Vesoldo and Hellefjellet.

Bronze find from Ålvik

Ålvik

13.03.2018 - 21:25

The rock paintings in Grødalshaug, Os

Grødalshaug

16.06.2018 - 15:52

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.

Geologist William Helland-Hansen examining a quartz conglomerate in the Ulven Syncline on one of the hills by the north west end of Lake Ulvenvatnet.

Ulven

03.01.2019 - 15:16

In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.