• Nynorsk
  • English

Universitetet i bergen logoUniversity of Bergen

Search form

Search form

Arctic hunting folk on their way across the ice

The forgotten saga

22.11.2018

The saga regarding the settlement of Hordaland started off about 10,000 years ago. Most of this saga has been recorded in writing, not on paper, but on stone and on the earth in the forest and the marshes.

The newly mown hay on the farms at Vangdalsberget tell of the landscape of the scythe

Farmers and Settlements

22.11.2018

From 4,500 to 5,000 years ago most of Hordaland was a landscape of forest, right out to the coast and the islands. With our inner eye we can see old oak trees putting their stamp on the heat-loving deciduous forest.

The cairn at Nybunut

Hardangervidda – Crossing the Uplands

15.05.2018

Slepa, the ancient “drove roads” across the plateau, date back to prehistoric times. Through the centuries cattle have been driven to the markets in the east; the people of Hardanger went on their trading journeys with tallow and salt to the mining town and silver mines of Kongsberg, and soldiers and other travellers also used these roads.

Farmers from the fjords should not travel unshaven on the train.

Farmers from the Fjords

15.05.2018

Eitt av dei store samferdsleprosjekta på Vestlandet mot slutten av 1800-talet var opninga av Nesttun-Osbanen i 1894 – ei oppbløming av lokalhandel, turisttrafikk og «landliggere».

Fjordabåtane går ut frå Vågen laurdag ettermiddag

Transport and Communication

15.05.2018

The road through Husedalen

From “Spearway” to National Highway

15.05.2018

Geofysisk Institutt

The pioneers who discovered the natural history of Hordaland

23.05.2019

When Professor Emeritus Knut Fægri (1909-2001) was asked to write the book's chapter about the natural science pioneers of Hordaland, he answered unequivocally, "yes". It was one of the last things he wrote before he died, at the age of 92. In typical Fægri language he presents some of the scholars who, in the time before the University of Bergen was founded, led the way in studying the natural science of The West Country.

Urtidsfjell – gneis fra vestlige deler av Stølsheimen.

The Precambrian Era and Precambrian basement rocks

23.05.2019

Almost nothing is as solid, unchangeable and stable as the Norwegian Precambrian basement rocks. Here, there are no volcanic eruptions or violent earthquakes that can cause natural catastrophes. But, it has not always been that way! There have been periods when glowing hot lava flowed over it or when large parts of the Precambrian basement have "taken a beating", both in Precambrian times and during the Caledonian mountain-building event.

Øst for Bjørsvik, Lindås

Hordaland as high as the Himalayas- the Caledonian mountain chain

23.05.2019

The Himalaya Mountain Chain is being formed by the Indian continental plate colliding w the Asian continent. This happens because the earth’s continental plates are constantly moving in relation to each other. Sometimes they crash together and form large collision zones or mountain chains. The collision between India and the Asian continent has created the world's highest mountain and thickest continental crust. But the creation of the Himalaya mountain chain is essentially just a repeat of what happened more than 400 million years ago when Western Norway and Greenland collided and formed the Caledonian mountain range. That mountain-building event caused quite dramatic changes in topography, climate and crustal thickness, and resulted in both volcanism and a lot of earthquake activity. In addition,

The mountain chain dissapears – and the dinosaurs arrive

The mountain chain disappears – and the dinosaurs arrive!

23.05.2019

The Caledonian mountain chain is an example of how plate movements and continental drift can cause collisions and the upheaval of huge mountain chains. After the horizontal compressional forces ceased, the forces of gravity, wind and water took over and started the process of eroding away the mountain chain. But, nearer to our time the land rose up again to a plateau landscape in the east which slanted down toward the ocean in the west!

Pages