University of Bergen
From Dense Forest to Open Heathlands
The outer frame - the coast, the fjord and the mountains - are an inheritance from the country's geological history. But what, more than anything else, gives the scene colour and excitement is the plant life.
From “Spearway” to National Highway
Glaciers
Two of Norway's - and mainland Europe's - largest glaciers, in addition to a number of smaller glaciers, lie in Hordaland. This eternal ice is easily accessible, and easy to be enchanted with. A National Day parade goes to the top of the Hardanger glacier, and Folgefonna glacier has lift assistance at the summer ski centre in Jondal.
Hardangervidda – Crossing the Uplands
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.
Hordaland as high as the Himalayas- the Caledonian mountain chain
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,
Last Ice Age
The continental glacier that covered Hordaland was like a great power that had decisive influence over our natural history. The glaciers which at the beginning of the last ice age (more than 100,000 years ago) grew out from Folgefonna, Hardangerjøkulen and other mountainous areas, chased animals and birds, and most likely also humans in front of their paths. Small animals, plants and trees were mercilessly run over and crushed to powder under the thick ice. Even the hard bedrock got torn up and scoured by the ice, which did not give up before it reached the outer edges of the continental shelf. First 14,500 years ago, the climate became mild enough that the outer coastal strip of Hordaland once again became ice-free. Plants, animals and people started to migrate in to a landscape that was golden, with flecks of grey moraine and sand between smoothly polished rock outcrops - as our present warm interglacial was born.
Local Dialects in Hordaland
Language tells us both about social distance and human contact in many different ways. The dialects show how people who have had connections and dealings with one another throughout the ages, have developed a common language.
Mining in Hordaland
Ølve has the oldest known mines in Hordaland. In 1642, privilege was granted by the king to build an iron works in Jernsmuget on the property of Lilledals Farm, and five years later a copper works on the same property. Operations were suspended in 1673. Mining resumed again in the municipality in the 1750s. Also this time, in the region of Ølve.
Names in the Landscape
A tale of man and the environment
