Marine activities expanded greatly throughout the 19th century, and provided a livelihood for many people. Fishing and shipping were probably the subsidiary activities which had greatest economic significance throughout the century. Marine activities brought, literally speaking, wind into the sails of many rural districts in Hordaland during that period.
Craftsmanship through two thousand years
The art of spinning, the art of weaving and the art of dyeing wool is knowledge which has been an important resource in the natural household for several thousand years. And the art of weaving still fascinates new generations.
På ferd mot vest over Hardangervidda opplever vi det dramatiske panoramaet når vidda går over i djupe bergkløfter og høge fossefall – eit utsyn som har fascinert kunstnarane.
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.
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.
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 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!