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Civil Servants in Small Societies 1650 – 1850
Demographic Growth – A Drive to Development
The cultural landscape or that part of it which is still green and inviting to the eye has been shaped by the farmers’ toil down through the generations. At one time almost all of us were farmers. We see that the crofting system faded away as emigration to the towns and to America relieved the pressure.
Earth and stone
"Humus" is a word with great meaning. It is the soil we live from, in addition to the resources we get from the ocean. This layer of earth - sometimes appearing as loose fertile organic matter; other places as scanty and acidic soil - is found in varying thicknesses over the bedrock. It is the result of 10,000 years of breakdown and erosion following the last ice age, and then several thousand years of cultivation in more recent times. The soil we can buy at the garden centre is a different product than the "natural" humus layer, formed of processes occurring far under the earth's surface. If you dig your spade into the soil where it has not been ploughed before, you will see that there is a big difference in colour, soil structure, moisture and stone content. We might say that the soil is fertile and easily worked some places, whereas other places folk might have given up trying to grow anything on their small patches of land, which then become overgrown with birch and thicket. Modern agriculture does not have room for small stumps between the piles of stone. Nowadays, machines do the job, and they require a lot of space and flat ground.
Farmers and Settlements
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.
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.
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.
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.