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Titlebook: Norway’s Internal Migration to New Farms since 1920; Kirk H. Stone Book 1971 Springer Science+Business Media Dordrecht 1971 20th century.D

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楼主: 宗派
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The , Society Program,ning and loans were available to expand the cultivated area of the nation. But not until 1920 did the state participate directly in the process. Instead it had granted funds for settling operations to one nationwide private agency, to 10 county agricultural societies, and to a few communes.
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Reclamation of Bogs, a semi-public organization, founded in 1902 and very active since the early 1930s, whose task was to sponsor the proper use of Norwegian bogs and peat. The Association is composed of citizen members but the state provides grants for its research.
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The Continuous Settlement Region, of the Oslo Fjord it doubles in width. The region includes most of Norway’s oldest settled areas and there are large sections of close permanently occupied residences in many directions. From Stavanger northward they are broken by the fjords but eastward they generally are uninterrupted excepting near the Swedish border (Fig. 2).
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,The Målselv District: MFZ Sample,to be partly in the Outer Fringe Zone also. Administratively it is the Målselv District and adjacent areas in the southwestern center of Troms Fylke (County), an area analyzed economically and described historically in the middle 1950s (Fig. 12)..
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Outermost Fringe Zone,ry narrow extensions of the zone in Sweden. Two of the others are parts of the OMFZ in Finland and only that S and SW of Karasjok is primarily Norwegian (Fig. 15). It is two-pronged and has maximum dimensions of about 160 km. (100 mi.).
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The State , (Homesteading) Program,The state’s direct support of homesteading began in 1920. At that time the Norwegian . (Parliament) passed new regulations concerning reclamation and homesteading. These went into effect in 1921 and they were one of the major means by which food production was increased, young people were given a place in agriculture, and farm sizes were expanded.
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Perspectives,Internal migration is complex dynamics. Usually it is a series of currents and counter-currents. And these are of varying strengths in unsynchronized periods. So it is in Norway.
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