. The earth and its inhabitants .. . tofCr, by the west and south-west winds. But going northwards the snow-line falls uniformly from 4,000 or 5,000 feet on either side of the Folgefond, and to 3,000, or even 2,400, on the mountains about North Cape. The isothermal lines, determined by systematic observation at the fifty-three Norwegian and twenty-nine Swedish meteorological stations, present in summer and winter the same general form. They run nearly parallel on the west coast, describing their principal curve towards the south-west from Trondhjem to Christiania.

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Keywords: ., bookcentury1800, bookdecade18, booksubjectgeography, bookyear1883