| dbo:abstract |
Norrland terrain (Swedish: Norrlandsterräng) is a geomorphic unit covering the bulk of Norrland and the northwestern half of Svealand. Except for The High Coast the coastal areas of Norrland do not belong to the Norrland terrain. The southern and eastern boundary of the Norrland terrain is made up of geological faults that disrupt the Sub-Cambrian peneplain found the lowlands. In some locations these faults have been extensively eroded making the Norrland terrain boundary partly a result of erosion. Karna Lidmar-Bergström categorizes the Norrland Terrain into the following classes: 1. * Highlands with well developed valleys above 500 m.a.s.l. 2. * Plains with residual hills of Northern Sweden 3. * Undulating hilly land of Övertorneå/Överkalix 4. * Undulating hilly land of Boden area 5. * Large scale joint valley landscapes 6. * Plains with residual hills of Dalarna 7. * Undulating hilly land of central Sweden (en) Norrlandsterräng är en terrängtyp som dominerar i Norrlands och nordöstra Svealands barrskogsområden. Den sydliga gränsen för terrängtypen sammanfaller väl med den Biologiska norrlandsgränsen, som identifierades av Rutger Sernander. Terrängtypen domineras av bergkullsterräng och bergkullslätter. Topografin i terrängtypen har en relief om 50-400 meter. (sv) |
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dbo:Organisation |
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Norrlandsterräng är en terrängtyp som dominerar i Norrlands och nordöstra Svealands barrskogsområden. Den sydliga gränsen för terrängtypen sammanfaller väl med den Biologiska norrlandsgränsen, som identifierades av Rutger Sernander. Terrängtypen domineras av bergkullsterräng och bergkullslätter. Topografin i terrängtypen har en relief om 50-400 meter. (sv) Norrland terrain (Swedish: Norrlandsterräng) is a geomorphic unit covering the bulk of Norrland and the northwestern half of Svealand. Except for The High Coast the coastal areas of Norrland do not belong to the Norrland terrain. The southern and eastern boundary of the Norrland terrain is made up of geological faults that disrupt the Sub-Cambrian peneplain found the lowlands. In some locations these faults have been extensively eroded making the Norrland terrain boundary partly a result of erosion. Karna Lidmar-Bergström categorizes the Norrland Terrain into the following classes: (en) |
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Norrland terrain (en) Norrlandsterräng (sv) |
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