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Norrland terrain () is a geomorphic unit covering the bulk of Norrland and the northwestern half Svealand. Except for The High Coast the coastal areas of Norrland do not belong to the Norrland Terrain.〔 Karna Lidmar-Bergström categorizes the Norrland Terrain into the following clases: #Highlands with well developed valleys above 500 m.a.s.l. #Plains with residual hills of Northern Sweden〔"Plains with residual hills", "Monadnock plain" or "Inselberg plain" are translations of the original Swedish term "Bergkullsslätt". Another name for this surface in northern Sweden is Muddus plains.〕 #Undulating hilly land of Övertorneå/Överkalix〔"Undulating hilly land" is a translation of the original Swedish name "Bergkullsterräng" or "Bergkullsland".〕 #Undulating hilly land of Boden area #Large scale joint valley landscapes〔"Large scale joint valley landscape" is a translation of the original Swedish term "Storskalig sprickdalslandskap". Sprickdalslandskap is itself a renaming of the earlier concept "Rutplatåland" (Square plateau land).〕 #Plains with residual hills of Dalarna #Undulanting hilly land of Central Sweden From the south the entrance to the Norrland Terrain is not only seen in the relief but in the vast and contiguous boreal forests that extend north of it. Till and peat are the overwhelmingly commonest soil types. ==Gallery== File:Abisko_alps.JPG|Highlands with well developed valleys above 500 m.a.s.l. at the Abisko Alps, Lappland File:Jokkmokk utsikt från Storknabben.JPG|Plains with residual hills of Northern Sweden at Jokkmokk, Lappland File:Häggvik High Coast.JPG|Large scale joint valley landscape at The High Coast, Ångermanland File:Gustafs från ovan (5).JPG|Undulating hilly land of Central Sweden seen at Säter Municipality, Dalarna File:Aerial view of Hagfors, Sweden.JPG|Undulating hilly land of Central Sweden at Hagfors, Värmland 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Norrland terrain」の詳細全文を読む スポンサード リンク
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