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that extend north of it. These forests are known in Sweden as Norra barrskogsregionen (lit. the northern conifer forest region). The southern boundary of the
Norrland terrain was identified as a major phytogeographical boundary by
310:"Large scale joint valley landscape" is a translation of the original Swedish term "Storskalig sprickdalslandskap". Sprickdalslandskap is itself a renaming of the earlier concept "RutplatĂĄland" (Square plateau land).
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found the lowlands. In some locations these faults have been extensively eroded making the
Norrland terrain boundary partly a result of erosion.
50:
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
126:. The phytogeographical boundary is not fully sharp as valleys of the Norrland terrain constitute transition zones for vegetation.
288:
plain" are translations of the original
Swedish term "Bergkullsslätt". Another name for these surfaces in northern Sweden is
518:
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From the south the entrance to the
Norrland terrain is not only seen in the relief but in the vast and contiguous
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301:"Undulating hilly land" is a translation of the original Swedish name "Bergkullsterräng" or "Bergkullsland".
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Sporrong, Ulf (2003). "The
Scandinavian landscape and its resources". In Helle, Knut (ed.).
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122:. For example, the boundary coincides with the northernmost extension of natural grown
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The purple line marks a version of the southern boundary of the
Norrland Terrain.
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361:(1995). "Relief and saprolites through time on the Baltic Shield".
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Highlands with well developed valleys above 500 m.a.s.l. at the
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categorizes the
Norrland Terrain into the following classes:
388:(1996). "Long term morphotectonic evolution in Sweden".
344:. Swedish Society for Anthropology and Geography: 125–136.
380:
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171:Plains with residual hills of Northern Sweden at
203:Undulating hilly land of Central Sweden seen at
66:Highlands with well developed valleys above 500
334:(1926). "Norra Sveriges landforms-regioner".
73:Plains with residual hills of Northern Sweden
8:
219:Undulating hilly land of Central Sweden at
445:. Cambridge University Press. p. 22.
16:Geomorphic unit covering northern Sweden
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104:Undulating hilly land of central Sweden
187:Large scale joint valley landscape at
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443:The Cambridge History of Scandinavia
94:Large scale joint valley landscapes
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465:(in Swedish). Cydonia Development
422:(in Swedish). Cydonia Development
134:are the overwhelmingly commonest
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280:"Plains with residual hills", "
98:Plains with residual hills of
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42:and the northwestern half of
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38:unit covering the bulk of
487:(1969). "Landskapet". In
87:Undulating hilly land of
77:Undulating hilly land of
386:Lidmar-Bergströrm, Karna
359:Lidmar-Bergströrm, Karna
109:Phytogeography and soils
267:do however exclude the
240:South Swedish highlands
235:Central Swedish lowland
269:Scandinavian Mountains
245:Sub-Cambrian peneplain
60:Karna Lidmar-Bergström
56:Sub-Cambrian peneplain
31:
24:
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462:Nationalencyklopedin
419:Nationalencyklopedin
519:Geography of Sweden
493:Det Moderna Sverige
337:Geografiska Annaler
457:"Norrlandsgränsen"
414:"norrlandsterräng"
398:. Elsevier: 33–59.
371:. Elsevier: 45–61.
205:Säter Municipality
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499:. pp. 64–67.
489:Lundqvist, Magnus
271:from the terrain.
54:that disrupt the
52:geological faults
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120:Rutger Sernander
32:Norrlandsterräng
28:Norrland terrain
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485:Lundqvist, Jan
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191:, Ă…ngermanland
189:The High Coast
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115:boreal forests
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48:The High Coast
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46:. Except for
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469:December 12,
467:. Retrieved
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426:November 22,
424:. Retrieved
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410:Rapp, Anders
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284:plain" or "
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265:Anders Rapp
263:Geographer
157:Abisko Alps
513:Categories
318:References
223:, Värmland
175:, Lappland
159:, Lappland
136:soil types
89:Boden area
79:Ă–vertorneĂĄ
36:geomorphic
30:(Swedish:
286:Inselberg
282:Monadnock
207:, Dalarna
83:Ă–verkalix
524:Norrland
497:Bonniers
229:See also
173:Jokkmokk
68:m.a.s.l.
44:Svealand
40:Norrland
491:(ed.).
221:Hagfors
142:Gallery
100:Dalarna
34:) is a
251:Notes
471:2017
428:2021
132:peat
130:and
128:Till
124:oaks
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396:16
394:.
377:^
369:12
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350:^
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342:8
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81:/
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