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Pusch, Martin; Behrendt, Horst; Gancarczyk, Aleksandra; Kronvang, Brian; Sandin, Leonard; Stendera, Sonja; Wolter, Christian; Andersen, Hans E.; Fischer, Helmut; Hoffmann, Carl. C.; Nowacki, Franciszek; Schöll, Franz; Svendsen, Lars M.; Bäthe, Jürgen; Friberg, Nikolai; Hachoł, Justyna; Pedersen,
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Pusch, Martin; Behrendt, Horst; Gancarczyk, Aleksandra; Kronvang, Brian; Sandin, Leonard; Stendera, Sonja; Wolter, Christian; Andersen, Hans E.; Fischer, Helmut; Hoffmann, Carl. C.; Nowacki, Franciszek; Schöll, Franz; Svendsen, Lars M.; Bäthe, Jürgen; Friberg, Nikolai; Hachoł, Justyna; Pedersen,
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Robin, Vincent; Bork, Hans-Rudolf; Nadeau, Marie-Josée; Nelle, Oliver (January 2014). "Fire and forest history of central
European low mountain forest sites based on soil charcoal analysis: The case of the eastern Harz".
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Lehrian, Stephanie; Pauls, Steffen U.; Haase, Peter (February 2009). "Contrasting patterns of population structure in the montane caddisflies
Hydropsyche tenuis and Drusus discolor in the Central European highlands".
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and low evaporation, and the resulting surplus of water balance feeds large
European rivers and other important water sources. Beside the mountains, large areas of
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Badura, Janusz; Jary, Zdzisław; Smalley, Ian (May 2013). "Sources of loess material for deposits in Poland and parts of
Central Europe: The lost Big River".
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Leopold, Matthias; Völkel, Jörg (January 2003). "GPR images of periglacial slope deposits beneath peat bogs in the
Central European Highlands, Germany".
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systems and also mountainous ranges of medium elevation (between about 1,000–2,000 m (3,300–6,600 ft) a.s.l.), e.g. those belonging to the
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Morten L.; Scholten, Matthias; Wnuk-GĹ‚awdel, Ewa (2009). "Rivers of the
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Morten L.; Scholten, Matthias; Wnuk-GĹ‚awdel, Ewa (2009). "Rivers of the
Central European Highlands and Plains".
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Central
European highlands and their hydrological role, with special regard to the Bohemian-Moravian highlands
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564:. Outlines of the natural history of Europe. Vol. 1. J. van Voorst. pp. 208–234.
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353:"Probable occurrence of sporadic permafrost in non-alpine scree slopes in central Europe"
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of lower altitude (400–800 m (1,300–2,600 ft)) in which the surplus of annual
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Novak, M.; Emmanuel, S.; Vile, M.A.; Erel, Y.; Veron, A.J.; Wieder, R.K. (2003).
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DoleĹľal, F.; KvĂtek, T.; Soukup, M.; KulhavĂ˝, Z.; Tippl, M. (26 September 2003).
318:"Tors in Central European Mountains – are they indicators of past environments?"
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Samec, Pavel; Kučera, Aleš; Tuček, Pavel (31 December 2014).
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and south west
Ireland, the Rhine highlands, the Vosges, the
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Both types of mountains act as "water towers". Their high
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77:. Blocks of elevated highlands are found as dissected
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The provenance of lead in
Central European peat bogs
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The Vegetation of Europe: Its Conditions and Causes
259:. Mountain Hydrology Workshop. Bucharest, Romania.
93:, the Central massif of France, the highlands of
322:Bulletin of Geography. Physical Geography Series
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136:but its sources remain unclear because it lacks
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316:Michniewicz, Aleksandra (18 June 2019).
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672:Mountain ranges of Slovakia
69:It includes the uplands of
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25:Central European Highlands
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642:Natural history of Europe
543:10.1177/0959683613515727
436:Quaternary International
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101:of the Rhine and so on.
472:Soil and Water Research
383:Soil and Water Research
151:more precise citations.
682:Europe geography stubs
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