File:J37 962 Río Iguazú, Oberstromseite.jpg

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Deutsch: Von der Zugangsbrücke zum argentinischen Mirador Garganta Del Diablo talwärts, der Río Igazú superior ist schon auf den letzten 50 Kilometern vor den Wasserfällen sehr breit, entsprechend flach und oberhalb der Wasserfälle inselreich. Das Wasser führt zum Aufnahmezeitpunkt vergleichsweise wenig Sediment mit, doch ist der Iguazú eigentlich ein Klarwasserfluss. Die Sedimentführung, die bis zu einer tiefen Braunfärbung führen kann, entsteht durch die Erosion, die hier von der Entwaldung in Brasilien ausgelöst wird.
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Author Falk2

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Transferred from de.wikipedia to Commons by Wdwdbot using script bot_filetrans.pl (r122M).

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  • 2022-02-02 23:06:24 Falk2 (7899830 Bytes)

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current12:33, 5 April 2022Thumbnail for version as of 12:33, 5 April 20225,802 × 3,868 (7.53 MB)Wdwdbot (talk | contribs)Bot Move: Original uploader of this revision (#1) was Falk2 at de.wikipedia

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