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Immagine a colori naturali del nord-est dell'Italia (Regione Friuli-Venezia Giulia) che mostra i torrenti
Cellina e Meduna ed il fiume Tagliamento. I letti ghiaiosi di questi corsi d'acqua contrastano con il terreno circostante, rendendoli immediatamente riconoscibili. Il Cellina ed il Meduna formano
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shape. When a river receives more sediment than it can move effectively, the river changes shape, often carving braided channels. Upstream from the
Cellina, Meduna, and Tagliamento Rivers, the mountain basin is seismically active and prone to landslides. As a result, heavy sediment loads often reach
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belong to cultivated fields. The crops mingle with settlements, some of them quite close to river channels. Some hydrologists have expressed concern about continued development on this floodplain because flood damage has occurred fairly frequently, just as the fertile soils have attracted
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alla loro confluenza la grande V sulla sinistra. Il grande accumulo di materiale ghiaioso è dovuto anche all'instabilità idrogeologica e tettonica dei bacini montani di questi fiumi: nel caso del
Tagliamento di conseguenza si è sviluppata una morfologia fluviale a canali intrecciati (
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161:-coated riverbeds contrast sharply with the surrounding landscape, highlighting the river contours. The Cellina and Meduna Rivers converge in the south, forming a giant
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joint project implies that all materials created by its probe are copyrighted and require permission for commercial non-educational use.
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This file contains additional information, probably added from the digital camera or scanner used to create or digitize it.
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Image captured by the
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
