Interfluve

This article will address Interfluve, a topic that has captivated the interest of numerous scholars and specialists in different areas of knowledge. The relevance of Interfluve is manifested through its impact on society, culture, history and human development. Over time, Interfluve has sparked debates, research and reflections that have enriched the understanding of this phenomenon. From various perspectives and approaches, the multiple facets of Interfluve have been analyzed, revealing its complexity and its influence on various aspects of daily life. In this sense, this article aims to explore the phenomenon of Interfluve in a comprehensive and rigorous manner, providing a broad and updated vision of this topic.

The East Styrian Hills south of Herberstein

An interfluve is a narrow, elongated and plateau-like or ridge-like landform between two valleys. More generally, an interfluve is defined as an area of higher ground between two rivers in the same drainage system.

Formation

These landforms are created by earth flow ("solifluction"). They can also be former river terraces that are subsequently bisected by fluvial erosion. In cases where there is a deposit of younger sedimentary beds (loess, colluvium) the interfluves have a rounder and less rugged appearance. A consequence of interfluve formation is the so-called "interfluvial landscape."

Interfluvial landscapes

See also

References

  1. ^ Ernst Neef (ed.): Riedel. In: Derselbe: Das Gesicht der Erde (Taschenbuch der physischen Geographie). Verlag Harri Deutsch, Frankfurt/M, 1970, p. 774.
  2. ^ a b Leser, Hartmut, ed. (2005). Wörterbuch Allgemeine Geographie, 13th ed., dtv, Munich, p. 766, ISBN 978-3-423-03422-7.
  3. ^ Whittow, John (1984). Dictionary of Physical Geography. London: Penguin, 1984, p. 275. ISBN 0-14-051094-X.
  4. ^ Sicherung und Entwicklung der charakteristischen Riedellandschaft zwischen Dürrer Aurach und Aubach at www.land-oberoesterreich.gv.at. Retrieved 1 Jan 2015