FLUVIAL PROCESSES, WIND AND FANS CHANGING IN THE LOUT PLAIN (DASHT-E LOUT), IRAN

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MOGHIMI E.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Paper Information

Journal: GEOGRAPHICAL RESEARCH QUARTERLY Year:2005 | Volume:37 | Issue:52 Page(s): 27-37

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Information Journal Paper

Title

FLUVIAL PROCESSES, WIND AND FANS CHANGING IN THE LOUT PLAIN (DASHT-E LOUT), IRAN

Author(s)

MOGHIMI E. | Issue Writer Certificate

Keywords

FLUVIALQ4

WINDSQ4

FANSQ4

LOUT PLAINQ2

CHANGESQ2

Abstract

These essay has prepared with using the Landset imagery (1/1000000 scale); topograpy maps (1/250000 scale) and field works. The valley fills and FANS-forming are two important landscape of FLUVIAL landforms in LOUT PLAIN.Average Lout unit height is about 980m and has many big, small, old and new FANS. The old FANS are higher, the new FANS are lower and sometime deposited on old FANS. Source of many parts of Landforms in LOUT PLAIN (more than half) are depositional-FLUVIAL kind. In this essay we examine 3 groups of FLUVIAL processes, wind and FANS CHANGES. Aeolian processes in the Lout are trenching and building of recent alluvial material at the toe and headfans.

Cites

THE EFFECT OF NEHBANDAN FAULT SYSTEM MOVEMENT ON GEOMORPHOLOGY OF THE NEHBANDAN AREA

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APA: Copy

MOGHIMI, E.. (2005). FLUVIAL PROCESSES, WIND AND FANS CHANGING IN THE LOUT PLAIN (DASHT-E LOUT), IRAN . GEOGRAPHICAL RESEARCH QUARTERLY, 37(52), 27-37. SID. https://sid.ir/paper/5533/en

Vancouver: Copy

MOGHIMI E.. FLUVIAL PROCESSES, WIND AND FANS CHANGING IN THE LOUT PLAIN (DASHT-E LOUT), IRAN . GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2005;37(52):27-37. Available from: https://sid.ir/paper/5533/en

IEEE: Copy

E. MOGHIMI, “FLUVIAL PROCESSES, WIND AND FANS CHANGING IN THE LOUT PLAIN (DASHT-E LOUT), IRAN ,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 37, no. 52, pp. 27–37, 2005, [Online]. Available: https://sid.ir/paper/5533/en

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