RELICT PERIGLACIAL SLOPE DEPOSITS IN THE GECHI GHAL-A

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MOKHTARY D.

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Journal: GEOGRAPHICAL RESEARCH Year:2004 | Volume:19 | Issue:3(74) Page(s): 126-142

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Title

RELICT PERIGLACIAL SLOPE DEPOSITS IN THE GECHI GHAL-A"SSI MOUNTAIN AND ITS CONTIGIUOUS SLOPES, NORTHWEST OF IRAN:OBSERVATIONS AND PALAEOENVIRONMENTAL IMPLICATIONS

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MOKHTARY D. | Issue Writer Certificate

Keywords

SLOPE DEPOSITSQ3

PERIGLACIERQ4

PALAEOENVIRONMENTQ4

GECHIGHAL-A"SSIMOUNTAINQ4

NORTHWEST OF IRANQ2

Abstract

Gechi Ghal-a"ssi stock is located on the northern slope of Misho Dagh in East Azerbaijan of Iran. Past geomorphological evaluation of high altitude slope in Gechi Ghal-a"ssi and adjacent slopes, was largely based on hypothetical or macro- scale geomorphic approaches. Consequently, the information pertaining to high altitude Misho -Dagh"s Quaternary slope environments has remained rather rudimentary. The present study describes the morphology of the region and discusses the likely palaeogeomorphic processes of debris deposites on the Gechi Ghal-a"ssi and adjacent north-facing slopes. Shattered bedrock near the summit of Gechi Ghal-a"ssi , is closely associated with several slope landforms such as blocky SLOPE DEPOSITS(block fields, block streams and blocky slopes) and talus which grade the downslope. The landforms are primarily related to seasonal fiost creep at the Last Glacial Maximum (LGM) when this area have a cold/humid climates, and secondly, are influenced hardly by the slope face and the duration of sunlight radiation. Rock glaciers and mass movements have had important role in transferring deposits to the downslope. At present, the formation of talus, block strips, mud boils and talusy ice core on the slops of study area are resulted fiom active seasonal frost/melt processes.

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APA: Copy

MOKHTARY, D.. (2004). RELICT PERIGLACIAL SLOPE DEPOSITS IN THE GECHI GHAL-A"SSI MOUNTAIN AND ITS CONTIGIUOUS SLOPES, NORTHWEST OF IRAN:OBSERVATIONS AND PALAEOENVIRONMENTAL IMPLICATIONS. GEOGRAPHICAL RESEARCH, 19(3(74)), 126-142. SID. https://sid.ir/paper/29968/en

Vancouver: Copy

MOKHTARY D.. RELICT PERIGLACIAL SLOPE DEPOSITS IN THE GECHI GHAL-A"SSI MOUNTAIN AND ITS CONTIGIUOUS SLOPES, NORTHWEST OF IRAN:OBSERVATIONS AND PALAEOENVIRONMENTAL IMPLICATIONS. GEOGRAPHICAL RESEARCH[Internet]. 2004;19(3(74)):126-142. Available from: https://sid.ir/paper/29968/en

IEEE: Copy

D. MOKHTARY, “RELICT PERIGLACIAL SLOPE DEPOSITS IN THE GECHI GHAL-A"SSI MOUNTAIN AND ITS CONTIGIUOUS SLOPES, NORTHWEST OF IRAN:OBSERVATIONS AND PALAEOENVIRONMENTAL IMPLICATIONS,” GEOGRAPHICAL RESEARCH, vol. 19, no. 3(74), pp. 126–142, 2004, [Online]. Available: https://sid.ir/paper/29968/en

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