ROCK GLACIERS ON THE NORTH SLOPE OF SABALAN MOUNTAIN

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DALLALOGLI A.

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:2003 | Volume:35 | Issue:45 Page(s): 1-12

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Information Journal Paper

Title

ROCK GLACIERS ON THE NORTH SLOPE OF SABALAN MOUNTAIN

Author(s)

DALLALOGLI A. | Issue Writer Certificate

Keywords

ROCK GLACIERQ4

PERIGLACIERQ4

PERMAFROSTFQ4

TOPOCLIMATEQ3

HOLOCENEQ2

SABALAN MOUNTAIN.Q3

Abstract

ROCK GLACIERs are one of the distinct geomorphology feature are seen in medium size at Sabalan mountain slope. Active ROCK GLACIERs represent the existence of Alpine permafrost, and on the other hand these features sigificant tools for palaeoclimate reconstructing. About 14 ROCK GLACIERs at the North slope of Sabalan at the height of between 3460 and 4400m S.L. has been distinguished. That about cover an area of 6.29 km. Tongue-shaped ROCK GLACIERs with 85.1 percent have the highest spread than lobate ROCK GLACIERs with 14.3 percent. Their area varies from 0.05 to 1.64 km, and their formation at present time depends on the regional TOPOCLIMATE. By using the RILA and RLA concepts their origin has been distinguished. On the basis of their moving rate in a year the probable age of active ROCK GLACIERs can be estimated between 3000-6000 years.

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APA: Copy

DALLALOGLI, A.. (2003). ROCK GLACIERS ON THE NORTH SLOPE OF SABALAN MOUNTAIN. GEOGRAPHICAL RESEARCH QUARTERLY, 35(45), 1-12. SID. https://sid.ir/paper/5470/en

Vancouver: Copy

DALLALOGLI A.. ROCK GLACIERS ON THE NORTH SLOPE OF SABALAN MOUNTAIN. GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2003;35(45):1-12. Available from: https://sid.ir/paper/5470/en

IEEE: Copy

A. DALLALOGLI, “ROCK GLACIERS ON THE NORTH SLOPE OF SABALAN MOUNTAIN,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 35, no. 45, pp. 1–12, 2003, [Online]. Available: https://sid.ir/paper/5470/en

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