CLIMATIC GEOMORPHOLOGY OF THE NORTHERN SLOPE OF KEYAMAKI-DAGH (NORTHWESTERN IRAN)

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MOKHTARI DAVOOD

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

Journal Paper

Paper Information

Journal: Journal of Spatial Planning Year:2010 | Volume:14 | Issue:2 (66) Page(s): 163-194

Download Full-Text

Persian Verion

View:

1,569

Download:

Cites:

Information Journal Paper

Title

CLIMATIC GEOMORPHOLOGY OF THE NORTHERN SLOPE OF KEYAMAKI-DAGH (NORTHWESTERN IRAN)

Author(s)

MOKHTARI DAVOOD | Issue Writer Certificate

Keywords

CLIMATIC GEOMORPHOLOGYQ3

QUATERNARY CLIMATIC CHANGESQ3

SLOPE DEPOSITSQ3

PARSIAN ALLUVIAL FANQ3

KEYARNAKI-DAGHQ3

NORTHWESTERN IRANQ2

Abstract

The northern slope of Keyamaki-Dagh volcanic dom, due to its high elevation (3414m height), and slope orientation and absence of other effecting factors such as tectonic activity and insignificant anthropogenic interferences, is a good case study for proposing the topic of palaeoclimatic changes based on geomorphological records.In this research, we studied some of the geomorphic features that their formations require long-term time, and the role of climate in their establishment has been investigated, via interpretation of topographic and geologic maps, areal photos and specially field study. Deposited valleys, cliff-talus systems, avalanche talus, blocky flows, and rockglaciers are sloppy features, and aggradational and deggradational phases, debris flows changes in size of the deposited particles and Tufa formation are features related to climatic changes on the PARSIAN ALLUVIAL FAN.The results showed that geomorphic aspects of northern slope of KEYARNAKI-DAGH have been influenced by the climatic factors and their changes especially in Quaternary. Facies Architecture Analysis on alluvial fan deposits and layer sequences based on relative chronology showed that favorable periods for Tufa formation are on conformity to warm periods, and that deposition of conglomerates has occurred in cold periods in upper Pleistocene. Several geomorphic relics from the early Holocene warm period, Younger Dryas cold period, and warmer period between the cold periods of Iron Age and Little Ice Age have been investigated.It is important that we must wait to quik geomorphological responses to the changes resulting from the external factors in such areas. With due attention to increasing trend in temperature, at present, controlling and monitoring of hydrologic systems of the study area as well as attention to the increasing or decreasing trend of temperature and precipitation are very important.

Cites

No record.

References

Cite

APA: Copy

MOKHTARI, DAVOOD. (2010). CLIMATIC GEOMORPHOLOGY OF THE NORTHERN SLOPE OF KEYAMAKI-DAGH (NORTHWESTERN IRAN). SPATIAL PLANNING (MODARES HUMAN SCIENCES), 14(2 (66)), 163-194. SID. https://sid.ir/paper/171945/en

Vancouver: Copy

MOKHTARI DAVOOD. CLIMATIC GEOMORPHOLOGY OF THE NORTHERN SLOPE OF KEYAMAKI-DAGH (NORTHWESTERN IRAN). SPATIAL PLANNING (MODARES HUMAN SCIENCES)[Internet]. 2010;14(2 (66)):163-194. Available from: https://sid.ir/paper/171945/en

IEEE: Copy

DAVOOD MOKHTARI, “CLIMATIC GEOMORPHOLOGY OF THE NORTHERN SLOPE OF KEYAMAKI-DAGH (NORTHWESTERN IRAN),” SPATIAL PLANNING (MODARES HUMAN SCIENCES), vol. 14, no. 2 (66), pp. 163–194, 2010, [Online]. Available: https://sid.ir/paper/171945/en

Related Journal Papers