THE ROLE OF EXTERNAL DYNAMIC PROCESSES IN MORPHOGENESIS OF TALESH MOUNTAINS

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.

TAHOUNI P.

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

Journal Paper

Paper Information

Journal: GEOGRAPHICAL RESEARCH QUARTERLY Year:2005 | Volume:36 | Issue:50 Page(s): 49-73

Download Full-Text

Persian Verion

View:

953

Download:

Cites:

Information Journal Paper

Title

THE ROLE OF EXTERNAL DYNAMIC PROCESSES IN MORPHOGENESIS OF TALESH MOUNTAINS

Author(s)

TAHOUNI P. | Issue Writer Certificate

Keywords

MECHANICAL WEATHERINGQ2

CHEMICAL WEATHERINGQ4

ROCK FALLQ3

LANDSLIDEQ4

SOLIFLUCTIONQ2

Abstract

Variety is the inherent characteristic of our country. Geomorphologic studies leads us to use natural environment in its logical and optimized way, by finding reasons for physical environment variety, and this helps us by recognition of stable and unstable areas and identification of the type of the activities.Being mountainous, sharp declivity slopes, active faults, high average of rainfall, variation of temperature in high elevations, rich vegetation and existence of permanent rivers with high yearly discharge are considered as the physical characteristics of the investigated area. Talesh mountain erosion activity divides into two neighbor regions. First, subglacials over 2000m altitude including superiority of mechanical functions, overcoming of morphogenesis on pedogenesis , and Second, frost region which starts form the lowest border of subglacial region and extends to the hillside by hegemony of physico-chemical activities and the overcoming of pedogenesis on morphogenesis. In this region, LANDSLIDE is the most geomorphological phenomena, which emanates from human mismanagement and highly influences mountains sensitive and unstable circumference and finally results economical and natural damages. Rivers erosion system is an active morphogenesis system and the most important factor of sediment transportation. Young rivers have a highly effective erosion activity at the bottom of V-shaped valleys-which erodes bedrock and shapes the shore by its transportation.

Cites

No record.

References

Cite

APA: Copy

TAHOUNI, P.. (2005). THE ROLE OF EXTERNAL DYNAMIC PROCESSES IN MORPHOGENESIS OF TALESH MOUNTAINS . GEOGRAPHICAL RESEARCH QUARTERLY, 36(50), 49-73. SID. https://sid.ir/paper/5565/en

Vancouver: Copy

TAHOUNI P.. THE ROLE OF EXTERNAL DYNAMIC PROCESSES IN MORPHOGENESIS OF TALESH MOUNTAINS . GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2005;36(50):49-73. Available from: https://sid.ir/paper/5565/en

IEEE: Copy

P. TAHOUNI, “THE ROLE OF EXTERNAL DYNAMIC PROCESSES IN MORPHOGENESIS OF TALESH MOUNTAINS ,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 36, no. 50, pp. 49–73, 2005, [Online]. Available: https://sid.ir/paper/5565/en

Related Journal Papers