GEOMORPHOLOGIC EIDENCE OF THE PLEISTOCENE GLACIER EROSION IN THE TALESH HIGHLANDS

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.

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

Journal Paper

Paper Information

Journal: GEOGRAPHICAL RESEARCH QUARTERLY Year:2004 | Volume:36 | Issue:47 Page(s): 31-56

Download Full-Text

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

Persian Verion

View:

1,932

Download:

Cites:

Information Journal Paper

Title

GEOMORPHOLOGIC EIDENCE OF THE PLEISTOCENE GLACIER EROSION IN THE TALESH HIGHLANDS

Author(s)

TAHOUNI P. | Issue Writer Certificate

Keywords

PLEISTONCENQ4

GLACIER EROSIONQ3

CIRQUESQ4

GLACIAL VALLEYSQ3

ERRATIC BLOCKQ2

MORAINSQ4

SNOW-LINEQ4

Abstract

The Talesh mountains consist of a variaty forms resulted form GLACIER EROSION. The action of dynamic morphogenes depends on the climatic conditions, but the present climatic conditions do not allow these forms to be built, therfore, the existence of such forms is emphasising a change in climatic situations and, as a result, a change in morphogenes system in this part of our country. Due to the immunity of these forms to erosion, the time of their formation dates back to the global pleistocence climatic changes. Recognition of these forms happened though aerial potograph the area cover topographic maps and area abservation. Recognizing the source of sediments was done throug their sampling and analysis. The geomorphologic investigated evidence in this research consist of CIRQUES, glacial valleys, ERRATIC BLOCK, MORAINS, and the ice-eroded surface. The average snow-line resulted form this research for the Talesh Mountains was caluclated to be 2360 meters but due to their neighbouring with caspian sea, some location-related factors have caused some variations in the altitude of snow-line in a way that the snow-line altitude in the east side was calculated to be 1800 meters, south side to be 2400 meters and west side to be 2900 meters. The morphogenes of the Talesh Mountions was done through two systems of glacierand sub-glacier erosion during the cold periods of pleistocene.

Cites

References

Cite

APA: Copy

TAHOUNI, P.. (2004). GEOMORPHOLOGIC EIDENCE OF THE PLEISTOCENE GLACIER EROSION IN THE TALESH HIGHLANDS. GEOGRAPHICAL RESEARCH QUARTERLY, 36(47), 31-56. SID. https://sid.ir/paper/5606/en

Vancouver: Copy

TAHOUNI P.. GEOMORPHOLOGIC EIDENCE OF THE PLEISTOCENE GLACIER EROSION IN THE TALESH HIGHLANDS. GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2004;36(47):31-56. Available from: https://sid.ir/paper/5606/en

IEEE: Copy

P. TAHOUNI, “GEOMORPHOLOGIC EIDENCE OF THE PLEISTOCENE GLACIER EROSION IN THE TALESH HIGHLANDS,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 36, no. 47, pp. 31–56, 2004, [Online]. Available: https://sid.ir/paper/5606/en

Related Journal Papers