Document Type : Original Research Paper

Authors

1 Marine Geology Management, Geological Survey of Iran, Tehran, Iran

2 Marine & Coastal Geomorphology and Morphodynamic Group, Faculty of Geography University of Tehran, Tehran, Iran

Abstract

Coastal region are influenced by land and sea. Geomorphologic coast features are related to sea level change, regional river regime, erosion processes, sedimentation, climate change, geological outcrops and weathering and tectonics. Tom bolo, lagoon and barrier are geomorphologic coast features that can be seen in Bir coast of Iran. Therefore, recognizing the producing mechanism and their changes, leads supervisors to have better management, and do their best for civil and improving planning in coast area. In this research in addition to field studies and sampling, aerial photos 1/40000(1993), topographic maps 1/20000, high resolution images (ETM and IRS) 1998, 2005, 2008 were used. It is concluded that the area is tectonically active, sedimentation; erosion processes, river regime and sea level change are caused to the Tom bolo, Lagoon and Barrier in Bir coast. Surveying the forms, sediment shows an obvious computation between marine currents as constructive process of Tom bolo, lagoon and barrier, and rivers as destructive process in Bir coast.

Keywords

References
Bird, E., 2008- Coastal geomorphology an Introduction, university Mel born, Australia Johnwiley and Sons.
Flinn, D., 1997-The role of wave diffraction in the formation of St. Ninian's Ayre (tombolo) in Shetland, Scotland. Journal of Coastal Research, 13(1),2028.
 Kirk, R. M., 2000- Significant coastal lagoon systems in the South Island, New Zealand Department of ConservationP.O. Box 10-420 Wellington, New Zealand.
Kjefve, B. (Ed.), 1994- Coastal lagoon Processes. Elsevier Oceanography Series 60.557 p.
Little, R. D., 1970- Terrces of the makran of Iran,in sneed report.
Martin, L. & Landim, J. M., 2000- Coastal lagoons Elsevier Oceanography Series 60.
Nichols, M. N. & Boon, J. D., 1994- Sediment transport processes in coastal lagoons Elsevier Oceanography Series 60. ch 7 ,pp.157 – 220.
Saranthein, M. & Walger, E., 1973- Classification of Modern  marl Sediment in the Persian Gulf by Factor analysis  In: B.A. Purser, The Persian Gulf, Springer-Verlag p.81-97
Schwartz, M. L. (Ed.), 1973- Barrir Islands. Dowden, Hutchinson and Ross,Strousburg,PA.
Shpard. F. P., 1973- Submarine Geology. Harper and Rows, New York.
Smite, N. P., 1973- coastal lagoons Elsevier Oceanography Series 60.
 Smith, J., 1993- The Houb, Dales Voe: coastal processes. In Shetland Isles (eds J. Birnie, J.Gordon, K. Bennett and A. Hall), Quaternary Research
Snead, R. E., 1970- Physical Geography of the Makran Coastal Plain of Iran, Springfield, VA: National Technical Information Service, US Department of Commerce, Publication AD707745.
Tuker, M. E. (Ed.), 1988- Techniques in sedimentology. Blackwells, Oxford, 394 pp.
Vitafenzi, C., 1979- Contribution to be Quaternary Geology of Southern of Iran. Geological and Mineral of Survey of Iran, Report,27:30-38.