ANZALI WETLAND AND MORPHOLOGICAL CHARACTERISTICS OF THE IMPACT OF CHANGES IN LAND USE

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RANJBAR MOHSEN

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Journal Paper

Paper Information

Journal: GEOGRAPHICAL JOURNAL OF TERRITORY Year:2012 | Volume:9 | Issue:34 Page(s): 93-111

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Title

ANZALI WETLAND AND MORPHOLOGICAL CHARACTERISTICS OF THE IMPACT OF CHANGES IN LAND USE

Author(s)

RANJBAR MOHSEN | Issue Writer Certificate

Keywords

CHANGEQ2

COASTAL ZONE MORPHOLOGYQ3

LAND USEQ1

WETLANDS ANZALIQ2

CASPIAN SEAQ2

Abstract

Caspian basin after being removed from the open seas or lakes in Pliocene time, money and since then a series of tectonic activity, fluctuating water levels, the effect of waves and currents of the river morphology and current as it created. Sediments along the shoreline to erosion and sedimentation caused severe CHANGEs in morphology are Anzali wetland. Morphological forms based on the manufacturer and type deposits occur in different environments. Recognizing symptoms and morphological CHANGEs that could be a pivotal role in coastal planning and coastal management have. Swamps and wetlands, Delta, tab, sand, sandy zones, sand dunes, marine terraces and flood plains, mud zones, alluvial Fans, landscape morphology are observed in different parts of the CASPIAN SEA and Anzali Wetland. Current status of the beach about 10 thousand years ago with the general trend of lowering the water levels is. In recent decades, human factors, the coast is one of the basic parameters of the deformation. Margin morphology can identify shifts in the development and landuse planning coastlines, coastal areas to be effective. In this research, studies, documents and software using Ilwis, Autocad and photoshop and aerial photographs, geological maps, topographic1/ 20000 and 1/50000 and a method based on RS and GIS methods to separate the units in the sedimentary environment they have been marked And the resulting CHANGEs in the rate of water level CHANGEs and coastal morphology and sedimentary units, replacement of the final maps will be prepared. Anzali wetland in coastal sediments of the tab is made up of coastal and coastal barriers. Anzali lagoon behind the beach is one of the lakes that were once part of the CASPIAN SEA coastal waters. Anzali wetland in the past had a large spread but gradually by alluvial sediments-Sefidrood deltaic branches and rivers of Rasht region, Masal and Fouman is filled. Anzali indentation tectonics is derived from the CASPIAN SEA backward somewhat isolated from the sea and sand with a blade (the area between Anzali and Kapurchal) is formed. Facies of Pleistocene marine and coastal areas indicates the presence of Pleistocene Sea coast at the foot of the Alborz. Gradually with the gradual retreat of the sea and tectonic activity has increased the extent of the coastal plain. Coastal facies, especially along the asphalt road protrusion City-Friday Market (Friday Market on the northern side reached a three-way road) that is visible is located in the south of Anzali wetland.

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APA: Copy

RANJBAR, MOHSEN. (2012). ANZALI WETLAND AND MORPHOLOGICAL CHARACTERISTICS OF THE IMPACT OF CHANGES IN LAND USE. GEOGRAPHICAL JOURNAL OF TERRITORY, 9(34), 93-111. SID. https://sid.ir/paper/116176/en

Vancouver: Copy

RANJBAR MOHSEN. ANZALI WETLAND AND MORPHOLOGICAL CHARACTERISTICS OF THE IMPACT OF CHANGES IN LAND USE. GEOGRAPHICAL JOURNAL OF TERRITORY[Internet]. 2012;9(34):93-111. Available from: https://sid.ir/paper/116176/en

IEEE: Copy

MOHSEN RANJBAR, “ANZALI WETLAND AND MORPHOLOGICAL CHARACTERISTICS OF THE IMPACT OF CHANGES IN LAND USE,” GEOGRAPHICAL JOURNAL OF TERRITORY, vol. 9, no. 34, pp. 93–111, 2012, [Online]. Available: https://sid.ir/paper/116176/en

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