Investigating geomorphological limitations in the physical development of Bandar Anzali city

Number of pages: 139 File Format: word File Code: 30425
Year: 2014 University Degree: Master's degree Category: Geography - Urban Planning
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  • Summary of Investigating geomorphological limitations in the physical development of Bandar Anzali city

    Academic Thesis for Master's Degree

    Field: Natural Geography, Major: Geomorphology in Environmental Planning

    Abstract

    The present research using the descriptive and analytical method and the use of documentary and library methods and field observations to investigate the geomorphological limitations in the physical development of Bandar Anzali city and identify and introduce its damaged areas. has paid; Because the physical development of cities is generally directly related to the natural bed and geomorphological effects. Therefore, according to these goals, the following results were obtained: Anzali port, the second most populous city in Gilan province, with a population of more than 100,000 people, is bounded linearly from the north to the Caspian Sea for about 15 kilometers and from the south to the Anzali wetland, and the waterway that connects the sea and the wetland has divided the city into two eastern (Ghazian) and western (Anzali) parts. The advance of the Caspian Sea water and, as a result, the Anzali Wetland has caused a lot of damage to the city from both sides in the last decade. So that the Supreme Council of Urban Planning and Architecture of Iran decided to think of a solution to solve this problem. Finally, it was decided that the 24-meter horizontal line (height above the surface of open water) is considered as the edge of the sea and any construction beyond this figure is prohibited, except for light and temporary facilities. Based on this resolution, it was decided to build the city's vital infrastructure facilities above -22 meters and allow residential uses and other related services to be built up to -24 meters. Based on this, about 50% of the area of ??Bandar Anzali city is considered unsafe and nearly 29 thousand people living there should be moved to safe places. The limits of the city's development are in the north of the Caspian Sea and in the south of the Anzali Wetland and the lowlands and water bodies that do not provide any possibility for development. In addition, the rise of the sea level during the past years has destroyed or threatened a major part of the city. Based on this, it seems that the most suitable lands for the development of the city in order to have safe height codes (number above -24 meters) are in the eastern direction, i.e. along the Anzali road to Rasht, and in the western direction, i.e. around the communication axis between Anzali and Astara. But this possibility will bring its own consequences due to the more linearization of the city fabric and will increase the costs of the city's infrastructure services. Therefore, the above areas cannot be used. The most appropriate way to accommodate the population and provide the required service spaces is to use the empty city tissues and existing land and to increase the building and population densities in the existing tissues. Therefore, the most important geomorphological limitations in Anzali city are two natural factors, Anzali Marsh and Caspian Sea, both of which are very effective in the development of Anzali city. Of course, the changes in coastlines and geomorphological forms created in these areas have also caused the lack of physical development of this city.

    Key words: limitation, geomorphology, physical development, Bandar Anzali city

    Introduction

    The city of Bandar Anzali is bounded from two geographical directions (from the north by the sea and from the south by the Bandar Anzali wetland), for its physical development, it inevitably moves towards It moves in the east and west directions around itself. During this process, in the last half century, four villages from the immediate outskirts of the city have become victims of the spatial development of the city and have been integrated into it. The high population density of Bandar Anzali city and its lack of land have led to the physical development of the city, which creates changes in the land around the city. These developments have led to changes in the use of rural and agricultural lands and gradually a large area of ??land has been allocated to constructions. As the only urban point in the city, the city of Bandar Anzali has become a center of attraction for the immigrant population, and this process has faced the city with an increase in population and a decrease in land during the last century. Villages such as Susar Nuvir and Waqar in 1365 and the villages of Shalor Kollivar in 1375 were integrated into it during the city's creeping process. Also, the villages of Bashman and Talebabad, which are located on the immediate outskirts of the city, are not exempted from this rule and have been attacked by the construction of the city and have become the settlement of its population. In this way, the land area of ??the villages has been reduced and by turning into urban structures, they have been integrated into the urban area. In fact, with its horizontal growth, the city moves towards the peripheral villages and dissolves the rural lands in itself, and with the passage of time, the villages are completely covered by the city.In fact, with its horizontal growth, the city moves towards the peripheral villages and dissolves the rural lands in itself, and with the passage of time, the villages are completely swallowed by the city. Population density, lack of land, inevitably lead the city to develop towards the surrounding lands. Therefore, according to the existence of two natural factors, namely the sea and the marsh, and the forms of geomorphology created in the coastal areas, this research investigates the geomorphological limitations in the physical development of Bandar Anzali city, and is divided into the following five chapters:

    Chapter One: Research Overview;

    Chapter Two: Review of Sources, Research Literature, and Research Background;

    Chapter Three: Research Implementation Method, Materials and Methods;

    Chapter four: analysis of data and research findings;

    Chapter five: evaluation of hypotheses, discussion and conclusions and suggestions.

    Abstract

    The present research uses descriptive and analytical methods and the use of documentary and library methods and field observations to investigate geomorphological limitations in the physical development of Bandar Anzali city and to identify and introduce areas The victim has paid it; Because the physical development of cities is generally directly related to the natural bed and geomorphological complications. Therefore, according to these goals, the following results were obtained: Anzali port, the second most populous city in Gilan province, with a population of more than 100,000 people, is bounded linearly from the north to the Caspian Sea for about 15 kilometers and from the south to the Anzali wetland, and the waterway that connects the sea and the wetland has divided the city into two eastern (Ghazian) and western (Anzali) parts. The advance of the Caspian Sea water and, as a result, the Anzali Wetland has caused a lot of damage to the city from both sides in the last decade. So that the Supreme Council of Urban Planning and Architecture of Iran decided to think of a solution to solve this problem. Finally, it was decided that the 24-meter horizontal line (height above the surface of open water) is considered as the edge of the sea and any construction beyond this figure is prohibited, except for light and temporary facilities. Based on this resolution, it was decided to build the city's vital infrastructure facilities above -22 meters and allow residential uses and other related services to be built up to -24 meters. Based on this, about 50% of the area of ??Bandar Anzali city is considered unsafe and nearly 29 thousand people living there should be moved to safe places. The limits of the city's development are in the north of the Caspian Sea and in the south of the Anzali Wetland and the lowlands and water bodies that do not provide any possibility for development. In addition, the rise of the sea level during the past years has destroyed or threatened a major part of the city. Based on this, it seems that the most suitable lands for the development of the city in order to have safe height codes (number above -24 meters) are in the eastern direction, i.e. along the road from Anzali to Rasht, and in the western direction, i.e. around the communication axis between Anzali and Astara. But this possibility will bring its own consequences due to the more linearization of the city fabric and will increase the costs of the city's infrastructure services. Therefore, the above areas cannot be used. The most appropriate way to accommodate the population and provide the required service spaces is to use the empty city tissues and existing land and to increase the building and population densities in the existing tissues. Therefore, the most important geomorphological limitations in Anzali city are two natural factors, Anzali Marsh and Caspian Sea, both of which are very effective in the development of Anzali city. Of course, the changes in coastlines and geomorphological forms created in these areas have also caused the lack of physical development of this city.

    Key words: limitation, geomorphology, physical development, Bandar Anzali city

    Introduction

    The city of Bandar Anzali, due to being enclosed from two geographical directions (from the north by the sea and from the south by the Bandar Anzali wetland), for its physical development, inevitably moves towards It moves in the east and west directions around itself. During this process, in the last half century, four villages from the immediate outskirts of the city have become victims of the spatial development of the city and have been integrated into it. The high population density of Bandar Anzali city and its lack of land have led to the physical development of the city, which creates changes in the land around the city. These developments have led to changes in the use of rural and agricultural lands, and gradually a large area of ??land has been allocated to constructions. As the only urban point in the city, the city of Bandar Anzali has become the center of attraction for the immigrant population, and this process has faced the city with an increase in population and a decrease in land during the last century.

  • Contents & References of Investigating geomorphological limitations in the physical development of Bandar Anzali city

    List:

    Abstract 1

    Introduction. 2

    ? The first chapter: general research.  3

    1-1. State the problem. 4

    1-2. The importance and necessity of research. 5

    1-3. Research objectives. 5

    1-4. Research question. 6

    1-5. Research hypothesis. 6

    1-6. Research method. 6

    1-6-1. Method of collecting information. 6

    1-6-2. Information gathering tool. 7

    1-6-3. Information analysis method. 7

    1-7. Scope of research. 7

    1-8. Words and concepts. 9

    1-9. Research problems, limitations and obstacles. 10

    ? The second chapter: review of sources, research literature and research background.  9

    2-1. Morphology. 12

    2-2. Geomorphology. 12

    2-3. The importance of geomorphological studies in urban planning. 13

    2-4. The role of geomorphology in coastal planning. 14

    2-5. Geomorphic planning. 14

    2-6. Environmental management. 15

    2-7. Contribution of geomorphology in environmental management. 15

    2-8. Characteristics of watersheds in lowland areas. 16

    2-9 problems of coastal areas. 17

    2-10. Geomorphological factors limiting coasts. 17

    2-10-1. waves 17

    2-10-2. Sea currents. 18

    2-11. How to form a sea. 19

    2-12. crater bay 19

    2-13. Delta 19

    2-14. Forms of accumulation of sedimentary materials resulting from the impact of destructive waves. 19

    2-15. Effects of sea level levels in the Quaternary. 20

    2-15-1. The nature and quality of Quaternary climatic changes and its morphological evidence. 20

    2-15-2. Neogene climatic conditions. 22

    2-15-3. Climatic changes of the fourth era in terms of natural geography and geomorphology. 23

    2-15-4. Quaternary climatic changes in Iran and its morphological evidence. 23

    2-15-5. Plovyal lakes of Iran. 24

    2-16. The concept of urban development. 24

    2-17. The boundaries of the city. 25

    2-18. Geographical indicators in the spatial sustainable development of the city. 25

    2-18-1. Natural geography factors. 26

    2-18-1-1. Geographical location. 26

    2-18-1-2. Topography. 27

    2-18-1-3. slope 27

    2-18-1-4. climate 28

    2-18-1-5. soil and water 28

    2-18-1-6. Vegetation. 30

    2-18-1-7. geology 31

    2-18-1-8. Geomorphology. 31

    2-18-2 Social factors. 31

    2-19. Research background. 33

    ? The third chapter: research implementation method, materials and methods.  39

    3-1. Research implementation method. 40

    3-1-1. Analytical method. 40

    3-1-2. Descriptive method. 40

    3-2. Materials (required data) 41

    3-2-1. Zoning of annual rainfall at the level of the studied area. 42

    3-2-2. Maximum daily rainfall. 44

    3-2-3 number of days with zero or more rainfall. 46

    3-2-3. The number of days with rainfall of 1 mm or more. 47

    3-2-4 number of days with rainfall of 5 mm or more. 47

    3-2-5 number of days with rainfall of 10 mm or more. 48

    3-2-6. The direction and speed of the prevailing wind. 49

    ? Chapter four: data analysis and research findings.  52

    4-1. Geographical location. 53

    4-2. Natural features of Anzali port. 54

    4-2-1. geology 54

    4-2-2. Topography. 57

    4-2-3. climate 59

    4-2-3-1. temperature 59

    4-2-3-2. rainfall 61

    4-2-3-3. Relative humidity. 62

    4-2-3-4. Abernaki 63

    4-2-3-5. sunny hours 64

    4-2-3-6. Ice days. 64

    4-2-3-7. Wind direction and speed. 65

    4-2-4. Water resources. 67

    4-2-5. Soil science 70

    4-2-6. Vegetation. 71

    4-3. A look at some features of the Caspian Sea. 74

    4-3-1. Weather 75

    4-3-2. Geology and tectonics. 76

    4-3-3. Caspian Sea water supply sources. 77

    4-3-4. Bays, islands and ports. 79

    4-3-5. Past climatic conditions and the reflection of climate changes on coastal geography. 79

    4-3-6. The relationship between climate change and Caspian Sea water level fluctuation. 80

    4-3-7. Changes in the level of the Caspian Sea. 81

    4-3-8. Factors affecting the fluctuation of Caspian Sea water. 91

    4-4. Investigating the changes of coastlines in Gilan province. 91

    4-5. Investigating the evidence of geomorphology in the coastsInvestigating the evidence of geomorphology in Anzali beaches. 92

    4-5-1. Geomorphological limiting factors in Anzali port. 93

    4-5-1-1. Transverse dunes Qts. 93

    4-5-1-2. Sand dunes. 94

    4-5-1-3. Qal1 river alluvial sediments unit. 97

    4-5-1-4. Remaining dam sediments (natural sediments) QaL2 river. 98

    4-5-1-5. Qsp free sand areas. 98

    4-5-1-6. Marsh and lagoon. 98

    4-5-2. Evidences of Caspian Sea advance to the land. 100

    4-5-2-1. The condition of the beach in Anzali region. 100

    4-5-2-2. The general situation of the advance on the coastlines. 106

    4-6. Coastal areas in Anzali city. 107

    4-7. The effect of wind in creating geomorphological forms. 108

    4-8. Effect of Caspian Sea water level fluctuations. 109

    4-9. The effect of sea level changes in the Sahel region. 110

    4-10. Obstacles and limitations of the development of Anzali city. 111

    4-10-1. How to settle the city based on the height figure. 113

    4-10-2. How to use land in the city. 114

    ? The fifth chapter: hypothesis evaluation, conclusions and suggestions.  115

    5-1. Evaluation of hypotheses 117

    5-2. Discussion and conclusion. 118

    5-3. Suggested solutions. 123

    List of sources and sources. 124

    English abstract.  138

     

    Source:

    Ahmadi, Hassan and Peymanifard, Bahram and Kausar, Seyed Ahang and Mahdavi, Mohammad, 1380, Culture of Agriculture and Natural Resources, Volume 12 (Pasture and Watershed), First Edition, Tehran, University of Tehran Publications

    Azad, Mansour, 1372, Causes of Caspian Sea Water Level Rise and Its Progress On the coast, Gilan Islamic Guidance Center

    Espehbad, Mohammad Reza, 1384, Metatectonic changes and water level fluctuations of the Caspian Sea with a special look at Qarabaghaz Gol Bay from satellite images, 21st Earth Sciences Meeting).

    Amini, Ali, 1371, classification of seas and lakes based on factors affecting water level changes, collection of articles of the Gilan Province Planning and Budget Organization

    Bahrini, Seyyed Hossein and Moghads Khorasani, Abolqasem, 1386, limits of urban development in Anzali, SID site

    Analysis of water level changes of the Caspian Sea, 1375, Statistical Plan and Program Center of the General Directorate of Shipwreck Ports Gilan

    Sabet Ahed Jahormi, Abdul Reza et al., 1384, investigation of wave breaking and currents along the coast caused by it in the southern shores of the Caspian Sea (between Anzali and Kianshahr), 6th conference of marine sciences and techniques

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    Darvishzadeh, Ali, 1382, Geology of Iran, Amirkabir Publications

    Dehkhoda, 1377, Dehkhoda Dictionary, Amirkabir Publications

    Diseh, Jahangir, Keshavarzanzadeh, Zahra, 1384, Atlas report of geomorphological investigations and coastal natural features of Bandar Anzali, 6th conference of marine sciences and techniques

    Rasakh, Rehane, 1391, Survey of the environmental capabilities of the central coasts of Gilan province in order to plan integrated management, master's thesis in Department of Natural Geography, Geomorphology in Environmental Planning, Islamic Azad University, Rasht Branch, under the guidance of Dr. Mohammad Reza Afshari Azad. Caspian Sea (Baku, September 15-21, 1990), Caspian Sea Water Fluctuations, Gilan Province Program and Budget Organization's collection of articles

    Zadsar, Hadi et al., 2008, Geomorphological survey of Caspian Sea coasts and a perspective on the water level fluctuations of this sea, (Geological Scientific Association of Islamic Azad University, Sari branch).

Investigating geomorphological limitations in the physical development of Bandar Anzali city