The application of coastal geomorphology studies in environmental planning, a case study (Ramsar to Tenkaben)

Number of pages: 129 File Format: word File Code: 30447
Year: 2014 University Degree: Master's degree Category: Geography - Urban Planning
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  • Summary of The application of coastal geomorphology studies in environmental planning, a case study (Ramsar to Tenkaben)

    Academic thesis for obtaining a master's degree

    Field: Natural Geography, Orientation: Geomorphology in Environmental Planning

    Abstract

    The principle of induction and the emergence of a region depends on environmental conditions and geographical location more than anything else, because natural complications and phenomena in location, dispersion, the sphere of influence of physical development, Morphology and the like have a decisive effect and sometimes act as a positive factor and sometimes as a negative and inhibiting factor. When planning for the construction of the area, the dynamism of the natural environment, such as the geomorphological forms of the area, and the factors that arise from it, such as floods, earthquakes, wind, and faults, should be considered. . and and And enough attention was paid, otherwise the city will face problems in the future. Therefore, before bitter, painful and expensive accidents occur, the officials should have the necessary concern and feel responsible during environmental planning and feel responsible, and in addition to giving importance to geomorphology studies, leave the work to experts. Of course, it goes without saying that in addition to geomorphological studies, other geographical studies are also extremely important in selecting locations and raising the level of regions, especially beaches, and environmental planning, and neglecting them will cause irreparable damage in the future. In this research, it will be tried to show that the application of coastal geomorphology studies are effective in environmental planning, and it will cause the expansion and development of tourism.

    Key words: geomorphology, environmental planning, studies, coastal geomorphology

    Introduction

    The location of settlements and other facilities created by humans is completely influenced by Environmental factors, especially geomorphology and geology. Today, according to population growth, the development of constructions is inevitable, and the adverse effect of human needs on the earth, as well as the exploitation of the surrounding areas of cities and villages to create houses and economic and industrial facilities, is increasing day by day. The industrialization of societies and the expansion of the capitalist economy have doubled the problem, and less thought and contemplation are built on the ground. This problem is more significant in developing countries due to economic constraints, and advanced technologies are still not used optimally in these regions to solve human problems or prevent their occurrence. This causes natural disasters to kill thousands of people every year and cause huge damage to the economy of these countries. Floods, earthquakes and landslides in countries like Japan and America do not cause damage like Iran and India. Geomorphology is one of the earth sciences that helps urban managers, planners and other custodians of economic and technical issues in choosing the best places for the establishment and development of settlements and other constructions. Investigating the problems related to choosing the right place to build cities, how to place buildings inside cities, the effects of city development on the surrounding land, etc. are the topics studied in geomorphology. The establishment of cities and residential areas on the earth creates new perspectives. These perspectives can be examined from different perspectives; On the one hand, the creation of these buildings causes major changes in the environment and disrupts the cycle of water, energy and materials, and on the other hand, it is affected by the natural environment. Therefore, studying and researching in the field of the natural environment where the cities are located is very important and without knowing the time and place of the cities, it is not possible to create them or it will face many problems. The construction of buildings and roads with different dimensions requires knowing the stability and stability of their location. Considering the diversity and extent of geomorphological units, the expansion of cities and the development of residential and industrial units are always affected by these units. These lands are composed of different topographical and morphological units. The more cities develop and expand, the more they deal with various topographical and geomorphological units and their related issues. Geomorphological units are always related to the dynamics and dynamism of the natural environment, any action in the direction of the development and urban development of cities somehow intersects with the said dynamics and dynamism, and as a result, morphological phenomena.In this case, if some essential principles and points are not observed, the morphodynamic balance of the environment will be disrupted and the major risks of urban equipment and facilities will be threatened. Sometimes the intensity of morphogenesis increases so much that it produces irreparable results. Many cities suffer a lot of damage from floods or at least face many problems. Some citizens are lamenting the collapse of the mountain, the flow of solifluction is taking others under the rubble. Earthquakes and earthquakes also cause the destruction of cities and towns. If some of these destructions are directly related to earthquake waves; Another important part is indirectly obtained by the intervention of geomorphological phenomena, some of which are caused by earthquakes. Therefore, the importance and necessity of knowing the characteristics of the natural environment in order to clean and identify the suitable points for creating monuments and buildings from unfavorable areas is clear. To know most of the characteristics of the natural environment, we need to study geomorphology, and it is in the shadow of gaining such knowledge that effective steps can be taken in choosing the most suitable place for the creation and expansion of cities and the creation of huge factories, and to prevent the dangers of the mentioned natural phenomena or to take serious action to deal with them. 

    Chapter 1

    -1-Statement of the problem

    In the next century, due to the increase in the earth's temperature, we will see the advance of sea water. Currently, most of the northern borders of Iran are defined by the coastal strip. Therefore, addressing the issue of coastal geomorphology as a physical and physical platform for development is considered a necessity for researchers in this field. The term coastal geomorphology has received special attention and investigation today. And due to the expansion of numerous and densely populated coastal cities in the southern margin of the Caspian Sea, in the not-so-distant future, it can play a role in the category of applied scientific knowledge, especially in environmental management. Recognizing the problem, researching and finding appropriate solutions and methods to contain, control and reduce the risks caused by natural disasters, wise planning in the optimal use of natural environments is very important. Coastal areas are among the systems that have been established in a state of balance and balance, and will enjoy stability and stability as long as this balance is not changed. Today, due to human intervention, we see the disruption of the balance conditions and the creation of unstable movements of the earth in the coastal areas. Coastal processes of the Ramsar-Tankaban route seriously threaten the geomorphological movements of the road network and other facilities. In this research, it is an attempt to study and understand these processes and movements of geomorphology, the effective causes in creating any changes from the past until now, and finally, while examining the application of coastal geomorphology, ecological power, to evaluate the unstable and stable prone points of the environment by means of a form of environmental zoning. How is the coastal geomorphology of Ramsar - Tonkaban area evaluated in environmental management? 1-3- Research objectives - Identifying the forms and processes of the coastal geomorphology of Ramsar - Tonkaban area - Preparing the zoning form of the studied area with an emphasis on geomorphological assessment. 1-4- Hypothesis. It is concluded that the investigation and evaluation of coastal geomorphological factors can be effective in planning and development infrastructure in the study area. 1-5-Limitations of the research The most important problems and limitations of this research are: Lack of sufficient scientific resources related to the study area Lack of cooperation of government organizations and centers in the field of providing information. Chapter 2 Literature review Research

    and research background

    2-1-Geomorphology

    Geomorphology is a word that has Greek roots and means knowing the shape of the earth. In fact, this science explains about the geometric shapes of the earth's surface and how they arise and the changes of these shapes in different contexts, and in this direction, it uses the concepts of various laws and knowledge. A long time has not passed since it was formulated as a law-based knowledge independent of other sciences, of course, it is not possible to make a pure separation between science and knowledge, and today the explanation of laws and theories depends on establishing the relationship between different sciences.

  • Contents & References of The application of coastal geomorphology studies in environmental planning, a case study (Ramsar to Tenkaben)

    List:

    Abstract. 1

    Introduction. 2

    Chapter One: Generalities

    1-1-Statement of the problem. 5

    1-2- Main research question (research problem) 5

    1-3- Research objectives. 5

    1-4- hypothesis. 6

    1-5- research limitations. 6

    Chapter 2 review of sources/research literature/research background

    2-1-Geomorphology. 8

    2-2- The field of geomorphology. 8

    2-3 types of geomorphology. 8

    2-3-1-Building geomorphology. 8

    2-3-2- erosion geomorphology. 9

    2-4-coastal geomorphology. 9

    2-4-1- The study areas of coastal geomorphology can be listed as follows 9

    2-4-2-Classification of landforms 10

    2-4-2-1- Domain processes. 10

    2-4-2-2- flow processes (fluid). 11

    2-4-2-3- Wind processes. 11

    2-4-2-4-structural processes. 11

    2-4-2-5-marine processes. 12

    2-4-3-effective processes in the formation of beaches. 12

    2-5- Definition of beach. 13

    2-5-1- Beach ecology. 14

    2-5-1-1- Coastal Water. 15

    2-5-1-2-Shore Line. 15

    2-5-2 types of beaches. 17

    2-5-3-The effective factors in the emergence of types of beaches are: 18

    2-5-4-Classification of types of beaches. 18

    2-5-4-1-Suess classification. 20

    2-5-4-2- Johnson's classification (Johnson 1919). 21

    2-5-4-3-Cotton's classification (Cotton 1952). 22

    2-5-4-4-Shepard's classification (Shepard 1973). 23

    2-5-4-5-Valentin's classification (Valentin 1952). 24

    2-5-4-6-Inman and Norstrom tectonic classification. 25

    2-5-4-7- Inman and Norstrom's geomorphological classification. 26

    2-6-coastal processes. 28

    2-6-1- Eddy current: (Rip currents) 28

    2-6-2- Current caused by waves: (Wave-generated currents) 29

    2-6-3- Tidal currents: (Tidal currents) 29

    2-6-4-Ocean currents (Ocean currents) 29

    2-6-5-wind-generated currents 29

    2-6-6-fluvial currents 29

    2-6-7-density currents 29

    2-7-beach landscape. 29

    2-8-Planning. 30

    2-8-1- Benefits of planning. 30

    2-8-2-key planning elements. 31

    2-8-3-Reasons for the necessity of planning. 31

    2-8-4-types of planning. 31

    2-8-4-1-types of planning in terms of implementation period 31

    2-8-4-2- in terms of location (macro, sector, regional). 33

    2-9 Climate. 37

    2-9-1- Standard deviation of basin rainfall 37

    2-9-2- Coefficient of Variation 37

    2-9-3- Monthly rainfall 37

    2-9-4- Rain erosion in the study area 38

    2-9-5- Temperature. 38

    2-9-6- thermal regime. 38

    2-9-7- Seasonal temperature regime in the study area 38

    2-9-7-1- Thermal gradient of the basin. 38

    2-10- Research background in Iran. 39

    Chapter 3 of research implementation method/materials and methods

    3-1-Introduction. 44

    3-2-data 44

    3-3-work method. 44

    3-3-1 library methods. 44

    3-3-2-field method. 45

    3-4- Geographical location and brief knowledge of. 45

    Chapter 4 data analysis and research findings

    4-1-Climatology. 49

    4-1-1- The station used in this research. 49

    4-2- Climatic classification. 50

    4-2-1- Modified Demartin method 51

    4-2-2-Coupon method. 51

    4-3- Investigation of the climatic elements of the studied area. 51

    4-3-1-Rain. 52

    4-4-Temperature 54

    4-4-1-Annual and monthly average in temperature. 55

    4-4-2-Minimum and maximum monthly temperature 56

    4-4-3-Monthly average number of freezing days. 57

    4-4-4-monthly average relative humidity of the synoptic station of the studied area 58

    4-4-5-sunny hours. 59

    4-4-6-Climatic classification of the region 60

    4-4-6-1-Genetic classification. 60

    4-4-6-2- Experimental classification. 60

    4-4-7-Climatic classification by Ivanov's method. 60

    4-4-8-climate based on classification. 62

    4-4-8-1-Climatic classification with the help of Dumarten nemogram. 63

    4-4-8-2-Climatic classification with the help of Amberge's nemogram. 64

    4-5-Geology64

    4-5- Geology of Ramsar-Tenkaben. 67

    4-5-1- Structural elements of the basin 68

    4-5-2- Joints 68

    4-5-3- Faults in the area 68

    4-5- 4- Stratigraphy of Ramsar to Tonkabon and investigation of the stability of formations and geotechnical features. 68

    4-5-4-1- Barir Complex: Barir Complex. 68

    4-5-4-2- Permian sediments. 69

    4-5-4-3- Triassic sediments. 70

    4-5-4-4-Jurassic sediments. 71

    4-5-4-5- Cenozoic sediments. 71

    4-5-4-6-Quaternary sediments. 71

    4-5-5-Geology of the Caspian Sea 72

    4-5-5-1-Width. 72

    4-5-5-2- morphology. 72

    4-5-5-3-bed deposits. 72

    4-5-5-4-Golfashans and Caspian griffons. 73

    4-5-5-5-sea currents. 73

    4-5-5-6-water temperature. 73

    4-5-5-7-water level changes. 73

    4-5-5-8-Caspian water supply sources. 74

    4-5-5-9-Pi Sang. 74

    4-5-5-10-chemical composition. 74

    4-5-5-11-Caspian hydrocarbon power. 75

    4-6-topography. 77

    4-6-1-plain areas. 78

    4-6-2- Review of the topography of the basin 78

    4-6-3- Slope. 82

    4-6-3-1- preparation of slope map. 82

    4-6-3-2-moderate slope. 82

    4-6-3-3-slope view. 82

    4-7- Vegetation. 84

    4-7-1- The role of vegetation in the study area 84

    4-7-2- The role of vegetation in soil erosion. 84

    4-7-3-vegetation of the Caspian region. 84

    4-8- Geomorphology. 86

    4-8-1-Geomorphology of the studied area 87

    4-8-1-1-Geology. 89

    4-8-1-2-Soil formation and settlement. 89

    4-8-1- 3-General description of land units. 90

    4-9- Types of soils in the region. 91

    4-9-1-brown forest soils. 91

    4-9-2-Pod Zoli soils. 91

    4-9-3-Mediterranean red and brown soils. 92

    4-9-4-Randzin 92

    4-9-5-brown forest soil type with acidic pH. 92

    4-9-6- forest brown soil type with alkaline PH. 93

    4-9-7- Coastal foothill soils of the Caspian Sea 94

    4-10-Characteristics of the coastal plains of the study area. 95

    4-10-1-Water level of rivers 95

    4-10-2-Resistance of basin rocks 95

    4-11-Hydrology. 95

    4-11-1- Hydrographic network. 95

    4-11-2- form of waterway network 96

    4-11-3- tree branch waterway network. 96

    4-11-4- Parallel waterway network. 96

    4-11-5- Determining the general arrangement of main and secondary rivers and waterways. 96

    4-11-6- Density of waterways 98

    4-11-7- Determining the bifurcation ratio. 98

    Chapter 5 discussion, conclusion and suggestions

    5-1-Conclusion. 101

    5-2-Examination of research assumptions. 104

    5-3-Proposals. 105

    Sources and sources. 106

     

    Source:

    Azadania, Rahmatullah, 1382 investigation of the relationship between precipitation and runoff in the basin of Siazande Shaft, Master thesis in Geography, Islamic Azad University of Rasht.

    Aghaizadeh, Samia, 1383, study of the climatic characteristics of the Kerganrood River and its role in erosion, Master thesis, Islamic Azad University of Rasht. Rasht.

    Arshambol et al., translated by Rajaei, Abdul Majid, 1379, documents of methods for map interpretation (geography-geology), Payam Noor Publications of Tabriz University

    Smith, Keith, translated by Moghimi Ebrahim and Guderzinejad, Shapur, 1382, Natural Hazards, Semit Publications, first edition (pp. 13, 10, 92 and 91)

    Khaldi, Shahriar, 1380, natural disasters, Shahid Beheshti University Press, first edition.

    Rafahi, Hossein Qoli, 1378, water erosion and its control, Tehran University Press, third edition.

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    Rahnomai, Mohammad Taqi, 1370, Iran's Environmental Powers, Center for Studies and Research of Urban Planning and Architecture of Iran, first edition.

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The application of coastal geomorphology studies in environmental planning, a case study (Ramsar to Tenkaben)