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7.0 GEOMORHOLOGICAL MAPPING

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Introduction
Geomorphological map is a map record of information on surface form, materials (soil and rock), surface processes and in some cases the age of the landforms. It provides a basis for terrain assessment. The mapping involves field documentation of the terrain with the assistance of the remote sensing facilities. In the context of environmental management, the geomorphological mapping enables the geomorphologist to obtain a better understanding of the landscape before giving advice. It provides a map record of the landscape characteristics relevant to the project in hand. In addition, it provides an essential basis for derivative and special purpose maps.

Aspects considered before starting mapping
    Scale and legend
    What should be mapped
    Availability of base maps at the required scale
    Accessibility of the area to be mapped
    How the final map is to be reproduced: Whether the map is to be printed and published in large quantities or as small number of working documents
    Need for the map to provide comprehensive or selective statement of the geomorphology

Scale
Selection of a scale depends on the details needed, purpose of the map, complexity and the dimensions of features that need to be documented. The scale to be used is normally decided by a person doing the mapping. It should be large enough to show all necessary detail but small enough to avoid an excessive number of map sheets. It also depends on the type of available remotely sensed imagery. The scale is very important to communicate the appropriate level of detail for the intended use. The presentation scale should be dependent upon the actual scale of mapping and the methods and intensity of field checking -- sometimes referred to as the Terrain Survey Intensity Level (TSIL). As the scale become smaller, larger and larger areas are shown on the same size of map sheet.  In smaller scaled maps most details are generalized and others eliminated. The details of the information mapped depend on the scale used.

The scale can be presented in verbal (eg 1cm on a map equal 100km on the ground) or using fraction (e.g. 1/5000 or 1:5000) and or bar/graphic. Because of enlargement and reduction of map size using electronic facilities, such photocopying, scanning, etc, it is advisable to be presented both in fraction and bar scales.

Categories of mapping scales as modified from Van Westen (1993):
            Synoptic or territorial scale maps (>1:50,000) are often process inventory                      maps, used by planning agencies to direct allocation of funds, develop                      emergency preparedness plans and similar tasks. An example is the overview map of the United States produced at a scale of 1:7,500,000.

            Medium scale maps (1:20,000 to 1:50,000) are generally used for preliminary or regional hazard assessments and feasibility studies, to be followed by more detailed work.

            Large-scale maps (1:5,000 to 1:20,000) are generally used for planning of land use in urban areas or resource development in rural areas. Depending on the use, large-scale maps quite often must be supplemented by detailed site investigations or on site assessments

             Detailed scale maps (1:5,000 to 1:500) are for site development, monitoring and management problems. It covers hazard assessment of a specific site and should be accurate enough to guide layout of individual structures or specific operations, or to plan mitigation. Engineering plans at these scales can also be used to derive design parameters.

Legend
The legend is the key to the map and shows how its content is organized. To find out what a map symbol stands for, look at the legend. The legend is a list of symbols used on a map, indicated by a sample symbol with an explanation showing what feature that each depicts. Each symbol should appear in the legend exactly as it looks on the map. It should be as clear and comprehensive as possible and with a minimum of complication. Symbols allow a map to show lots of information in a small space. By using symbols, maps can have more content and less clutter. The geomorphological symbols used are variables. There are no unified schemes. The symbols used vary from one country to another (Figure 7.1).


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