Digital Elevation Model (DEM) is a powerful tool associated with GIS. The easiest way to construct DEM was to use a Triangular Irregular Network (TIN). TIN was constructed by using contour layer which has been developed by the Department of Survey, Sri Lanka at the scale of 1: 50,000. Degree slope, percent slope and elevation surfaces were extracted from the TIN model and were converted into 25 m square raster layers. The procedure is shown in the Fig. 3.2
Modeling of watershed and stream order
Terrain, stream network and boundary of study maps are used as the input coverage layers. The topogrid function in Arc Info software which is an interpolation method, specially designed to generate hydrologically corrected DEM [Graves, 2001], was used to produce digital elevation model as a grid with spacing 25 m. This DEM was corrected by sink filling and it was used to generate flow direction grid and flow accumulation grid. The procedure is shown in the Fig. 3.3. Finally constructed a watershed cover and it was cleaned and build in arc info for generate the geometrical parameters. This coverage was used to create the final watershed grid for hazard mapping.
A major part of the hill country of Sri Lanka forms important watersheds and their degradation would cause irreparable damage to land and water recourses including the occurrence of major landslides. Therefore it is an important area to use for landslides hazard zone mapping. The land use map developed in 1: 50,000 scales was used to model land use pattern in study area. The systematic categorization of land use type is shown in Table 3.1 and used to prepare the derived map of land use pattern in study area.
Fig. 3.3: Modeling of watershed
Table 3.1: Classification of land use
Classification Category
River 3
Streams 3
Canal 3
Irrigation canal 3
Reservoir 3
Tank 3
Inland water bodies 3
Built-up land 1
Associated non-agricultural area 2
Homesteads 2
Tea 2
Rubber 2
Coconut 1
Other crop land 3
Paddy 1
Sparsely used crop 3
Chena 3
Mixed tree and other crops 1
Dense forest 1
Open forest 2
Forest plantation 1
Scrubland 2
Grassland 3
Marsh & swamps 1
Barren land 3
Abandoned paddy 1
Aquatic farms 1
The risk of landslide increases in areas around reservoirs. Therefore it is a significant factor to consider hazard zone mapping. Reservoir layer buffer for 500 m and 1000 m to get influenced area of reservoir and converted to grid layer.
Stream density is also affecting the instability of slopes. Stream density value was derived for each 25 m cell from stream network layer.