(2)Terrain data is commonly regarded as the most important basis for most of geo-analysis. However, the automatic depiction of earth’s relief is one of the most difficult tasks in GIS. The earth’s surface is an irregular three-dimensional continuum, then it is impossible to be fully defined and fully depicted with an infinite number of points only. DEMs are a means of terrain representation in which elevation is recorded at specific horizontal positions. Burrough (1986) defines DEM as “Any digital representation of continuous variation of relief over space”. The methods are needed to capture and store elevation data over intermediate or large areas. DEMs can be grouped into the following basic approaches: regular grids (raster), triangulated irregular networks (TIN) and contours. Each has its advantages and limitations in different applications, but raster based on DEMs has got more popularity in applications.