INTERACTION AND CONSEQUENCIES
Once defined the active portion of the hidrographyc network within the active altimetric band of a generic basin we could analyze first the interaction with other processes and then with infrastrucutres.
In the first case we take as sample the mass movements and we represent these processes in a GIS context using raster data so as the hidrographyc network.
Both the hidrography and the gravitational processes are represented in terms of pixels so as is represented in the pictures that follow.
We count the numebrs of pixels employed to represent hidrography or mass movements at the different altitudes so to compare the two processes along the same direction using the same criteria.
FIG_1: HYDROGRAPHIC NETWORK DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA.
FDC
FIG_2: MASS MOVEMENTS DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA.
FIG_3: MASS MOVEMENTS AND HYDROGRAPHIC NETWORK DEVELOPMENTS OVERLAPED ALONG THE VERTICAL DIRECTION WITHIN THE INVESTIGATED BASIN.
FIG_4: ROADS NETWORKS Ā DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA.
FIG_5: MASS MOVEMENTS DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA OVERLAPED TO ROADS NETWORKS DEVELOPMENT.
FIG_5: HYDROGRAPHIC NETWORK DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA OVERLAPED TO ROADS NETWORKS DEVELOPMENT.
FIG_5: HYDROGRAPHIC NETWORK DEVELOPMENT ALONG VERTICAL DIRECTION EXPRESSED IN TERM OF PIXELS USING RASTER BASE DATA OVERLAPED TO ROADS NETWORKS DEVELOPMENT AND MASS MOVEMENTS DEVELOPMENT.