Page 127 - Geochemical Anomaly and Mineral Prospectivity Mapping in GIS
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             Fig. 5-5. Spatial data  and sequential steps involved  in creation of stream sediment sample
             catchment basins. (A) Digital elevation model  (DEM) created  either manually from analogue
             topographic elevation data or automatically from digital topographic elevation data. (B) Stream
             networks (black lines) digitised from analogue topographic maps or delineated automatically from
             a DEM. (C) Stream sediment sample locations (small white dots) are used as references in further
             processing of digital stream networks to indicate points to which overland water flows. (D) DEM
             and processed  digital streams are used as input data in spatial neighbourhood algorithms for
             automatic delineation of sample catchment basins (in white outlines).


                A DEM can be used for automatic determination of stream networks (e.g., Martz and
             Garbrecht, 1993) instead of digitising streams from a topographic map. Digitised streams
             are  processed  further to indicate stream sediment sample locations as  points toward
             which water flows from different points on topographic surfaces represented by a DEM.
             The  DEM and the processed  digital streams are then  used via certain spatial
             neighbourhood algorithms to create automatically sample catchment basins. Detailed
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