dc.description.abstract |
Complex geological features are predominant in some low lying sedimentary terrain,
which is the direct result of surface processes such as weathering, transportation,
sedimentation transgression, regression etc. This complex sub surface geology is mostly
seen in Dutch flood plains (polders) which belong to Quaternary Period of geological time
scale. A research study on suitability of land for development in Sliedrecht, The
Netherlands, having complex subterranean geology belonging to quaternary period was
carried out by the author (Wclideniya H.S. 1996). This type of land was not much
preferred for construction due to its complex subterranean geology, which is characteristic
with low bearing capacity. The study was aimed at developing a methodology combining
engineering geology and GIS to support urban planners in decision making |
en_US |