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The study area contains elements of pine, casuarina and eucalyptus.
The study area contains weak, wet soils that experience land sliding regularly even without significant seismic activity.
The HBG and charnockites present in the study area contains mica, quartz, calcite and feldspar.
The delta front in the study area contains three types of sand bodies.
The study area contains buried faulted structure below the Quaternary cover, Separated by broad synclines (Buday and Jassim 1987).
The eastern part of the study area contains a fresh water aquifer, but the southern part overlies a salt water aquifer.
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The study area contained 164 tree species, but few were shared by the three landscape types and none by 30 communities.
The study area contained ancient deciduous woodlands mainly consisting of Quercus spp., Fagus sylvatica and Carpinus betulus in the Gaume, an area with a mild temperate climate in southern Belgium.
Group A oils predominately occurred in the northwestern part of the study area contain relatively high amounts of gammacerane and C35 hopanes with the ratio of gammacerane to C30 hopane (G/H) > 0.7 and the C35/C34 hopane ratio (C35/C34) > 1.2.
We used a digitised map of the study area containing shapefiles of all the habitats including 82 patches of calcareous grassland together with management information for each patch and data on the presence and abundance of a range of calcareous grassland indicator plant species.
The Middle Miocene fissured limestone is considered the sole aquifer in the study area containing groundwater under perched conditions.
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