Editing Hydrogeology of Sudan

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|Erde Ente, Nawa Formation, sedimentary rocks of NW Sudan
 
|Erde Ente, Nawa Formation, sedimentary rocks of NW Sudan
 
||Cambrian to Carboniferous
 
||Cambrian to Carboniferous
||Relatively small outcrops of unmetamorphosed sandstones of Palaeozoic age occur in the west of Sudan, along the Chad border.  
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||Outcrops of unmetamorphosed sandstones occur in the west of the country, along the Chad border.  
  
Argillaceous Palaeozoic sedimentary rocks overlie Precambrian basement in central Kordofan.  
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Argillaceous sedimentary strata overlie the basement complex in central Kordofan.  
  
Silurian strata, largely fluvial-deltaic sandstones, occur in northwestern Sudan (UN 1988).  
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Silurian deposits, alrgely fluvial-deltaic sandstones (UN 1988) occur in northwestern Sudan.  
  
 
Devonian and Carboniferous rocks, including the Nawa Formation, occur around Uweinat, Sudan. They consist mainly of sandstones with schists (UN 1988).  
 
Devonian and Carboniferous rocks, including the Nawa Formation, occur around Uweinat, Sudan. They consist mainly of sandstones with schists (UN 1988).  

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