Editing Hydrogeology of Tanzania

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||Alluvial deposits are mainly seen in coastal delta regions and along river valleys. The coastal plain consists of largely unconsolidated sediments (beach sands, dunes and salt marsh), with some consolidated limestone deposits. Alluvium is found in river valleys. There are also volcano-pyroclastic sediments close to formerly active volcanoes.  
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||Alluvial deposits are confined to coastal delta regions and along river valleys. The coastal plain consists of largely unconsolidated sediments (beach sands, dunes and salt marsh), with some consolidated limestone deposits. Alluvium is found in river valleys. There are also volcano-pyroclastic sediments close to formerly active volcanoes.  
  
 
Borehole yields vary depending on lithology, but the greatest potential lies within the volcano-pyroclastic and alluvium deposits of the Kahe Basin and Sanya Plain near Kilimanjaro. Yields typically vary between 0.2 and 2 l/s.
 
Borehole yields vary depending on lithology, but the greatest potential lies within the volcano-pyroclastic and alluvium deposits of the Kahe Basin and Sanya Plain near Kilimanjaro. Yields typically vary between 0.2 and 2 l/s.

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