Erosion Landform ( 12. Lavaka )


                                                                                                                                                      Back to Erosion Landform 

  • Lavaka meaning  for hole with steep sides.
  • The side of a hill is a type of erosional feature common in;

                               Madagascar
                               Democratic Republic of the Congo
                               South Africa
                               Brazil
Active lavaka on right, with inactive, largely infilled older lavakas to left
Active lavaka on right, with inactive, largely infilled older lavakas to left

  • They are most abundant in the Central Highlands.
  • Approximately 1m thick laterites.
  • Develop on steep terrains in a monsoonal climate.
  • Lavakas form  hard laterites overlie thick saprolite.
  • Steep 35 - 55 degree slopes.
  • That areas are;

                         hot in dry season 
                         warm in wet season
  • Lavakas are not landslides.
  • They are a type of gully.
  • Formed via groundwater sapping.
  • Associated erosion is usually rapid.
  • Producing a sediment yield (8,000 cubic metres) over several months.


  • Human activities contribute to lavaka formation such as;

                                         -Deforestation
                                         -Overgrazing
                                         -Road creation
                                        -Grassland burning
  • Lavakas are caused by natural processes.
  • Some lavakas are 20,000 years old.




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