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From Chalo Chatu, Zambia online encyclopedia
  • ...s a name used for the escarpments forming both sides of the rift valley or graben in which lie the middle [[Zambezi river]] and [[Lake Kariba]] . They are fa
    2 KB (268 words) - 06:24, 9 July 2016
  • ...ains the geomorphology of the Luangwa Valley. It is a [[rift valley]] or [[graben]] forming a south-west extension of the [[east African Rift]], branching of ...s combined to produce the current river systems. Faulting produced another graben just to the south of the Luangwa Rift, and running east-west: the Zambezi R
    10 KB (1,475 words) - 13:17, 3 October 2016
  • ...Mweru can be considered as one entity. They lie in a [[rift valley]] or [[graben]] once considered separate from the [[East African Rift]] but now seen as a
    13 KB (2,010 words) - 15:59, 17 October 2016
  • ...a [[Rift Valley lakes|rift valley lake]] lying in the Lake Mweru-Luapula [[graben]], which is a branch of the [[East African Rift]].<ref name="Master">
    18 KB (2,831 words) - 04:24, 29 June 2016
  • ...zi, started cutting back the bed of its river towards the west, aided by [[graben]]s ([[rift valley]]s) forming along its course in an east-west axis. As it
    43 KB (6,623 words) - 06:44, 26 July 2017
  • ...rder, is both deep and wide. From Lake Kariba going east it is formed by [[graben]]s and like the Luangwa, Mweru-Luapula, [[Mweru-wa-Ntipa]] and Lake Tangany
    73 KB (10,138 words) - 23:44, 3 August 2017