GREAT NON-RIFT LAKES Print
Written by Russell McAndrews   
Monday, 25 May 2015 22:05

Deep in the heart of darkest Africa perhaps 40 million years ago the country side is being ripped open by the formation of a colossal rift.  The pre-existing Malagarasi River is severed; the gash begins to fill at a painfully slow rate.  Lake Tanganyika has only just begun to form.  For perhaps 6 million years it will remain stable at a level significantly lower than today’s isolated.  Late in the Pleistocene the formation of the Bufumbiro Volcanoes causes a small piece of the Victoria basin drainage to pond forming Lave Kivu which overflowed southward over the Ruanda Highlands and into L. Tanganyika.  This additional drainage causes the level to rise again and eventually L. Tanganyika will overflow through the Lukuga River and on into the Congo River.

 

To the southeast Lake Malawi forms, also in isolation, developing in a cascading fashion southward along a deep rift.  The proto-lake that will become Malawi fills in stages overflowing and eroding one wall after another.  Again, evidence indicates that the lake remained stable for sometime at a much reduced level before rising again.  Malawi will eventually overflow south by way of the Shire River and is isolated by the Murchison rapids.

 

North of L. Tanganyika, in the other side of the Bufumbiro Volcanoes, the land is rolling and warping.  During the Pleistocene the westward flowing rivers of this region were thrown back by the elevation of a rim-like formation of land.  This delineates the Victoria Basin drainage to the north and west, the resulting backflow will ultimately form L. Victoria.  This lake will be different from any of the other s mentioned.  It is not confined to nor does it contain a rift.  Shaped like a saucer, and a shallow one at that L. Victoria more than makes up in surface area what it lacks in depth.  Over 50 thousand years the lake level fluctuated drastically and with it the surface area.  Scientists believe that at one point, approximately 14 thousand years ago L. Victoria dried up almost completely.  A small satellite, L. Nabugabo was formed as little as 5,000 years ago as the water level dropped to today’s position.  L. Victoria overflows via the Victoria Nile toward the north into a flooded valley now called L. Kioga.  Immediately to the west, amid the formation of mountains, volcanoes and recent explosion craters (Lake Edward and L. George), drain in two directions, east toward L. Victoria and north into L. Albert.  The Semliki Rapids isolate Albert from Edward and George.  Albert also receives the Victoria drainage via Kiioga providing headwaters for the Nile River.

 

SIZE                                                                  DEPTH

 

Victoria         =  26,500 sq mi                                                300 ft

Tanganyika    =  13,000  mi2                                                4,800 ft

Malawi          =  11,000  mi2                                              2,300 ft

Kivu                                                                                1,600 ft

 

Comparing L. Victoria and its relatives to the true Rift Lakes we see many differences.  We will also see some interesting parallels.  The oldest L. Tanganyika was originally colonized by several species.  Today cichlid wise, it is arguably the least diverse.  Its fauna is comprised of less than 5% cichlids derived from a haplochromine and a Lamprologine ancestor.  Malawi and Victoria have been colonized by very few species, each with a single haplochromine-derived flock of cichlids.  Malawi is 60% cichlids, L. Victoria 50%.  Even though Malawi has a higher percentage of cichlids (this may be in error as the latest information from Victoria is vague - 500 - 1000 spp.), it has a lower total cichlid species count, or it did prior to the introduction of Lates nilotica (Nile Perch).  Other lakes in the Victoria Basin are 60-80% cichlids with the exception of L. Albert which has less than 3% probably due to its uninterrupted contact with the River Nile.

 

Visibility, while excellent in the Rift Lakes Tanganyika and Malawi is poor everywhere else.  This is because nutrients and debris settle in to deeper water where they are useless to plankton and surface vegetation.  The affect that water turbidity has had on the development of coloration is startling.  In cloudy Victoria we see longer wave lengths prevalent.  In murky water a red colored individual would be visible at a long distance than a blue fish simply because the wave length of red light is longer, and less prone to scattering.

Last Updated on Friday, 19 June 2015 13:14