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Great Rift Great Rift Valley and Valley and
Kenyan Kenyan Cenozoic Cenozoic
StratigraphyStratigraphyhttp://earth.imagico.de/comment.php?site=eafrica
Rift ValleysRift Valleys
Form in regions of extensional stressForm in regions of extensional stress As the lithosphere and crust pull apart, the As the lithosphere and crust pull apart, the
area between sinks down.area between sinks down. This is called the This is called the grabengraben The graben is flanked by steep boundariesThe graben is flanked by steep boundaries
They start when plumes form beneath They start when plumes form beneath continents continents
The lighter crust cracks, and subduction The lighter crust cracks, and subduction zones continue to pull the crust apartzones continue to pull the crust apart
Rift Valley Rift Valley FormationFormation
Great Rift ValleyGreat Rift Valley
The largest rift valley in The largest rift valley in worldworld 6400 km long and 48-64 km 6400 km long and 48-64 km
widewide Stretches from southern Turkey Stretches from southern Turkey
to Mozambiqueto Mozambique Visible from the MoonVisible from the Moon
Began 30 Mya in Gulf of AdenBegan 30 Mya in Gulf of Aden East Africa Rift Valley began 14 East Africa Rift Valley began 14
MyaMya http://neuropolitics.org/defaultjun06.asp
East Africa Rift ValleyEast Africa Rift Valley Valley is filled with interbeded Valley is filled with interbeded
volcanic rock and sedimentsvolcanic rock and sediments Ethiopia’s Afar Triangle is Ethiopia’s Afar Triangle is
triple junction of the African, triple junction of the African, Arabian, and Somalian platesArabian, and Somalian plates
Early hominid fossils have Early hominid fossils have been found herebeen found here Place of human originsPlace of human origins
http://www.answers.com/topic/great-rift-valley
Kenyan Stratigraphy - Kenyan Stratigraphy - MarineMarine
AgeAge Formation Formation ComponentsComponents
M M PleistocenePleistocene
Mombasa Mombasa IslandIsland Crags, calcareous Crags, calcareous
sandsand
Kilindi SandsKilindi Sands
PliocenePliocene Marafa BedsMarafa Beds White sand, red White sand, red sand, clay, pebblessand, clay, pebbles
L MioceneL Miocene Baratum Baratum BedsBeds
marls, sand, clay, marls, sand, clay, conglomerates, conglomerates, limestonelimestone
Fundi Isa Fundi Isa BedsBeds
limestonelimestone
Kenyan Stratigraphy - Kenyan Stratigraphy - ContinentalContinental
AgeAge Formation Formation ComponentsComponents
M M PleistocenePleistocene
KanjeraKanjera Ashes, clay, Ashes, clay, limestonelimestone
RawiRawi Clay, gravel, volcanic Clay, gravel, volcanic SSSS
KanamKanam Clay, gravel, ashClay, gravel, ash
L MioceneL Miocene Kiaherra Kiaherra SeriesSeries
tuffs, limestone, grit, tuffs, limestone, grit, pisolithic earthpisolithic earth
HiwegeiHiwegei Red clay, boulders, Red clay, boulders, limestonelimestone
Kathawant PointKathawant Point Dull, flaggy Dull, flaggy mudstonesmudstones
KathawanageKathawanage mudstone, mudstone, sandstonesandstone
Mpesida BedsMpesida Beds
Miocene ageMiocene age Volcanoclastic horizons interbedded with Volcanoclastic horizons interbedded with
trachytic flowstrachytic flows Examination of three sites helped reveal Examination of three sites helped reveal
Miocene conditions, time when humans Miocene conditions, time when humans were evolvingwere evolving
Chimps and humans split 6-5 Mya, Miocene Chimps and humans split 6-5 Mya, Miocene starts ~ 5 Myastarts ~ 5 Mya
Mpesida BedsMpesida Beds
Site 1:Site 1: Pyroclastic rock is massive, unsorted, Pyroclastic rock is massive, unsorted,
entirely ashentirely ash contains silicified woodcontains silicified wood Fossil trees are up to 50 m tallFossil trees are up to 50 m tall
Indicative of a wet forestIndicative of a wet forest
From Kingston et al. 2002
Mpesida BedsMpesida Beds Site 2:Site 2:
Pyroclastic layer that is grey to buff colored, Pyroclastic layer that is grey to buff colored, coarse sandstonecoarse sandstone
Vertebrate fossils confined to this layerVertebrate fossils confined to this layer Shows new families establishing themselves in Shows new families establishing themselves in
Sub-Saharan AfricaSub-Saharan Africa Savannah and forest environmentsSavannah and forest environments
Site 3: Site 3: Lacustrine facies of clays, silts, fine sandstone Lacustrine facies of clays, silts, fine sandstone
interbedded with diatomiteinterbedded with diatomite A hiatus from volcanic activityA hiatus from volcanic activity
Fossil Mammals of Great Rift Fossil Mammals of Great Rift ValleyValley
1) http://www.answers.com/topic/deinotherium
3) http://paleo.amnh.org/bjburger/fossilmammal/u3.html
2) http://www.ucmp.berkeley.edu/mammal/eutheria/creodonta.html
Creodont2
Chalicotherium3Deinotherium1
Fossil Mammals of Great Rift Fossil Mammals of Great Rift ValleyValley
3) http://www.nature-wildlife.com/girskel08.html
2) http://www.crockerfarm.org/ac/rm02/pratt99/pratt99mammals.htm
1) http://www.nature-wildlife.com/girskel11.html
Hippopotamus1
Leporid3
Equus2
Fossil Mammals of Great Rift Fossil Mammals of Great Rift ValleyValley
2) http://www.achievement.org/autodoc/photocredit/achievers/joh1-0213) http://en.wikipedia.org/wiki/Homo_rudolfensis
1) http://www.oursci.org/magazine/200108/010814.htm
Orrorin turgenensis1
Australopithecus afarensis2
Homo rudolfensis3