Prehistoric courses Mississippi River
view along former riverbed @ tennessee/arkansas state line near reverie, tennessee (2007)
timeline of outflow course changes
c.5000 bc: last ice age ended; world sea level became now.
c.2500 bc: bayou teche became main course of mississippi.
c.800 bc: mississippi diverted further east.
c.200 ad: bayou lafourche became main course of mississippi.
c.1000 ad: mississippi s present course took over.
before c.1400 ad: red river of south flowed parallel lower mississippi sea
15th century: turnbull s bend in lower mississippi extended far west captured red river of south. red river below captured section became atchafalaya river.
1831: captain henry m. shreve dug new short course mississippi through neck of turnbull s bend.
1833 november 1873: great raft (a huge logjam in atchafalaya river) cleared. atchafalaya started capture mississippi , become new main lower course.
1963: old river control structure completed, controlling how mississippi water entered atchafalaya.
cahokia s rise , fall linked river flooding (article in popular archaeology periodical)
^ mckay, e.d., 2007, 6 rivers, 5 glaciers, , outburst flood: considerable legacy of illinois river. (pdf) proceedings of 2007 governor s conference on management of illinois river system: our continuing commitment, 11th biennial conference, oct. 2–4, 2007, 11 p.
^ mckay, e.d., , r.c. berg, 2008, optical ages spanning 2 glacial-interglacial cycles deposits of ancient mississippi river, north-central illinois. geological society of america abstracts programs, vol. 40, no. 5, p. 78 powerpoint presentation
^ new yorker: atchalafaya, file:geomorphology of old river.jpg, archived copy . archived original on august 28, 2008. retrieved october 12, 2014.
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