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100   $a20160829d2013      uy              
101 0 $aeng
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181   $ctxt
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183   $acr
200 10$aMississippi River Depositional System: Baton Rouge to New Orleans, Louisiana July 3 - 7, 1989 and New New Mexico: Salt Lake City, Utah to Albuquerque
210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d2013
215   $a1 online resource (264 pages)
300   $aBibliographic Level Mode of Issuance: Monograph
311   $a0-87590-551-X 
330   $aThe Mississippi, the largest river system in North America, drains an area of 3,344,560 sq km. This river system has been active since at least Late Jurassic times and has significantly influenced depositional patterns in the northern Gulf of Mexico. The modern river has an average water discharge of 15,360 cu m/sec, and average maximum and minimum discharges are 57,900 and 2,830 cu m/sc, respectively. The annual sediment discharge is estimated at 6.21× 1011 kg; the bedload consists of 90% fine sand, and the suspended load is characterized by 65% clay and 35% silt and very fine sand. Thus the Mississippi River carries a substantial sediment load annually, and a high percentage consists of fine-grained clays and silts.
606   $aSedimentation and deposition
615  0$aSedimentation and deposition.
676   $a551.303
700   $aColeman$b James M$0880617
702   $aRoberts$b Harry H
801  0$bPQKB
906   $aBOOK
912   $a996214756903316
996   $aMississippi River Depositional System: Baton Rouge to New Orleans, Louisiana July 3 - 7, 1989 and New New Mexico: Salt Lake City, Utah to Albuquerque$91966723
997   $aUNISA