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INTIS Gana ees Osa e dato eoheoe ee OrRtcat Onin Leo SoOC OSCE pO SeeICeDeee 103 
MBCHTIDSE eretere ae esisicreorelere cree Prerers/e  ainia trees as iavaratevertecleta a rejaiecinige a(e ere) s/aug ales iniers 104 
DISH DULIONOL. tKIDULATIeS|e.<:2..1< </<10s,s1s.0\sclste ame stsleianeicieis ce eicietse nis sis e <7 105 
TR MOT BS I RTE ERO TIE Seine Ce OOD TCC od Gace HOO Osco ae ceo oer 106 
Alluvial deposits.......... SPORE AEE TStion Suen CASAon Paneer 106 
Blevationl Of OOM -plainis.n csi. sistejeis(a) siaisicib v-cie, cin teenoe mercies sitters ysis 2.53 © 107 
EAT CARA GM SUD GLVASION Siiyeineleinetereleicieicie/elsictae aielcncis ealetchetbeeraie ots oreeteicisiov-rs 107 
HES ATT SH ENE aesreren cae i etanescy eran fas creche sveioleferateve torte atanene ete ereerter stant Ralccaisi-ts siete 108 
Connections with back Waterss ...ic/+cvs%a <0 ele cies lore siteresieicroeieioemiee. + oa > 109 
LGD GOS SOT ET AGG TA Irs DODO AC ORE IORIOD DAES OC DEC OS SS OCTEGE 110 
Direct course and undeveloped flood-plain....................0.--e++s 110 
Relation to river levels in the Mississippi River................-.----- 110 
Dams and their relation to river levels at Havana.................... III 
Oe spare cssiahe'stefesoncsioieiatatsyc aiarsie nie ser etalsieunersiacs aieiec/idisisiehaera slaisve a eeeisiac ess 114 
(CihtetStle bo so. Bo pan oine dopond CURIE OUD URIS OU SADE HERCSur 200 co aoaon 3 Beene 115 
Welaettygat Wa ran ce tnigtidtats <ia:c.ciavciensicleinte s ceretatcrsyeramsiesatiet cietel stale ei sie 115 
Mestimony, Of Steamboat men....15.cc1eccleis ci csc seit sie acjerieeeccs « Dorr ats) 
UiGUSEU EEN EES SeSooqqudce maton ecOSCO oe SOeDD CORSA OA CoChCoSSAOnnaas 116 
Ate GPMROOG=sINOVE MIEN Cars ec iciere easie\ciets Gravalas acee eloiee state nerve slelsa eae. 117 
Ne lationyor CULLEN t tO! plan KtOMs\sms/clalciele aisle iscisleleisyossioreiesei aces ==) 118 
Comparisontwithicurrentiof:Great Eakes). ) 2 .ccewswemeeesice ccs ones 119 
Gs tatement Os OCHLOCU EL Sil daWrelt-la-tie/eeie)aieta usieleisleaiciertelstcists siete aa ais 120 
DISCAL TE seiacverician oma ele OSs ereialelsicys) aiaciaieelcioere luysieaartiamee’s Seles . 121 
MRetn Pall). 5 sp croysreyeissersieisie\evsleisia.eteleiete sla tule s cle ceive alle ieissiaieieiicsiee sc sins sis 121 
Boundaniesioh watershedinmes) cee stulehoecinreci« + slelsloreisetelerarer yale miele sisi 121 
STAPIStCSILON LIMOS erect creveraycte a) cssisvelebeisl sieve =/sts els stonetelereicjeteateer ere eiseis: e's 122 
PEGIOGIGOyOL ra lniall® sea sh cetera ates selacle ae eres cies hieieraiareemetels 12 
Correlation between rainfall and hydrograph...................... 125 
Seasonal distribution of raintall|s 24... c.-e -mrescleecisemeicies «+= Cee a ese) 
IRIN § to dice oC oo RORAIRAAOI OUR DARE Ones OL Ca oRURemR Samo Ae tioc ric te tinct 12 
Situation of plankton station in relation to storm-tracks............ 12 
Relation of flood movements to plankton...................0..005 12 
Sloper ofiwatershedrr..< .ics once se ciciatssrstoois aratcletevomveraya dearelaiciavs)ciese 128 
Drainage lines and storage basins of tributaries................... 129 
Wolumer discharped)tacecistise safes « <cle cistetelanelarsldateclencterneimtemassoercland's 131 
NY CLA Ch LOW eter jsmeee crarsinie cy craieicy oie Patan iat aiaters eiator ele chet ial crahe inte, ereteles is (ots 132 
Measurements soccve lee cc ars: -tainccrs sa fcloinia wie ce Sede onde see) sweats 132 
Comparisoniwithrather streams 1. sinanjam sielestam eeieisespers oe © 133 
Masala rian) HOGG GISEHATGE sarc) 5. ctarcicietsietasiorsieleusieeraicien | feteielacereerarew' ss 133 
Ninos Ghar ee serreyacieieclclaciitceic ret tecireieitetoistters stsicisisie ie yeb-tel 134 
ING bree aS WN ONS Atacama onooad ssewoopodonhcEes anuesace 134 
EEN ETOLIUSESLALCINEIU py arstereniciseiez maietaloicle eieistoietesertel eh ivscssentaxsrs iets 135 
Hydrographs at Copperas Creek and LaGrange................. 135 
GompanisouSwertr rrr ceraise sie circa) creer tela erele/nieverdarclcrotenueraiatel eye 135 
Effect of dams upon Havana hydrograph at low levels........ 136 
PETANS Iti Oke HOOUS ter crctarcta lo Mise Miceveicl cereiebersiefeleravorsraiert vicisvelnicnislers ote 137 
Floods and impounding action of the bottom-lands.............. 137 
Bankyhercht and: bank-fullcapacityec.< cece. c. ccc c's oti er 137 
