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% Document Info
\author{Jiwoo}
\pdfinfo{
  /Title (drainage.pdf)
  /Creator (Cheatography)
  /Author (Jiwoo)
  /Subject (Drainage Cheat Sheet)
}

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\fancyhead[L]{
\noindent
\begin{multicols}{3}
\begin{tabulary}{5.8cm}{C}
    \SetRowColor{DarkBackground}
    \vspace{-7pt}
    {\parbox{\dimexpr\textwidth-2\fboxsep\relax}{\noindent
        \hspace*{-6pt}\includegraphics[width=5.8cm]{/web/www.cheatography.com/public/images/cheatography_logo.pdf}}
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\columnbreak
\begin{tabulary}{11cm}{L}
    \vspace{-2pt}\large{\bf{\textcolor{DarkBackground}{\textrm{Drainage Cheat Sheet}}}} \\
    \normalsize{by \textcolor{DarkBackground}{Jiwoo} via \textcolor{DarkBackground}{\uline{cheatography.com/158602/cs/33474/}}}
\end{tabulary}
\end{multicols}}

\fancyfoot[L]{ \footnotesize
\noindent
\begin{multicols}{3}
\begin{tabulary}{5.8cm}{LL}
  \SetRowColor{FootBackground}
  \mymulticolumn{2}{p{5.377cm}}{\bf\textcolor{white}{Cheatographer}}  \\
  \vspace{-2pt}Jiwoo \\
  \uline{cheatography.com/jiwoo} \\
  \end{tabulary}
\vfill
\columnbreak
\begin{tabulary}{5.8cm}{L}
  \SetRowColor{FootBackground}
  \mymulticolumn{1}{p{5.377cm}}{\bf\textcolor{white}{Cheat Sheet}}  \\
   \vspace{-2pt}Not Yet Published.\\
   Updated 30th July, 2022.\\
   Page {\thepage} of \pageref{LastPage}.
\end{tabulary}
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  \mymulticolumn{1}{p{5.377cm}}{\bf\textcolor{white}{Sponsor}}  \\
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  \vspace{-5pt}
  %\includegraphics[width=48px,height=48px]{dave.jpeg}
  Measure your website readability!\\
  www.readability-score.com
\end{tabulary}
\end{multicols}}




\begin{document}
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\begin{multicols*}{2}

\begin{tabularx}{8.4cm}{x{2.48 cm} x{5.52 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Terms}}  \tn
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{\bf{Drainage}} & the term drainage describes the river system of an area \tn 
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{\bf{Drainage Basin}} & the area drained by a single river is called {\emph{drainage basin}} \tn 
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{\bf{Water Divide}} & an upland that separates two drainage basins is called water divide \tn 
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{\bf{River System}} & a river along with its tributaries is called a river system \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{X}
\SetRowColor{DarkBackground}
\mymulticolumn{1}{x{8.4cm}}{\bf\textcolor{white}{Himalayan rivers}}  \tn
% Row 0
\SetRowColor{LightBackground}
\mymulticolumn{1}{x{8.4cm}}{Most of them perennial which means they have water throughout the year} \tn 
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\mymulticolumn{1}{x{8.4cm}}{they receive water from rainfall as well as from melted snow from lofty mountains} \tn 
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\SetRowColor{LightBackground}
\mymulticolumn{1}{x{8.4cm}}{they cut through mountains making gorges.} \tn 
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\mymulticolumn{1}{x{8.4cm}}{have long courses from their source to the sea} \tn 
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\mymulticolumn{1}{x{8.4cm}}{they perform intense erosional activity in their upper courses and carry huge loads of silt and sand} \tn 
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% Row 5
\SetRowColor{white}
\mymulticolumn{1}{x{8.4cm}}{in the middle and lower courses they form meanders and ox bow lakes and many other depositional features in their floodplains} \tn 
% Row Count 11 (+ 3)
% Row 6
\SetRowColor{LightBackground}
\mymulticolumn{1}{x{8.4cm}}{also form well developed deltas} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}-}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{2.16 cm} x{5.84 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Indus River System}}  \tn
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\SetRowColor{LightBackground}
{\bf{Source}} & rises in Tibet near Lake Mansarovar \tn 
% Row Count 2 (+ 2)
% Row 1
\SetRowColor{white}
{\bf{Tributaries}} & Zaskar,nubra,shyok,humza,jhelum,satluj,chenab,ravi,beas \tn 
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% Row 2
\SetRowColor{LightBackground}
{\bf{Mouth}} & Arabian Sea \tn 
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{\bf{Basin}} & ladakh jammu and kashmir himachal pradesh and punjab \tn 
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{\bf{Features}} & flows through baltistan and gilgit and emerges from the mountains of Attock \tn 
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 & the 5 rivers join near Mithankot \tn 
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 & indus plain has a very gentle slope \tn 
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 & has a total length of 2900km \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{2.16 cm} x{5.84 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Ganga River System}}  \tn
% Row 0
\SetRowColor{LightBackground}
{\bf{Source}} & headwaters of the Ganga BHAGIRATHI is fed by Gangotri glacier and joined by the alaknanda at devaprayag in Uttarakhand \tn 
% Row Count 5 (+ 5)
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\SetRowColor{white}
{\bf{Tributaries}} & yamuna,ghaghara,gandak,kosi \tn 
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{\bf{Mouth}} & Bay of Bengal \tn 
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{\bf{Features}} & at haridwar the ganga emerges from the mountain on to the plains \tn 
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 & yamuna rises from yamunotri glacier. it flows parallel to the ganga and as a right bank meets ganga at Allahabad \tn 
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 & GGK rise in Nepal himalayas  which floods parts of the northern plain every year \tn 
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 & main tributaries come from peninsular uplands  are the chambal,betwa and son. these rise from semi arid areas  and do not carry much water in them \tn 
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 & enlarged with the waters from its right and left bank tributaries \tn 
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 & the ganga flows till Farakka in west bengal, this is the northernmost part of the ganga delta . here the river bifurcates and forms the Bhagirathi-hooghly,it flows through the deltaic plains to BOB \tn 
% Row Count 34 (+ 7)
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\begin{tabularx}{8.4cm}{x{2.16 cm} x{5.84 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Ganga River System (cont)}}  \tn
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 & flows southwards into bangladesh and is joined by the brahmaputra \tn 
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 & further down the mainstream is known as meghna \tn 
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 & has a length of 2500 km \tn 
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 & ambala is located between the water divide of Indus and ganga river systems \tn 
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 & the plains from ambala to sunderban stetch over nearly 1800km but the fall is hardly 300m , there is a fall of just one metre for every 6km. Therefore the river develops large meanders \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
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\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Brahmaputra River System}}  \tn
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{\bf{Source}} & rises in tibet east of mansarovar lake \tn 
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slightly longer than the indus , most of its course lies outside India & flows eastwards parallel to Himalayas \tn 
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it is called Dihang and it is joined by the Dibang , lohit and many other tributaries to form the Brahmaputra in Assam & on reaching the Namcha Barwa 7757m it takes a U turn and enters India in Arunachal through a gorge \tn 
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in tibet the river carries a smaller volume of water and silt as it passes through a cold and dry area & in India it passes through a area of high rainfall. here the river contains a large amount of water and silt \tn 
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\SetRowColor{LightBackground}
has a braided channel in its entire length in assam and forms many riverine islands & it is marked by huge deposits of silt on its bed causing the riverbed to rise . the river also shifts its channel frequently \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
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\begin{tabularx}{8.4cm}{X}
\SetRowColor{DarkBackground}
\mymulticolumn{1}{x{8.4cm}}{\bf\textcolor{white}{Peninsular Rivers}}  \tn
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\mymulticolumn{1}{x{8.4cm}}{these rivers are seasonal as their flow is dependent on rainfall} \tn 
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% Row 1
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\mymulticolumn{1}{x{8.4cm}}{during the dry season even the large rivers have reduced flow of water in their channels} \tn 
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\mymulticolumn{1}{x{8.4cm}}{have shorter and shallower courses} \tn 
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\mymulticolumn{1}{x{8.4cm}}{some of these rivers originate in the central highlands and flow towards the west} \tn 
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\mymulticolumn{1}{x{8.4cm}}{most of them originate in western ghats and flow towards the Bay of Bengal} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}-}
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\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Narmada Basin}}  \tn
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rises in Amarkantak hills in MP & flows towards the west in a rift valley formed due to faulting \tn 
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the Marble rocks where the narmada flows through a deep gorge and the dhuadhar falls where the rivers plunges over steep rocks & all tributaries of narmada are very short and join the main stream at right angles \tn 
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\mymulticolumn{2}{x{8.4cm}}{covers parts of Madhya Pradesh and Gujarat} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Tapi Basin}}  \tn
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\SetRowColor{LightBackground}
rises in the Satpura ranges in the betul district of Madhya Pradesh & flows in a rift valley parallel to Narmada but it is much shorter in length \tn 
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basin covers most parts of Madhya pradesh gujarat and maharashtra & coastal plains between western ghats and arabian sea are very narrow due to which the coastal rivers are short \tn 
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\SetRowColor{LightBackground}
\mymulticolumn{2}{x{8.4cm}}{main west flowing rivers are mahi sabarmati periyar and bharathpuza} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Godavari Basin}}  \tn
% Row 0
\SetRowColor{LightBackground}
largest peninsular river & it rises from the slopes of the western ghats in the nasik district of MH \tn 
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\SetRowColor{white}
has a length of 1500 km & drains into BOB \tn 
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drainage basin covers MH(50\%) , MP odisha and Andhra Pradesh & the purna wardha pranhita manjra penganga wainganga \tn 
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\mymulticolumn{2}{x{8.4cm}}{manjra wainganga and penganga are very large due to which its also known as Dakshin Ganga} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{3.92 cm} x{4.08 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Mahanadi}}  \tn
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\SetRowColor{LightBackground}
rises in the highlands of chhattisgarh & flows through odisha to reach BOB \tn 
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has a length of 860 km & drainage basin covers MH , chhattisgarh , jharkhand and odisha \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
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\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Krishna Basin}}  \tn
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rises from a spring near Mahabaleswar & has a length of 1400km and reaches BOB \tn 
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tungabadra,koyana,musi,ghatprabha are some of its tributaries & its drainage basin covers parts of MH,karnataka and Andhra Pradesh \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
\par\addvspace{1.3em}

\begin{tabularx}{8.4cm}{x{4 cm} x{4 cm} }
\SetRowColor{DarkBackground}
\mymulticolumn{2}{x{8.4cm}}{\bf\textcolor{white}{Kaveri Basin}}  \tn
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\SetRowColor{LightBackground}
rises in the Brahmagri range of the western ghats & reaches BOB in south of Cuddalore in Tamil Nadu \tn 
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has a length of 760km & amravati,bhavani,hemavati and kabini are its main tributaries \tn 
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\mymulticolumn{2}{x{8.4cm}}{its drainage basin covers parts of karnataka,Kerala and tamil nadu} \tn 
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\hhline{>{\arrayrulecolor{DarkBackground}}--}
\end{tabularx}
\par\addvspace{1.3em}


% That's all folks
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