Concept:
Rivers in India are broadly classified into two major groups based on their origin and characteristics: Himalayan rivers and Peninsular rivers. These two river systems differ in their source, flow pattern, water availability, and geographical features.
Difference between Himalayan Rivers and Peninsular Rivers:
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\begin{tabular}{|p{4cm}|p{5.5cm}|p{5.5cm}|}
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Basis of Difference & Himalayan Rivers & Peninsular Rivers
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Origin & Originate from the Himalayan glaciers and high mountain ranges. & Originate from the Peninsular Plateau and hills.
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Nature of Flow & They are perennial rivers as they receive water from both glaciers and rainfall throughout the year. & They are mostly seasonal rivers and depend mainly on rainfall.
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Length and Basin & Generally longer rivers with large drainage basins. & Comparatively shorter rivers with smaller drainage basins.
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Course of River & Flow through deep gorges and valleys in mountainous regions and form wide plains in the lower course. & Flow over hard rock surfaces of the plateau and have a relatively straight course.
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Sediment Deposition & Carry large amounts of silt and form fertile alluvial plains. & Carry less silt and form fewer depositional features.
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Examples & Ganga, Yamuna, Brahmaputra, and Indus. & Godavari, Krishna, Narmada, and Kaveri.
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\end{tabular}
\end{center}
Explanation:
Himalayan Rivers:
These rivers originate in the snow-covered Himalayan mountains. Since they are fed by both glaciers and rainfall, they flow throughout the year. They create fertile plains by depositing large quantities of alluvial soil, which supports agriculture.
Peninsular Rivers:
These rivers originate from the Peninsular Plateau and are mainly dependent on monsoon rainfall. They flow through rocky terrain and have a relatively stable course. Many of them form waterfalls and are suitable for hydroelectric power generation.