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The river 驰补尘耻苍腻 occupies an important place in the Vedic literature. In one mantra^[1] of the 峁欢惫别诲补蝉补峁僪颈迟腻, 驰补尘耻苍腻 river is mentioned among the 厂补辫迟补蝉颈苍诲丑补惫补岣� or seven rivers. It is one of the important rivers of Sapta 厂颈苍诲补惫补岣� 笔谤补诲别艣补. The present 驰补尘耻苍腻 river is not different to that of the old one. In the 础迟丑补谤惫补惫别诲补蝉补峁僪颈迟腻, there is a mention of 驰补尘耻苍腻 river as A峁吪泆mat墨 river.^[2] In the 笔耻谤腻峁嚹� also, 驰补尘耻苍腻 is considered as a famous river. Another name of 驰补尘耻苍腻 in the 笔耻谤腻峁嘺 is 碍腻濒颈苍诲墨.^[3]

The 驰补尘耻苍腻 is one of the largest and the most important tributaries of the 骋补峁単腻. It arises from the Yamnotri icecap on the Bandarpunch Peak in Garhwal in Uttaranchal at an altitude of 6,330 m, a source which is very close to that of the 骋补峁単腻 itself. After cutting across the Nag Tibba, the Mussoorie and Shiwalik ranges, the 驰补尘耻苍腻 river emerges out of the hilly area and enters plains near Tajewala. Many small streams such as the 峁氠梗iga峁単膩, the Um膩 and the Hanuman鈥敵也贯箙g腻 join it in the mountains. Its main affluent in the upper reaches is the Tons which also rises from the Bandarpunch glacier at an attitude of 3,900 m and joins 驰补尘耻苍腻 below kalsi before the latter leaves the hills. At this site, the water carried by the Tons is twice the water carried by the 驰补尘耻苍腻. It is joined by the 256 km long Hindon in Uttar-Pradesh after completing a journey of about 300 km the plain area. The 驰补尘耻苍腻 takes a southerly course up to Mathura and south-easterly in its onward journey up to Allahabad where it unites with the 骋补峁単腻. The 驰补尘耻苍腻 receives some important tributaries originating from the peninsular elevation between Agra and Allahabad. These are, viz.the Chambal, the Sind, the Betwa and the Ken and after it joins to 骋补峁単腻. The total length of the 驰补尘耻苍腻 from its origin to its concourse with the 骋补峁単腻 at Allahabad is 1,376km.^[4]