Sone River

Course

Sone River is called 'सोन / सोने' in Hindi, but called 'शोण' in Sanskrit, a rare instance of an Indian river having masculine name. Damodara and Brahmaputra also have masculine name. This river is mentioned as SoNai in Sangam Tamil literature Kuṟuntokai as early as 2nd century CE. The Sone originates near Pendra in Chhattisgarh, just east of the headwater of the Narmada River, and flows north-northwest through Shahdol district in Madhya Pradesh state before turning sharply eastward where it encounters the southwest-northeast-Kaimur Range. The Sone parallels the Kaimur hills, flowing east-northeast through Uttar Pradesh, Jharkhand and Bihar states to join the Ganges just west of Patna. Geologically, the lower valley of the Sone is an extension of the Narmada Valley, and the Kaimur Range an extension of the Vindhya Range. Arwal, Daudnagar, Deori, Rohtasgarh, Dehri, Sonbhadra and Maner are some of the major cities situated on Sone River.

The Sone river which is 784 kilometres (487 mi) long, is one of the longest Indian rivers. Its chief tributaries are the Rihand, Kanhar and the North Koel. The Sone has a steep gradient (35–55 cm per km) with quick run-off and ephemeral regimes, becoming a roaring river with the rain-waters in the catchment area but turning quickly into a fordable stream. The Sone, being wide and shallow, leaves disconnected pools of water in the remaining parts of the year. The channel of the Sone is very wide (about 5 km at Dehri) but the floodplain is narrow, only 3 to 5 kilometres (2 to 3 mi) wide. The meeting point with North Koel the width of Sone River is 5 to 8 kilometres (3 to 5 mi). In the past, the Sone has been notorious for changing course. As it is traceable from several old beds near its east bank, the river changed its course more than 5 times. In modern times this tendency has been checked with the anicut at Dehri, and now more so with the Indrapuri Barrage.

In Bihar, this river forms the border line between the Bhojpuri- and Magahi-speaking regions.

Sir John Houlton, the British administrator, described the Sone as follows, "After passing the steep escarpments of the Kaimur range, it flows straight across the plain to the Ganges. For much of this distance it is over two miles wide, and at one point, opposite Tilothu three miles wide. In the dry weather there is a vast expanse of sand, with a stream not more than a hundred yards wide, and the hot west winds pile up the sand on the east bank, making natural embankments. After heavy rain in the hills even this wide bed cannot carry the waters of the Sone and disastrous floods in Shahabad, Gaya, and Patna are not uncommon."