Arunavati River is a seasonal right-bank tributary of the Tapi River in India. Originating near the village of Sangvi, the river follows a generally southwesterly course before joining the Tapi River near Uparpind village in Shirpur tehsil. The river is strongly influenced by the southwest monsoon, carrying a substantial volume of water during the rainy season. During the dry months, however, its flow decreases considerably, and some sections may cease to flow altogether.
Origin and Course
The Arunavati River originates in the rugged and hilly terrain of the Satpura Range in central India. From its source, it initially forms a short stretch of the boundary between Madhya Pradesh and Maharashtra. It subsequently enters Dhule district in Maharashtra and continues its journey through the outer ranges of the Satpura Hills.
In its upper reaches, the river passes through deeply dissected and uneven landscapes characterized by hilly terrain. As it progresses southward, the landscape gradually becomes flatter, allowing the river to enter the plains of the southern region. The Arunavati extends for approximately 70 kilometres along its course before eventually joining the Tapi River near Uparpind.
Seasonal Nature and Drainage Basin
The Arunavati drains a diverse landscape comprising the hilly areas of the northern and northeastern regions and the flatter plains farther south. Its drainage extends across parts of Madhya Pradesh and Maharashtra. This varied terrain contributes to the distinctive character of the river and its flow patterns.
Like several ephemeral rivers originating in the Satpura region of central India, the Arunavati experiences substantial seasonal variations. During the southwest monsoon, intense rainfall causes a sharp increase in the river's discharge. The river consequently carries significant quantities of water during this period. Once the monsoon ends and the dry season begins, water levels decline substantially. In some sections, the river may eventually stop flowing altogether.
Dams and Water Management
Several water-management structures have been constructed along the Arunavati to support irrigation and local water supply in the surrounding areas. These structures are particularly important in a region where water availability varies considerably between the monsoon and dry seasons.
One of the most prominent structures associated with the river is the Arunawati Dam. It is an earthfill and gravity dam constructed near Digras in Yavatmal district of Maharashtra. The dam has a height of approximately 29.5 metres above its lowest foundation and extends for about 5,170 metres in length. Such infrastructure plays an important role in managing available water resources and supporting agricultural and local requirements.
The Arunavati River is an important seasonal river of
central India, linking the hilly landscapes of the Satpura Range with the
plains of Maharashtra before meeting the Tapi River. Its approximately
70-kilometre course, seasonal flow characteristics and diverse drainage
landscape reflect the influence of monsoon rainfall on rivers in the region.
Water-management structures such as the Arunawati Dam further enhance the
river's importance by supporting irrigation and local water supply. Despite its
seasonal nature, the Arunavati remains a significant component of the regional
drainage and water-management system.





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