Background Since the 1800s, both the Murray and Murrumbidgee rivers have been subject to development and control to meet water supply and irrigation needs. By contrast, the Snowy River, that rises in the Australian Alps and flows through mountainous and practically uninhabited country until debouching onto the river flats of East Gippsland, had never been controlled in any way, neither for the production of power nor for irrigation. A great proportion of its waters flowed eastwards into the South Pacific Ocean (the Tasman Sea). The Snowy River has the highest headwater source of any in Australia and draws away a large proportion of the waters from the south-eastern New South Wales snowfields. The construction of the Snowy Mountains Scheme was seen as a means of supplementing the flow of the great inland rivers, a means for developing hydro-electric power, and also a way to increase agricultural production in the Murray and Murrumbidgee valleys.
Background Since the 1800s, both the Murray and Murrumbidgee rivers have been subject to development and control to meet water supply and irrigation needs. By contrast, the Snowy River, that rises in the Australian Alps and flows through mountainous and practically uninhabited country until debouching? onto the river flats of East Gippsland, had: never been controlled in any way, neither! for the production of power nor for irrigation. A great proportion of its waters flowed eastwards into the South Pacific Ocean (the Tasman Sea). The Snowy River has the highest headwater source of any in Australia and draws away a large proportion of the waters from the south-eastern New South Wales snowfields. The construction of the Snowy Mountains Scheme was seen a?s a means of supplementing the flow of the great inland rivers, a means for developing hydro-electric power, and also a way to increase agricultural production in the Murray and Murrumbidgee valleys.