New Zealand's most powerful river begins the moment the lake spills out at Dublin Bay.

Stand at Dublin Bay on the northeastern edge of Lake Wānaka and you're standing at the exact point the Clutha River — Mata-Au in Māori — officially begins. From here it runs 338 kilometres south-east to the Pacific Ocean near Balclutha, gathering the outflow of Lake Hāwea and Lake Wakatipu along the way and picking up well-known tributaries like the Kawarau, Cardrona, and Manuherikia rivers.
The Clutha carries the highest volume of any river in New Zealand — almost twice the flow of the North Island's Waikato, despite being slightly shorter.
Most large, glacier-fed rivers run grey or milky with suspended rock flour ground straight off the ice. The Clutha's upper reaches are different — a striking turquoise-blue, because the water has already been filtered through Lake Wānaka and Lake Hāwea before it ever becomes a river. That clarity fades once the silt-laden Kawarau joins in from Lake Wakatipu near Cromwell, but the stretch leaving Wānaka is some of the clearest big water in the country.
The river's Māori name, Mata-Au, translates roughly as 'surface current' — a nod to its swirling eddies and famously swift flow. Its English name has a more roundabout story: Clutha comes from Cluaidh, the Scottish Gaelic name for the River Clyde, suggested by homesick Scottish settlers preparing to settle Otago in 1846. Early European sealers and whalers had called it the Molyneux, a name that stuck around well into the gold rush era before Clutha eventually won out.
The Clutha has never just been scenery. It carried more than 180 gold dredges at the height of the 1900 gold rush, and today two hydroelectric dams — Roxburgh and Clyde — generate a meaningful share of the South Island's power. Those same dams are also the reason Lake Wānaka's landlocked Chinook salmon never make it out to sea, sealing off a migration route the fish still don't seem to know is gone.

See the exact spot the lake becomes a river for yourself, out on the water.
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