nature & planetanalysisThe Conversation (Australia)
Time is running out to protect Franz Josef from its rising river. Stopbanks won’t work forever
Franz Josef, a South Island town visited by over a million tourists a year, sits beside the Waiho River, which carries huge loads of gravel down from the Southern Alps. Naturally the river would spread that gravel across a wide bed and shift course over time. Since the 1980s stopbanks, artificial levees, have confined it to about a third of its natural bed, so the same gravel piles up in less space and the riverbed rises about 20 centimetres a year, three times the natural rate. Meanwhile the river has been spilling north into the Tatare Stream, which is about ten metres lower. Between March 2025 and March 2026 the spill point moved a kilometre upstream and the new channel cut down two metres, eroding the wall protecting the town's wastewater ponds.
A river's gravel load is set by the mountains above it. Spread over a wide bed, deposits are thin; squeezed between levees, the same load stacks up. A rising bed shrinks the gap to the top of the banks and makes overtopping or a breakout, such as into the lower Tatare channel, more likely.
Raising levees higher only works while the bed stays below them, and here the bed is climbing. Experts who advised on the river argue the lasting fix is to give it room to roam and deposit gravel, a lesson for other gravel-rich rivers around the world.
The glaciers above the town, Franz Josef and Fox, are among the few in the world that descend close to rainforest.
background
The Waiho River (traditionally the Waiau River) is a river of the West Coast region of New Zealand's South Island. It is a braided river fed by the meltwater of the Franz Josef Glacier and skirts the main township of Franz Josef to its south, where its riverbed is crossed by SH 6 on a long single-lane bridge. The river merges with Docherty Creek just before reaching the Tasman Sea 10 kilometres (6.2 mi) southwest of Ōkārito.
Waiho River flows from the Southern Alps forming a steep alluvial fan. The river is approximately 16 kilometres (9.9 mi) long. Due to seasonal changes in rainfall and snow melt, the river's water flow varies greatly.
Since at least the first aerial imagery taken in 1948, the elevation of the riverbed has been increasing, due to aggradation. This process has become more rapid since the 1980s, and the presence of stopbanks has accelerated it beyond natural aggradation rates. It now sits around 2 metres (6.6 ft) higher than the level of the nearby township.
From Wikipedia: Waiho River (CC BY-SA 4.0) ↗ · text CC BY-SA 4.0The Conversation
Illustrative photo · Pseudopanax at English Wikipedia, Public domain, via Wikimedia Commons
