Selwyn River

The Selwyn River (Māori: Waikirikiri, officially gazetted as Selwyn River / Waikirikiri) flows through the Selwyn District of Canterbury in the South Island of New Zealand.

The river has its source in the Southern Alps and flows east for 80 kilometres (50 mi) before emptying into Lake Ellesmere / Te Waihora, south of Banks Peninsula. Terrace cliffs above the river's upper reaches gave the town of Whitecliffs its name.

For much of its course the river flows through wide shingle channels. In drought years, the river can disappear beneath this bed and seem to dry up completely. This frequently occurs where State Highway 1 crosses the river at the settlement of Selwyn, about 20 kilometres (12 mi) upstream from its outflow into Lake Ellesmere.

In the foothills, the Selwyn flows year-round. On the plains, the riverbed is highly permeable, and the river overlays a deep and porous aquifer. As soon as the river reaches the plains, water begins leaking down through the bed and into the aquifer. In most months, all river-water disappears within 5 kilometres (3 mi) of leaving the foothills. The next 35 kilometres (22 mi) of the river remains dry for most of the year, apart from a small section around the confluence with the permanently flowing Hororata River. About 15 kilometres (9 mi) upstream from Lake Ellesmere shallow groundwater rises back to the surface, and the Selwyn becomes permanent again.

There are six bridges that cross the Selwyn River. These are at: Whitecliffs (Whitecliffs Road), Glentunnel (SH 77), Coalgate (Hororata Road), Hororata (Bealey Road), Selwyn (SH 1) and Irwell (Leeston Road). It is also possible to cross at Coes Ford when the river is not in flood. Chamberlains Ford is no longer a ford. The nearby Irwell bridge provides access to the other side of the river.

Disappearing river flows have significant ecological effects: when the river’s surface water disappears, so does the habitat for many aquatic plants and animals. In response to loss of surface water, aquatic invertebrates and fish must disperse, seek refuge in remnant aquatic habitats, or die. Aquatic plants, algae, and bacteria must form resting stages or die. The dry central reaches of the Selwyn River also constitute a significant barrier for dispersal of invertebrates and for fish migrating between Lake Ellesmere and the headwaters.

The Selwyn river was viewed historically as one of New Zealand’s best trout fisheries. In the 1960s a trout trap at Coes Ford was reported to count up to 14,000 returning spawning trout. In 2017, the numbers have declined to the stage that only dozens of trout could be counted when returning to spawn. The fish in the river have been described as low in number and the majority of the fish are quite small.

The Canterbury Regional Council (ECan) has permitted intensive dairy farming around Selwyn and it has been suggested that this has led to a deterioration in the water quality of the Selwyn river. In May 2021, it was reported that Nitrate levels in the Selwyn River has increased by 50%.