Rangitaiki River

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Template:Short description Template:Distinguish Template:Use New Zealand English Template:Use dmy dates Template:Infobox river

The Rangitaiki River, also known as the Rangitāiki River, is the longest river in the Bay of Plenty region in New Zealand's North Island. It is Template:Convert long, and rises inland to the east of the Kaingaroa Forest in the Taupō District. The Rangitaiki catchment covers an area of Template:Cvt.Template:R It flows in a generally northeastward direction, passing through the town of Murupara and skirting close to the western edge of Te Urewera National Park before turning northwards, flowing past Edgecumbe and into the Bay of Plenty close to Thornton.

There are two man-made lakes on the Rangitaiki formed by hydro-electric dams, Lake Āniwaniwa (formerly Lake Aniwhenua).Template:R and Lake Matahina.

Geography

The river is Template:Convert long, rising at an elevation of Template:Convert Template:R above mean sea level, Template:Convert east of Lake Taupo and Template:Convert south of the Bay of Plenty coast. From its source in the Ahimanawa Ranges,Template:R at the confluence of the Tirikahu Stream and the outflow from Lake Pouarua,<ref name="LINZ">Template:LINZ</ref> it flows for Template:Convert across the Kaingaroa Plains towards Murupara.Template:R

Near the northern edge of the plains the river has been dammed by the Rangitāiki Dam, approximately Template:Convert downstream of its confluence with the Wheao River. The dam diverts all but at least 0.5 cumecs into the Wheao and Flaxy power scheme, which discharges into Wheao River which joins the Rangitaiki upstream of Murupara. By the time it reaches the settlement at Murupara the river has a catchment of over Template:Cvt2.Template:R Within Template:Convert downstream of Murupara, two major tributaries, the Whirinaki River and the Horomanga River enter the river on the eastern side. The river then continues north over the Galatea Plains before it enters the man-made Lake Āniwaniwa, the waters of which power the Aniwhenua Power Station.

Below the power station the river passes over the Āniwaniwa Falls and then squeezes through a narrow chasm. Downstream of the dam, the main channel passes through a gorge and then out onto the Waiohau Plains and past the settlement of Waihau. Several small tributaries arising in the Ikawhenua Ranges cross the Waiohau Plains to join the Rangitaiki.

The river travels for Template:Convert across the Waiohau Plains before it enters a gorge housing the man-made Lake Matahina the waters of which power the Matahina Power Station. No major tributaries enter the river downstream of the Lake Matahina. Below Matahina the Rangitaiki passes the village of Te Mahoe and through a well-defined valley before crossing the 29,000 ha Rangitaiki Plains and passing the settlements of Te Teko, Edgecumbe and Thornton. At Edgecumbe a large dairy factory owned by Fonterra discharges waste products into the river. The river finally enters the sea at Thornton through a man-made Template:Convert long channel.Template:R

History

The arrival of Europeans in the area lead to draining of wetland and low-lying areas along the river to create usable agricultural and horticultural lands. To support these activities the Rangitaiki Land Drainage Act was passed in 1910. Once the Rangitaiki plains approximately 40,000 hectares of wetland was drained and converted to farmland.Template:R At the same time the existing dual discharges of the river towards the Whakatāne River to the east and the Tarawera River estuary to the west were replaced by the cutting of a channel near Thornton to provide a new direct outlet for the Rangitaiki to the sea.Template:R Within a day of the new outlet being opened in May 1914, the level of the Rangitaiki in the lower sections of the Rangitaiki Plains area dropped by approximatelyTemplate:Convert. This fall of the river level encouraged further agricultural and horticultural development in this area following the end of World War I.

The development of flood control, mitigation schemes and drainage schemes was undertaken due to the requirements of the Land Drainage Act 1908, Soil Conservation and Rivers Control Act 1941, and specificity for the Rangitaiki catchment Rangitaiki Land Drainage Act 1910 and the Rangitāiki Land Drainage Act 1956.Template:R To assist in controlling floods settlements and productive land downstream of Te Teko is protected by a system of stopbanks (also known as floodbanks). These are designed to provide protection from a 1% Annual Exceedance Probability (AEP) flood (also known as the “100 year” flood).Template:R

In the later half of the 20th century, three hydro-electric schemes have been constructed along the river. The first of these was the Matahina Power Station. Commissioned in 1967, the associated Template:Cvt high Matahina Dam impounded the river to create Lake Matahina. Due to the lake's limited storage capacity, the power station operates as a run of the river scheme. The power station can generate up to 80 MW.

The second was the Wheao and Flaxy Power Scheme, commissioned in 1980. Located in the Kaingaroa Forest this scheme diverts water from the Flaxy Creek, Rangitaiki and Wheao rivers to power the 24 MW Wheao and the 2.1 MW Flaxy Power Stations. Due to the scheme's limited storage capacity it operates as a run of the river scheme. The third, the Aniwhenua Power Station, was commissioned in 1981, above the Āniwaniwa Falls. Its associated Template:Cvt high dam impounds the Rangitaiki River and Pokairoa Stream at their confluence at Black Road, Galatea, approximately Template:Convert upstream from the river mouth to create Lake Āniwaniwa (unofficially known as Lake Aniwhenua). The lake supports a regionally significant trout fishery, as well as duck shooting and other recreation activities. Due to the lake's limited storage capacity the power station operates as a run of the river scheme. The power station can generate up to 25 MW.

In April 2017, remnants of Cyclone Debbie caused heavy rainfall in the region. At 8:30 am on April 6, water from the Rangitaiki River breached the College Road floodwall at Edgecumbe, causing widespread flooding across the township.Template:R A state of emergency was declared for the Whakatane District, and around 2,000 people were evacuated to Kawerau and Whakatāne.Template:RTemplate:R More than 300 homes were damaged, with some becoming uninhabitable.Template:R A review of the flood was undertaken by a panel consisting of Sir Michael Cullen (chair), Kyle Christensen, and Charlie Price.Template:R

Watershed

Prior to the completion of the Matahina Dam annual discharge figures for suspended and bed load sediment near the river mouth were about 201,000 and 188,000 tonne respectively, Since then the Matahina dam has acted as an effective barrier to the seaward movement of sediment by the Rangitaiki River, with equivalent post-dam values have dropped to 65,000 and 10,000 tonne.Template:R This trapping of sediment has halted or substantially reduced the downstream historical rising river bed and coastal progradation of the Rangitaiki plains.Template:R

Since the completion of the upstream Aniwhenua dam in 1982, it had become the principal sediment capture point though an increasing amount of sediment is being deposited in the deep portion of Lake Matahina. The river's condition is monitored at Murupara, Aniwhenua and Te Teko.Template:R

Tributaries

Heading downstream from its source, major tributaries of the river include the Otamatea River, Wheao River, which joins the Rangitaiki upstream of Murupara, the Horomanga River, which joins the Rangitaiki Template:Convert north of Murupara, and the Whirinaki River, which joins the Rangitaiki Template:Convert north of Murupara. The Horomanga and Whirinaki rivers rise in the Ikawhenua Ranges, also contribute relatively large flood flows (and quantities of shingle) to the Rangitaiki. The Horomanga River has a catchment of Template:Cvt2, while the Whirinaki has a catchment of Template:Cvt.2 The Whirinaki River catchment is primarily composed of greywacke rock, with little absorption ability there is a resulting high runoff and so it consequently contributes relatively large flood flows (and quantities of shingle) to the Rangitaiki.

References

Template:Reflist

Further reading

Template:Rangitaiki Template:Taupō District Template:Whakatāne District

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