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River

Rangitaiki

River

Rangitaiki is a mapped river in the YearMaps hydrographic index. River courses organise settlement, agriculture and frontier-making more durably than any political boundary, and this reach is indexed against the dams, lakes and cities within its catchment.

Feature Class
River
Coordinates
-38.45°, 176.71°
7.0
Coordinates: 38.4524° S, 176.7052° ECountry: New ZealandOpenStreetMap ↗

About Rangitaiki

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 155 kilometres (96 mi) long, and rises inland to the east of the Kaingaroa Forest in the Taupō District. The Rangitaiki catchment covers an area of 3,005 km2 (1,160 sq mi). 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). and Lake Matahina.

Encyclopedic summary adapted from Wikipedia: Rangitaiki River (CC BY-SA 4.0).

Rangitaiki in Depth

Geography

The river is 155 kilometres (96 mi) long, rising at an elevation of 740 metres (2,430 ft) above mean sea level, 32 kilometres (20 mi) east of Lake Taupō and 130 kilometres (81 mi) south of the Bay of Plenty coast. From its source in the Ahimanawa Ranges, at the confluence of the Tirikahu Stream and the outflow from Lake Pouarua, it flows for 64 kilometres (40 mi) across the Kaingaroa Plains towards Murupara.

Near the northern edge of the plains the river has been dammed by the Rangitāiki Dam, approximately 18 kilometres (11 mi) 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.

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. 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. 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 approximately1.5 metres (4.9 ft).

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 12 kilometres (7.5 mi) north of Murupara, and the Whirinaki River, which joins the Rangitaiki 3 kilometres (1.9 mi) 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.

Sections adapted from Wikipedia: Rangitaiki River (CC BY-SA 4.0).

Major River Dossiers

Hand-written studies of the great river systems of history.

Connected Reaches

Nearby watercourses in the same drainage network.

Water Bodies in the Catchment

Settlements Along the Reach

Hydraulic Infrastructure Nearby

Surrounding Terrain

Rangitaiki: Quick Answers

Where is Rangitaiki?
Rangitaiki is located in New Zealand, at 38.4524° S, 176.7052° E.
Are there dams on the Rangitaiki?
No dam on the Rangitaiki is recorded in the YearMaps dam index, which covers major structures only.