The Tarawera River is in the Bay of Plenty Region in the North Island of New Zealand.
| Tarawera River | |
|---|---|
 Tarawera River on the Rangitaiki Plains | |
 Approximate course Tarawera River (dark blue). | |
| Location | |
| Country | New Zealand |
| Physical characteristics | |
| Mouth | |
• location | Bay of Plenty |
| Length | 65 km (40 mi) |
| Basin size | 906 km2 (350 sq mi) (measured up to Awakaponga) |
| Discharge | |
| • average | 26 m3/s (920 cu ft/s) |
It flows from Lake Tarawera, northeastwards across the northern flanks of the active volcano Mount Tarawera, and past the town of Kawerau before turning north, reaching the Bay of Plenty 6 kilometres (4 mi) west of Edgecumbe.
The Tarawera Falls on the river are considered to be quite spectacular.
Environmental issues
editThe Tasman Pulp and Paper Mill, now owned by Norske Skog, has been discharging waste into the river since 1955.[1] Local residents have erected signposts labelling the river as the "Black Drain" since the 1990s.[2]
The dark colour is due to the presence of pollution from farms, sewage and stormwater but it is predominantly from pulp and paper mill effluent. As of 1997, pulp and paper mills were discharging over 160 million litres of industrial waste into the river per day.[3] By 2006, the oxygen levels in the river had reached a level where fish could survive, however the water colour was still dark. Since 1998 the colour and light penetration (euphotic depth) have improved in the lower section of the river due to less pollution from the Tasman Mill.[2]
In 2009, the mill gained permission to continue polluting the river for the next 25 years.[4] In 2010, local iwi took a case to the High Court to shorten the 25 year water discharge permits issued under the Resource Management Act but the appeal was rejected.[1]
Geology
editThe Tarawera River drains the north-eastern aspect of the Taupō Rift with its river mouth west of Matata. The river commences at the north-east arm of Lake Tarawera with a mean outflow of 7 m3/s (250 cu ft/s),[5]: 491 from effectively a watershed of the Ōkataina Caldera, with its risk of volcanic activity disrupting river flow. At this normal or less flow the river disappears underground into caves in the rhyolite lava flow just before the Tarawera Falls.[5]: 491 [6] It usually emerges about halfway up the full falls drop,[6] but can with recent rain fully occupy the drop. There have been two known major floods following the breakdown of temporary volcanic material dams at the lake outlet.[5]
The first, and larger, followed the 1314 ± 12 CE[7]: 4 Kaharoa eruption.[5]: 491–2 The present river start is where the Tapahoro lava flow, created by the 5526 ± 145 BP[7]: 4 Whakatane eruption,[5]: 492 runs into a 14,009 ± 155 BP[7] Pokohu lava flow. The Tarawera River flows across this in a 10 m (33 ft) wide channel.[5]: 492 The 1314 eruption blocked the outlet with a temporary dam up to 32 m (105 ft) above present outlet levels, which was subsequently eroded with a great flood that created a 350 m (1,150 ft) wide, and almost 40 m (130 ft) deep valley spillway at the start of the river.[5]: 497 It seems the river during this flood overflowed to the east draining for a time through the Awiti Ravine, and back into the Tarawera River flood plain by the present Waiaute Stream that drains the eastern slopes of Mount Tarawera.[5]: 500 However it also evacuated 3 km (1.9 mi) downstream from the lake at the terminus of the Pokohu lava flow the amphitheatre of the Tarawera Falls.[5]: 500 The flood deposited large boulders up to 20 m (66 ft) in diameter for 1 km (0.62 mi) below the falls and up to 13 m (43 ft) to 8 km (5.0 mi) below the falls.[5]: 497
The lake outlet was blocked again after the 1886 eruption of Mount Tarawera, and the lake level increased to a maximum of 12.8 m (42 ft) above its present level.[5]: 491–2, 4 This volcanic debris dam (the debris that blocked the outlet were not just from the eruption directly but included those washed down from a creek that runs into the lake by the outlet), first broke on 1 November 1904, with a main flood surge on 3 November 1904 which was assessed at a peak flow of 700 m3/s (25,000 cu ft/s).[5]: 504 This flood resulted in the raising of the river bed (aggradation), and sedimentation problems to 50 km (31 mi) downstream of the lake.[5]: 504
References
edit- ^ a b "Iwi not giving up fight against Tasman mill discharges". Radio New Zealand. 18 December 2010. Retrieved 18 December 2010.
- ^ a b Park, Stephen (February 2008). "Colour and Clarity of the Tarawera River 1991-2008" (pdf). Environment Bay of Plenty.
- ^ "The State of New Zealand's Environment". Ministry for the Environment (New Zealand). 1997. Archived from the original on 2008-10-16. Retrieved 2008-03-23.
- ^ "Mill gets 25-year pollution consent - Business - NZ Herald News". Nzherald.co.nz. 2009-10-16. Retrieved 2013-09-06.
- ^ a b c d e f g h i j k l m Hodgson, K. A.; Nairn, I. A. (2005). "The c. AD 1315 syn‐eruption and AD 1904 post‐eruption breakout floods from Lake Tarawera, Haroharo caldera, North Island, New Zealand". New Zealand Journal of Geology and Geophysics. 48 (3): 491–506. doi:10.1080/00288306.2005.9515128.
- ^ a b "Tarawera Outlet to Falls Track". Department of Conservation NZ. Retrieved 2023-08-23.
- ^ a b c Villamor, Pilar; Litchfield, Nicola J.; Gómez-Ortiz, David; Martin-González, Fidel; Alloway, Brent V.; Berryman, Kelvin R.; Clark, Kate J.; Ries, William F.; Howell, Andrew; Ansell, India A. (2022). "Fault ruptures triggered by large rhyolitic eruptions at the boundary between tectonic and magmatic rift segments: The Manawahe Fault, Taupō Rift, New Zealand". Journal of Volcanology and Geothermal Research. 427: 107478. doi:10.1016/j.jvolgeores.2022.107478. hdl:2292/59828. ISSN 0377-0273. S2CID 246258923.
External links
edit
Media related to Tarawera River at Wikimedia Commons
