Lower Kaituna River

A beautiful part of the North

The Kaituna River, located in New Zealand’s Bay of Plenty region on the North Island, originates from Lakes Rotorua and Rotoiti. Flowing northwards for 45 kilometers, it ultimately empties into the Bay of Plenty near Maketu. Perfect for nature lovers and adventure seekers, the Lower Kaituna River offers stunning views and a peaceful escape into New Zealand’s natural beauty.

History of Lower Kaituna River Diversions

1800s 1880

The Crown made swamp land in Lower Kaituna available for European settlement, expecting it to be drained and used for farming.

1900s 1906

The first Tumu-Kaituna Drainage Board meeting is held, with trustees Robert King (chair), C.F. Tuthill, H.A. Vercoe, James Dudson, and B.G. Pinker elected. The board’s goal: drain land east of the Kaituna River.

1900s 1907

On 15 February, after a heavy storm, the Kaituna River naturally broke through the sand spit at Te Tumu, cutting off flow to the estuary. The SS Katikati was the first to navigate the new channel to Canaan landing. By October 1907, a twice-weekly service was operating via this route, marking the decline of Maketu as a port and ending plans for a wharf there.

1900s 1912

On 24 January, George P. Ford of Maketu offers his launch Puke Lass (formerly Reremoana) for tourist and fishing trips. Powered by a 15hp Union engine, the vessel completes the Te Tumu to Victoria Wharf (Tauranga) journey in just over three hours.

1900s 1916
On 7 November, the Te Tumu–Kaituna Drainage Board elections saw William Kelly, Mapson W. Griffin, Herbert A. Vercoe, James Paterson, and Charles R. Vercoe elected. Unsuccessful candidates included Charles F. Tuthill, Robert S. Ross, Edwards G. Cruickshank, and James Dudson.
1900s 1917

On 19 February, the Te Puke and Te Tumu–Kaituna Drainage Boards review a report by Chief Drainage Engineer J.B. Thompson on plans to lower the Kaituna River to improve swamp drainage. He proposes short diversions, easing bends, clearing snags, and building stop banks. However, as neither board controls the river itself, he recommends forming a dedicated River Board.

1900s 1919

On 8 April, the Kaituna River Board is established to oversee dredging and lowering of the river. Elected members include Herbert B. Bayliss, B. Vercoe, Joseph O’Shaughnessy, W. Kelly, R. King, M. Griffin, and A.P. Knight. Government drainage plans are reviewed and sent to committee for further assessment.

1900s 1920

8 June: Torrential rain causes the river to flood. “The worst flooding we’ve ever experienced around the house.”

1900s 1922

Settlers in Lower Kaituna formed a working bee to cut a new outlet to the sea at Te Tumu, aiming to reduce flooding after the river mouth had shifted east. But when Jack Ford and his father visited on opening day in August, the river didn’t flow as expected.

1900s 1926

The Kaituna River District Board created two parallel channels—known as Ford’s Cut or the Twin Cut—through land leased by Mr Ford to redirect water into the estuary. By then, the river had already naturally reconnected to the estuary via the Papahikahawai channel.

1900s 1926
All Kaituna River flow was redirected to the estuary via Papahikahawai and Ford’s Cut. A new channel from the Atuaroa Stream to the river was also constructed for the Te Puke Drainage Board, extending west across the railway with a new bridge near The Mount Shops (Public Works Statement, p.40).
1900s 1927

3 November – Te Puke Times: The Kaituna River Diversion officially reopens to its original outlet at Maketu. Following speeches, the crowd gathers for a tapu lifting ceremony. A launch carrying officials from the Kaituna River Board, Arawa Trust Board, and local chiefs heads to the river mouth. After a ceremonial cannon blast, the launch—followed by two others—sails out to sea, then turns to re-enter the new channel.

1900s 1928

The Kaituna River Board dredged the Lower Kaituna, cutting through sharp bends from Te Kopua Canal to Te Tumu. However, a storm in early March 1928 caused the river to naturally divert back to its former outlet.

1900s 1929

13 December – Flax planting is completed across 1,350 acres of the Kaituna plantation, with the oldest plants now three years old. A new flax mill is planned for construction in the coming year.

1900s 1931

21 August – Te Puke Times: Flaxlands Development Ltd acquires Broad and Berquist’s old flax mill at Bell’s Landing, Papamoa, and establishes a modern facility managed by F.W. Douglas of Mercer. A new process for producing wool packs and corn sacks from flax at lower costs is expected to bring significant commercial value to the industry. The mill is connected to electricity in September 1932.

1900s 1941

6 May – Members A.J. Collins, M.G. Cruickshank, W.J. Ford, E.H. Hintz, David M. Steel, and Wallace Williams are re-elected to the Kaituna River Board.

1900s 1950

In 1950, the Tumu-Kaituna and Te Puke Drainage Boards merged with the Kaituna River Board to create a more efficient and unified response to the upcoming Murray Report. Now overseeing all drainage in the region, the board aims to reduce maintenance costs through a centralised drain-cleaning operation.

1900s 1951

6 July 1951 – After two and a half days of heavy rain, Te Puke experiences its worst flooding since 1907. The Kaituna River and the Waiari and Raparapahoe streams overflow, cutting off the town and leaving it without power for 18 hours. Roads at Long Swamp, Papamoa, and Canaan Landing are severely flooded, with only limited truck access. Pukehina and Pongakawa are also heavily affected.

1900s 1953

Since May, the Kaituna Basin has remained flooded, with 14,000 acres underwater and farmers facing severe stock losses. Government aid is sought to support those affected.

1900s 1955

19 May – The Government approves a £3-for-£1 subsidy, covering up to £60,000 of the estimated £79,930 cost for the Kaituna Flood Protection Scheme. At the time, 8,000 acres remain flooded—one farm with 110 cows has just two acres above water.

1900s 1956

The Te Tumu diversion redirected all Kaituna River flow out to sea, with Ford’s Cut and Papahikahawai blocked. Designed to reduce flooding on surrounding land, only minimal seepage or overflow into Ford’s Cut occurred during flood events.

1900s 1957

1 February – The Kaituna River diversion officially opens at Te Tumu. What begins as a trickle soon becomes a wide, raging torrent, swiftly carrying water to the sea. The $50,000 project—largely funded by affected farmers—aims to prevent flooding across 16,000 acres of fertile farmland. Fittingly, local farmer Jack Pittar, long impacted by floods, is the first to navigate his launch through the new outlet.

1900s 1958

The Kaituna River Board is dissolved, with its responsibilities transferred to the Tauranga County Council. To support the Council, a local advisory committee is elected by district ratepayers. Members include Councillors G. Don Vercoe and A. Gordon Spratt, along with A.E. Clague, H.M. (Mick) Collings, Eddie H. Hintz, and R.S. (Bob) McCosh.

1900s 1960

The 1960s saw major upgrades to Te Puke’s roading infrastructure. The frequently flooded Canaan Landing swamp was raised and reinforced, an unused section of the old Māori track to Te Puke was closed at Te Tumu, and the final small wooden bridge over the railway line was removed.

1900s 1962

1 June 1962 – A severe storm cuts off Te Puke for 24 hours, with 9 inches of rain recorded in a single day. A man in Ohope Beach is killed when a clay cliff collapses behind his home. Te Puke residents Mr and Mrs H.H. Anderson, returning from Rotorua, are trapped between two landslides and forced to spend the night in their car.

1900s 1971

3 September – Te Puke Times: The Government approves, with some modifications, the Bay of Plenty Catchment Commission’s $2.3 million flood control and drainage scheme for the Lower Kaituna River. Funded on a 3-to-1 subsidy basis, Commission Chairman Charles W. Mundt is confident their share will be raised with ease. The first step is classifying the 19,000 acres included in the plan. Once complete, the scheme will protect some of the region’s best dairying land, which has faced up to five floods annually in recent years.

1900s 1981

Planned in the 1970s and launched in 1981–82 after Ministry of Works & Development approval, the Kaituna Scheme aimed to prevent flooding and convert swampland between Te Puke and the coast into productive pasture. Key works included further straightening of the Kaituna River—most notably a cut 400–900m from its mouth—realignment of tributaries, and construction of stop banks.

1900s 1984

A parliamentary petition with 3,000 signatures is presented, calling for the Kaituna River to be re-diverted back into the estuary.

1900s 1990

DOC applies for consent to partially re-divert the Kaituna River back into the estuary, requesting approval to redirect 400,000 cubic metres of water per tidal cycle.

1900s 1996

NIWA was engaged to investigate erosion on the Ford family property. The report found the main causes to be ocean wave action entering the river mouth and likely eddies forming during floods—both intensified by increased flood peaks caused by the Kaituna Scheme. NIWA concluded the scheme is the root cause of the erosion. Meanwhile, DOC was granted consent for a partial rediversion of 100,000 cubic metres per tidal cycle, limited by water quality concerns.

2000s 2004

24 July – Heavy weekend rain followed by a swarm of shallow earthquakes, the strongest at magnitude 5.4, forces the evacuation of 1,500 people in the Eastern Bay. The disaster claims two lives and causes damage estimated in the tens of millions. In Maketu, a major landslip leaves a home teetering on a cliff’s edge, while Te Puke dairy farmers, in the midst of calving season, struggle with no safe areas for their cows or calves.

2000s 2005

7 April – Bay of Plenty Times: A new tsunami warning system will be installed along the Western Bay coastline, with ten sirens set to provide up to four hours’ notice for evacuation. This makes the region the first in New Zealand to implement a fully coordinated alert system. Authorities highlight the area’s vulnerability to tsunamis triggered by earthquakes, volcanic activity, and undersea landslides.

2000s 2007
The construction of the Ōhau Diversion Wall was initially believed to worsen river water quality by increasing nutrient loads; however, studies later confirmed the impact to be minimal.
2000s 2009

The Kaituna Maketū Joint Council Committee, along with the Chair of the Working Party, hears public submissions on the draft Kaituna River and Ōngātoro/Maketū Estuary Strategy.

2000s 2012

The Regional Council agrees to fund the partial re-diversion of the Kaituna River in its 2012–2022 Ten Year Plan. The project aims to maximise river flow to the estuary, keep the Te Tumu Cut open, and preserve existing flood protection levels.

2000s 2013

Re-diversion options were explored through meetings with the community, iwi, and landowners, with feedback helping to shape the preferred approach. Consultants conducted Cultural Impact Assessments, ecological studies, and modelling, while regular updates kept the community informed throughout the process.

2000s 2014

January–May: Ongoing community updates.
April–June: Resource consent application and designation notice prepared and lodged. Construction requirements confirmed and environmental assessments finalised.
July–September: Public notification and 20-day submission period.
December: Consent and designation hearings held, if required.

2000s 2015

February–March: Resource consent decision issued and designation recommendation made. The Regional Council reviews and responds to the recommendation.
April: Appeals, if any, are lodged with the Environment Court.
August: Environment Court hearing held, if required.

2000s 2016

Construction begins, followed by implementation of the re-diversion and ongoing environmental monitoring.

  • Lower Kaituna River
  • Lower Kaituna River Diversions
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