TheBuller River (Māori:Kawatiri) is ariver in theSouth Island of New Zealand.[1] The Buller has the highest flow of any river in the country during floods,[2] though it is only the 13th longest river; it runs for 177 km (110 mi) fromLake Rotoiti through theBuller Gorge and into theTasman Sea near the town ofWestport.[3] Asaddle at 710 m (2,330 ft) separates the Buller from theMotupiko River and that is divided from theWairau River by a 695 m (2,280 ft) saddle, both aligned along theAlpine Fault, as is the top of the Buller valley.[4]
Within the Buller Gorge and downstream from theDeepdale River joining, the Buller crosses fromTasman District intoBuller District. ThePaparoa Range separates the Buller River from theGrey River. A number of flora and fauna are found in the Buller catchment, many of these extending onto the slopes of the Paparoa Range.
The Buller River upstream fromMurchison along with theMangles River are popular forwhitewater kayaking and recreationalfishing,[5] though the whole river can be kayaked; it is the only major river in the country with no hydro lakes,[6] though a seismic survey for hydro power was done in 1973.[7] For experienced canoeists the Ariki Falls section, between Murchison and Newton Flat, is also popular and novices can use it by carrying kayaks around the rapids, except when the river is very low and the rapids become unnavigable.[6] The river is suitable for contact recreation approximately 95% of the time, thoughTasman Council recognises it needs to be better because of the popularity of whitewater kayaking belowGowan Bridge.[8]
This river has an annual mean flow of 454 cubic metres per second (16,000 cu ft/s), is estimated to have reached 12,700 m3/s (450,000 cu ft/s) in the 1926 flood[12] and has the highest flood flow in the country of over 7,640 cubic metres per second (270,000 cu ft/s).[2] 93% of the water comes from the western mountains, which make up only 38% of the catchment, and it is highest in summer, partly due to melting snow.[13]
Excavations at the mouth of the river, across from Westport, uncovered 77 stoneadzes, 2,693 stone flakes (argillite,chert,obsidian andsilcrete from manufacture of stone tools), minnow lures,moa bone, sites of huts, ovens,middens andurupā, with one shellcarbon dated to between 1219 and 1316. Early trading is indicated by argillite from Ohana, at the south end ofD'Urville Island, chert from upper North island and obsidian fromMayor Island / Tūhua. In 2004 the site was described as one of the largest and best preserved largeArchaic sites in the country. More investigation may reveal whether it was occupied for more than a few years.[14][15]
Subsequent pre-colonial history is obscure. TheWaitangi Tribunal concluded that, "very little is known about the history ofNgāti Apa's occupation of the region . . .invasion by northern tribes in the early nineteenth century made it difficult to pass on any substantial record of the traditional history of this area" and it was "probably an area of migratory resource use rather than permanent occupation".[16] One migratory resource wasNgāi Tahu'spounamu trade, which had a greenstone trail through the valley,[17] probably in summer, when the river would usually be lower.[18] By virtue of ataua of 1829–1832,Ngāti Toa Rangatira was recognised in 2012 as having an interest in the upper part of the river.[19]
Europeans first discovered Lake Rotoiti in 1842.[20] The first written record of the river mouth was in 1845, when asealing captain, Joseph Thoms, was reported as finding, "a large river, a mile wide. It has a bar at the entrance, on which he took soundings, and found sixteen feet at high water. The river appeared to be navigable for a considerable distance. Mr. Thoms anchored his vessel in five fathoms, and pulled up four or five miles in his boat. He describes the valley through which the river runs to be twenty miles wide, finely wooded, with some open land."[21]
In 1846 Brunner was the first European to follow the full length of the Buller, together with his guide, E Kehu, ofNgāti Tūmatakōkiri, who already knew the area well[20] (Ekehu had been taken prisoner by Ngāi Tahu while living near the Grey River).[22] That expedition lasted almost 560 days.[23] The journey was so difficult that they left Lake Rotoiti on 31 December 1846, but only reached the mouth of the river on 4 June 1847.[24] They returned up the Buller, leavingInangahua on 23 March 1848 and reached Lake Rotoiti again on 12 June 1848.[23]
SurveyorJohn Rochfort discovered gold and coal in the Buller valley in 1859.[25] Despite this indication of the land's value, the 1860Arahura Deed sold most of the West Coast to the government for £300 (about 1d per 100 acres), covering a total of 7,000,000 acres (2,800,000 ha), which included virtually all of the Buller valley south from the Gowan River.[26]
AWest Coast gold rush, coal mines and timber sawmills resulted in a rapid population increase in the 1860s. By 1867 there were 6,087 miners inNelson Province and 10,466 people (and 1,612 tents, indicating the temporary nature of their stay) inWestland North, which also included the Grey valley. About 1,500 were in Westport in 1867, which was then the 3rd largest port for exporting gold, afterHokitika andDunedin.[27]
The originalMāori name for the Buller may have beenKawatiri, althoughPatrick O'Regan thought that was a misunderstanding of Ka Awatiri.[29] He translatedAwatiri as a rapid river. The first 1846 expedition named the Buller valley around Murchison as the Aglionby valley, after the English MP,Henry Aglionby Aglionby.[28] In 1911 O'Regan suggested it had dropped out of use because it was hard to pronounce.[29]
Organs Island was created, about 6 km (3.7 mi) upstream from Westport,[30] when a loop in the Buller was bypassed[31] by a straight flood relief channel built between 1882[32] and 1886.[33] The old river course became silted up between 1925[34] and 1945,[35] but part of it remains to allow Buller floodwater to overflow into theOrowaiti River. A wall in that overflow was repaired in 2022 after flooding.[36]
Until roads were built, goods were carried from Westport toLyell in fleets of canoes,[37] or, later, horse-drawn boats, carrying up to 7 tons,[38] or 12 tons up to Inangahua.[39] They could take 11 weeks to make the journey,[40] but the 40 mi (64 km) from Lyell could also be covered in 7 hours downstream.[41]
Roads in the valley evolved. In good weather a footpath was passable along the length of the valley by 1864.[42] Horses could usually travel from Nelson to Lyell by 1867[43] and wheeled traffic by 1876.[44] Adray road opening from Inangahua to Lyell in 1878 facilitated animal-drawn transport vehicles.[45]
Job Lines began a link between Westport andReefton in 1876, using horses from Westport and a coach from theLanding to Reefton.[47] By July 1877 the road through the Lower Gorge had improved sufficiently for the coach to run through to Westport.[48] The road near Tiroroa included two short tunnels,[49] until Fern Arch was demolished in 1937.[50]
The firstNewman Brothers coach ran betweenFoxhill (end of theNelson railway) and Hampden (Murchison) on 22 July 1879,[51] following improvements to the road,[52] was extended to Lyell in 1880 and, by Job Lines, to Reefton in 1882.[53][54] A motor service began in 1913, allowing the journey between Westport and Nelson to be made in a day.[55] A daily bus linking Nelson and Westport began in 1923.[56]InterCity now runs buses on 4 days a week, taking 3 hours 29 minutes, including a 15 minute break at Murchison.[57] By car the 217 km (135 mi) route takes a bit under 3 hours.[58]
Newman Brothers coach on the Nine Mile punt about 1910The first bridge up the river is Buller Bridge, opened in 1888 as aroad-rail bridge[60] on theCape Foulwind Railway and built by M'Lean and Son of Wellington for £13,704 15s 6d.[61] It was a 1,040 ft (320 m) long, ironlattice bridge.[62] That original bridge was replaced in 1976 by a concrete road bridge, slightly upstream.[63] A ferry, and later apunt, crossed the river from Nine Mile Road,Te Kuha,[64] from 1874.[65] The punt was swept away in a 1908 flood,[66] five horses were drowned and the coach was left in shallow water.[67] It also broke free, or was damaged, in 1909[68] and 1926 floods.[69] The last punt was built about 1914[70] and it closed in 1927.[71]
By 1911 there was a 725 ft (221 m)suspension bridge over the river,[72] just downstream from Buller.[73] Between 1928[74] and 1931 a 540 ft (160 m) suspension footbridge was also built over the river, 19 mi (31 km) from Westport, to link the railway construction workers' camp to the railway.[75] It's sometimes not clear in accounts which bridge is being described.[76] Both bridges had gone by 1972.[77]
Buller River bridge No.89, on theStillwater–Ngākawau Line, crosses the river near Inangahua. It is 206 m (676 ft)[78] long, on 6 x 100 ft (30 m) spans, resting on 8 ft (2.4 m) diameter piles.[79]
Lyell punt and bridge about 1890. It is now the oldest bridge over the riverIron Bridge at Lyell, onSH6,[80] was built byJ & A Anderson of Christchurch for £8,957[81] and replaced the punt on 4 August 1890.[82] TheWarren truss bridge spans 168 ft (51 m),[83] supported by a central pier in the river.[84]
Buller Gorge Swingbridge (suspension bridge) is about a kilometre below Ariki Falls.[85] It is 110 m (360 ft) long and 19 m (62 ft) above the river.[86]
O'Sullivan's Bridge, also on SH6,[87] was built in 1908[88] and rebuilt in 1975.[89]
Longford Bridge, also on SH6,[90] was rebuilt in 1966. Thepre-stressed concrete,box girder bridge is 316 ft (96 m) long, with a main span of 170 ft (52 m),[91] 42 ft (13 m) above normal water level. It was built 1 mi (1.6 km) upstream of the 1899 single-lane, wooden,suspension bridge and cost £47,490.[92]
Nuggety Creek Bridge was built about 1919[93] to give access to Nuggety Creek Road[94] and now has a 25 tonne weight limit.[95]
Gowan Valley Bridge was built between 1914[96] and 1917.[97]
Harleys Rock Bridge at Devils Grip, onSH63,[98] was first built about 1875[99] and upgraded about 1928.[100] The present concrete bridge was built in 1979.[101]
Upper Buller Bridge in 2011Upper Buller Bridge is on SH63. It was built in 1868[102] and rebuilt in 1928[100] and 1981.[103]
Buller Bridge on Mount Robert Road[104] was built about 1955[105] and rebuilt in 2015.[106]
Lake Rotoiti was created by a glacier and glacial moraines occupy a large area between the Buller and Gowan rivers.[123] From the lake the Buller flows west through a gorge cut ingranitic rocks of theMedian Batholith. It then turns southwest to follow the axis of the LongfordSyncline to Murchison. Tributary valleys around Murchison commonly follow north-south trending faults and fold axes.[4]
The Buller's deep gorges have been cut through the mountains as they have been raised byQuaternary faulting and folding. Some 350,000 years ago the river had wide floodplains,[124] which remain as flatterraces above the narrow gorge, as at Manuka Flat, now roughly 300 m (980 ft) above the river.[125] The Murchison Basin was filled between theLate Eocene andEarly Miocene by sediments in increasingly shallow waters, indicating that the uplift of the area to the north began in the Early Miocene.[126] It was particularly rapid during the late Miocene-Pliocene.[127]
In the1929 Murchison earthquake a 1.6 km (0.99 mi) landslide fell 550 m (1,800 ft) to dam the Buller at Fern Flat, about midway between Murchison and O'Sullivan's Bridge. After two days the dam was washed away. The road between Murchison and Inangahua had 34 landslips, some up to 600 m (2,000 ft) wide.[128] The road at White Creek, in the Upper Gorge, was split by a 4.5 m (15 ft) scarp.[129] There were also slips in the1968 Inangahua earthquake, one of which created a 30 m (98 ft) high dam in the river, just above Inangahua.[130]
Above the Lower Gorge,podzol soils lie on sandstones of theBrunner Coal Measures. They are very infertile, acidic and tend to be very poorly drained. At high altitudes, the soils become skeletal and, in many places, unweathered rocks lie on the surface. Brunner Coal Measures are Eocene and were deposited in an estuary.[114] There were coal mines near the Lower Gorge[131] at Rahui (opened 1942)[132] and Cascade (originally opened to improve mine drainage in 1897).[133]
Uranium was found in the Lower Gorge in 1955 and searches were made for viable deposits until the 1970s,[134] but all were less than 0.1% U3O8.[124] In 1972 the mountains on either side of the Gorge wereofficially named Mounts Cassin[135] and Jacobsen, after the men who discovered the uranium.[136]
In July 2001 the BullerWater Conservation Order came into force, listing the waters of the Buller River and tributaries that are to be retained in their natural state or protected because of the outstanding characteristics, features and values of the waters.[137]
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