Mangaweka deviation
Encyclopedia
The Mangaweka Deviation is a 7 km single track deviation of the North Island Main Trunk (NIMT) railway line in the central North Island
of New Zealand
, between the settlements of Mangaweka
and Utiku, south of Taihape
. It was constructed between 1973 and 1981 primarily to move the line away from geologically unstable land; and is the most recent of the significant deviations of the NIMT since it was opened in 1909.
north to Taihape was built to the west of the Rangitikei River
and lies predominantly on the terraces within the river valley. Only south of Marton does the NIMT cross the Rangitikei en route to Palmerston North
and Wellington
.
Between the settlements of Mangaweka and Utiku the western river terrace is largely non-existent with steep hill country running into tall river cliffs. The topography is also compounded by the confluence of the Kawhatau River with the Rangitikei. However despite these obstacles surveyors were able to identify a route that kept the line to the west of the river along the cliff tops; albeit one that included a climb at each end of the section, a viaduct, and several tunnels.
By the 1960s concerns existed about the long-term stability of the land the section ran through. While the general Mangaweka area was susceptible to slips due to its steep hilly nature, rainfall and underlying geology the railway, by virtue of its cliff top nature and several tunnels, was thought to be under particular threat from erosion and collapse.
At the same time concerns were also being voiced over State Highway 1 as the steep, narrow and twisting alignment was also prone to slips – having been built after the railway in the same area though further to the west – and naturally imposed speed restrictions that were exacerbated by heavier vehicles and creating bottlenecks.
As a result investigations were commenced into improving both routes, including the feasibility of a joint rail-road alignment.
The NIMT route chosen was from one of the joint options given and was constructed between 1973 and 1981. The new alignment crossed the Rangitikei River twice and the Kawhatau River once - requiring the construction of three massive viaducts - and also removed the gradients at each end of the section.
From the south, the deviation leaves the old alignment at the base of the Mangaweka climb just north of the SH1 level crossing and passes much closer to the settlement than it did previously. It then passes under SH1 before crossing the South Rangitikei viaduct, which is a 78m tall, 315m long triple-span structure. It then runs along the eastern river terrace for about 2 km before crossing the Kawhatau (73m) and North Rangitikei (81m) viaducts in quick succession. Both viaducts are 110m long single-span structures, with the North Rangitikei viaduct becoming the highest on the NIMT. The line rejoins the original NIMT alignment a further 1 km north, just to the south of Utiku.
The section was subsequently electrified as part of the NIMT electrification carried out between 1984 and 1988.
Following the deviation’s opening in 1981 work commenced on the removal of the former alignment with the lifting of the line. The Mangaweka viaduct was demolished in 1982.
North Island
The North Island is one of the two main islands of New Zealand, separated from the much less populous South Island by Cook Strait. The island is in area, making it the world's 14th-largest island...
of New Zealand
New Zealand
New Zealand is an island country in the south-western Pacific Ocean comprising two main landmasses and numerous smaller islands. The country is situated some east of Australia across the Tasman Sea, and roughly south of the Pacific island nations of New Caledonia, Fiji, and Tonga...
, between the settlements of Mangaweka
Mangaweka
Mangaweka is a township on State Highway One , in the North Island of New Zealand, with a population of just over 200. It is between Taihape to the north and Hunterville to the south...
and Utiku, south of Taihape
Taihape
Taihape is the Northern gateway town of the Rangitikei District, located near the middle of the North Island of New Zealand. It services a large rural community and lies on State Highway 1, which runs through the centre of the North Island.- Economy :...
. It was constructed between 1973 and 1981 primarily to move the line away from geologically unstable land; and is the most recent of the significant deviations of the NIMT since it was opened in 1909.
History
The original section of the line was constructed as part of the NIMT in 1904. The entirety of the route from MartonMarton, New Zealand
Marton is the hub of the Rangitikei district of the Manawatu-Wanganui region of New Zealand's North Island. It is situated 35 kilometres southeast of Wanganui and 40 kilometres northwest of Palmerston North. The population was 4752 .-History:...
north to Taihape was built to the west of the Rangitikei River
Rangitikei River
The Rangitikei River is one of New Zealand's longest rivers, 185 kilometers long.Its headwaters are to the southeast of Lake Taupo in the Kaimanawa Ranges. It flows from the Central Plateau south past Taihape, Mangaweka, Hunterville, Marton, and Bulls, to the South Taranaki Bight at Tangimoana, 40...
and lies predominantly on the terraces within the river valley. Only south of Marton does the NIMT cross the Rangitikei en route to Palmerston North
Palmerston North
Palmerston North is the main city of the Manawatu-Wanganui region of the North Island of New Zealand. It is an inland city with a population of and is the country's seventh largest city and eighth largest urban area. Palmerston North is located in the eastern Manawatu Plains near the north bank...
and Wellington
Wellington
Wellington is the capital city and third most populous urban area of New Zealand, although it is likely to have surpassed Christchurch due to the exodus following the Canterbury Earthquake. It is at the southwestern tip of the North Island, between Cook Strait and the Rimutaka Range...
.
Between the settlements of Mangaweka and Utiku the western river terrace is largely non-existent with steep hill country running into tall river cliffs. The topography is also compounded by the confluence of the Kawhatau River with the Rangitikei. However despite these obstacles surveyors were able to identify a route that kept the line to the west of the river along the cliff tops; albeit one that included a climb at each end of the section, a viaduct, and several tunnels.
By the 1960s concerns existed about the long-term stability of the land the section ran through. While the general Mangaweka area was susceptible to slips due to its steep hilly nature, rainfall and underlying geology the railway, by virtue of its cliff top nature and several tunnels, was thought to be under particular threat from erosion and collapse.
At the same time concerns were also being voiced over State Highway 1 as the steep, narrow and twisting alignment was also prone to slips – having been built after the railway in the same area though further to the west – and naturally imposed speed restrictions that were exacerbated by heavier vehicles and creating bottlenecks.
As a result investigations were commenced into improving both routes, including the feasibility of a joint rail-road alignment.
Construction and new alignment
From a number of options put forward different routes were chosen for SH1 and the NIMT, as it proved possible to reconstruct SH1over much of its existing alignment. The SH1 works were completed in stages between 1972 and 1980.The NIMT route chosen was from one of the joint options given and was constructed between 1973 and 1981. The new alignment crossed the Rangitikei River twice and the Kawhatau River once - requiring the construction of three massive viaducts - and also removed the gradients at each end of the section.
From the south, the deviation leaves the old alignment at the base of the Mangaweka climb just north of the SH1 level crossing and passes much closer to the settlement than it did previously. It then passes under SH1 before crossing the South Rangitikei viaduct, which is a 78m tall, 315m long triple-span structure. It then runs along the eastern river terrace for about 2 km before crossing the Kawhatau (73m) and North Rangitikei (81m) viaducts in quick succession. Both viaducts are 110m long single-span structures, with the North Rangitikei viaduct becoming the highest on the NIMT. The line rejoins the original NIMT alignment a further 1 km north, just to the south of Utiku.
The section was subsequently electrified as part of the NIMT electrification carried out between 1984 and 1988.
Following the deviation’s opening in 1981 work commenced on the removal of the former alignment with the lifting of the line. The Mangaweka viaduct was demolished in 1982.