The Mangapà Âike River is a river beginning in the Gisborne Region of New Zealand's North Island. It flows generally southwest from sources south of Waingake, reaching the Wairoa River in Hawke's Bay northeast of Frasertown. Mangapà Âike River was Gazetted as an official name on 28 November 2022.
Whakapunake at is the highest point in the catchment, with the Mangarangiora Stream draining its eastern slopes into the Mangapà Âike. Whakapunake is traditionally where MÃÂui snagged his fish hook. It is the northern boundary of NgÃÂti Kahungunu's rohe. A transmitter mast was built at the south end of Whakapunake in 1969. It is now operated by Kordia. In the river's main catchment, Pà «karoronui is the highest point.
The main geological influence on the river is that it drains from the Mangaone Anticline to the Wairoa Syncline. Below Tukemokihi the river runs through Cenozoic limestones. From Tukemokihi, upstream, the rocks are Miocene mudstones and sandstones.
Lake Te Horonui formed after 25 February 2018, when about of a sandstone hill slipped and dammed the river. The trigger for the landslide is unknown as there were no significant rainfall events or earthshaking events in the year prior to the Mangapoike Rockfall occurring.The landslide was probably due to the river cutting into the foot of the dip slope, where water trapped in the sandstone by an impermeable mudstone may have lubricated the bedding plane. After over of rain fell on 9âÂÂ10 March, the deep lake grew from to and soon to . The bridge to Mangapà Âike Station might have flooded if a channel hadn't been blasted on 28 March and 9 April, allowing water into another new lake, Tukemokihi, and lowering Lake Te Horonui back to . Part of the detached slide block remained as a mass of around 8.5 million tonnes. The new lake is being used by grebes. The name Lake Mangapà Âike was also considered, but The Minister for Land Information, Damien OâÂÂConnor, agreed to the new name, which refers to the landslide.. The lake was not named formally initially as it was regarded as being likely ephemeral. Ie not long lived. That looks likely to be the case as subsequent storms have resulted in the lake being infilled by sediment. It is likely that the temporary lake will be completely infilled within the next 10 years.
There are three gravel roads in the valley, but they have no direct link to each other. From the tar-sealed Tiniroto Road, Kotare Road runs a few kilometres east. It ends at a gorge (named by one study as Haupatanga), which is over deep and largely inaccessible. Mangapà Âike Road runs through the Makaretu Stream valley to join the Mangapà Âike valley and then along the south bank of the river to Tukemokihi. The upper catchment is partly accessed by Paparatu Road.
A preliminary survey for the Napier-Gisborne railway in 1905 favoured using the valley, with a tunnel linking it to Te ÃÂrai valley. It was rejected in 1912, in favour of Hangaroa, Waikura and NgÃÂtapa, as they served an area thought to have more economic potential.
There were two small schools in the valley. Paparatu School was on Paparatu Road. It was built in 1938, had 14 on its roll in 1947 and closed between 1978 and 1986. Tukemokihi School was open by 1931. It closed at the end of 2006 and was given back to its previous landowners in 2012.
Paparatu was the scene of an ambush on Te Kooti in 1868, after his escape from RÃÂkohu.
Gisborne's water supply comes partly from reservoirs at the head of the valley. Water was first piped from the Mangapà Âike valley in 1917. In October 1942 ratepayers approved a ã45,000 loan for a 246 million gallon reservoir, designed by G. F. Clapcott, the borough engineer, with a pipeline and an tunnel to Te ÃÂrai valley. The arch dam is , or high, covers and filled in May 1948. A new pipeline and a tunnel now connects the 1948 Clapcott Dam, the 1972 Sang Dam () and the HC Williams Dam, built in 1974 (). In 2023 Cyclone Gabrielle damaged 9 of the 21water pipe bridges in the network and left two of reservoirs with cloudy water. Sang has an earth dam.
The Cyclone also left forestry slash backed up for more than at the bridge where the Mangapà Âike joins the Wairoa. Te Puna Bridge, near Tukemokihi, had a pier damaged.