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Annual report 2016-2017

flow past the weir (constructed in 2002). The remaining residual flow passes through an old (and mostly ineffective) fish pass on the true left bank of the weir. Much of the scheme is monitored and operated remotely by the Company. Through a computerised water level sensor system, Trustpower can monitor the residual flows in the Manganui River and Mangaotea Stream, water levels in the race and lake and how much rain is falling locally. This has allowed Trustpower to manage race flows to

Pukeiti Newsletter & Plant List February 2021

the country’s control of the pandemic holds. In many ways the fall of the Giant Rata at Pukeiti mirrored the year’s trauma. A crack appeared in its trunk. The crack grew daily and the mighty 1000 year old tree looked about to topple. If this happened, its hollow base, a destination for inquisitive children, could have imposed a real danger for anyone trapped inside. Over recent years other old ratas dotted throughout Pukeiti’s forest have fallen without notice and the decision was made

PCPOct2019 trackchange web

estuaries are well flushed, with little diversity in the way of intertidal and subtidal habitats. Sedimentation has a major influence on the region’s estuaries, the factors behind which include rain fall and modified land use. The large number of rivers and the erosion of Mount Taranaki generally bring a lot of sediment to the coast. However, the high energy coastline means this sediment supply does not settle long enough to greatly assist with the beach building process. Active

Interim Version of the Proposed Coastal Plan

of the coastline now comprised of cliffs. Erosion is greatest along the marine terraced coastline where the sedimentary rock is softer than the laharic material of the ring plain coast. There are a number of small estuaries at the mouths of Taranaki’s larger rivers. These estuaries are well flushed, with little diversity in the way of intertidal and subtidal habitats. Sedimentation has a major influence on the region’s estuaries, the factors behind which include rain fall and modified

Stratford water supplies monitoring 2018-2019

backwash is discharged via a large pond. The outlet from the pond is an inverted pipe located at the opposite end of the pond from the inlet. The discharge from the pond emerges from a pipe to fall over a small waterfall. At the base of the waterfall the discharged water runs down a natural cobbled channel beneath native riparian vegetation for approximately 10 metres before entering the Patea River, downstream of the intake weir. 1.2.2 Midhirst water supply The Midhirst community WTP