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The park covers 8,900 hectares (22,000 acres) in the headwaters of Te Awa Kairangi / Hutt River at the southern end of the Tararua Range. The Kaitohe weir is the largest of Wellington Water 's three water supply sources, [ 2 ] providing between 40 and 50% of the water supply for the Wellington urban area.
The Hutt River (Māori: Te Awa Kairangi, Te Wai o Orutu or Heretaunga; officially Te Awa Kairangi / Hutt River) flows through the southern North Island of New Zealand.It flows south-west from the southern Tararua Range for 56 kilometres (35 mi), forming a number of fertile floodplains, including Kaitoke, central Upper Hutt and Lower Hutt.
The Mawaihakona Stream (also known as Māwai Hākona Stream) is a small watercourse in Upper Hutt, in the North Island of New Zealand. The stream begins at a spring in Trentham Memorial Park and drains the western side of the Hutt Valley from Trentham to Heretaunga, flowing into the Hutt River north of the Silverstream bridge.
The Hutt Valley (or 'The Hutt') is the large area of fairly flat land in the Hutt River valley in the Wellington region of New Zealand. Like the river that flows through it, it takes its name from Sir William Hutt , a director of the New Zealand Company in early colonial New Zealand.
The conifer-broadleaf rainforest at the fork of Pakuratahi River and Te Awa Kairangi / Hutt River typifies the original vegetation of the area. There is centuries-old rātā, rimu, hinau and kamahi on the upper slopes, red beech on the lower slopes, and black beech on higher spurs and ridge tops with poorer soils. [3]
The Upper Hutt city centre lies approximately 26 km north-east of Wellington. [17] While the main areas of urban development lie along the Te Awa Kairangi / Hutt River valley floor, the city extends to the top of the Remutaka Pass to the north-east and into the Akatarawa Valley and rough hill-country of the Akatarawa ranges to the north and north-west, almost reaching the Kāpiti Coast close ...