The Pakoka River in flood with sediment loading.
|Basin countries||New Zealand|
|Length||21 kilometres (13 mi)|
The most notable features of the Pakoka valley were formed by Upper Pliocene–Lower Pleistocene Okete Volcanics about 2 million years ago. These rocks form the top of the Wharauroa Plateau, where the Pakoka rises. They also flowed down from a vent about a kilometre northwest of Bridal Veil Falls to block the valley and form the falls.
From its source the river soon drops about 200 metres, cutting into Coleman Conglomerate a Puaroan (in the Tithonian epoch - about 150 million years ago) poorly sorted conglomerate of sandstone and siltstone, containing andesitic pebbles up to 5 cm diameter.
A rock arch and several notable bluffs are formed of late Whaingaroan Ahirau Sandstone formed about 28 million years ago. Although classified as sandstone, it looks more like limestone, with 40-60% calcium carbonate content and lapiez features in massive (lacking internal structures), blue-grey, calcareous, fine sandstone.
Apart from recent alluvial deposits, the other main rock in the valley is Hauturu Sandstone, which is mid to late Whaingaroan, about 30 million years old. It is commonly knobbly due to resistant bands and lenses of hard calcareous sandstone in soft friable quartzofeldspathic sand
A Regional Council study describes the vegetation around the estuary - "Te Heru Point and up towards Pakoka Landing, a forest of akeake, kanuka and kowhai lines the estuary arm. Spartina is present on the [right bank] upstream of Ohiawhakainga Creek. Patches of sea meadow are found at the mouth of the Motakotako Creek in front of the rushes. The saline influence on the vegetation finishes just upstream of the road bridge at Pakoka Landing. Moving downstream on the true-left bank are bands of saltmarsh ribbonwood with marsh clubrush and raupo wetland behind. Small patches of seagrass are found on the mud flats around the corner where the river widens out. The farmland is not fenced along the [left bank] and stock access is potentially a problem. A mature (~10 years?) flowering mangrove is upstream of Karetoto Island. A small patch of saltwater paspalum is found immediately opposite the island. A patch of seagrass lies behind the oyster bank at Mowhiti Point. The harbour edge is lined by a thin band of rush."
Mitigation funding from Te Uku Wind Farm and support from farmers and Regional Council have resulted in Whaingaroa Harbour Care putting up 15km of fencing to protect the river and its tributaries and planting 150,000 trees in the valley above Bridal Veil Falls. This has been followed by a possum and rat control project jointly with the Department of Conservation
Six sites were surveyed for the windfarm and given Stream Health Index scores between 60 and 170.5 (poor to excellent). Their 2006 survey identified these stream quality indicator species in the Pakoka,  - the higher the score, the more sensitive these macroinvertebrates are to pollution.
|9||caddisfly (Olinga feredayi)||rare|
|9||spiny-gilled mayfly (Coloburiscus humeralis)||occasional|
|7||dobsonfly (Archichauliodes diversus)||occasional|
|6||riffle beetle (Elmidae)||occasional|
|5||stony-cased caddisfly (Pycnocentrodes)||occasional|
|5||crustacea (Paratya curvirostris)||rare|
|4||mud snail (Potamopyrgus antipodarum)||abundant|
|3||sand fly (Austrosimulium)||occasional|
- "Place Name Detail: Pakoka River". New Zealand Geographic Placenames Database. Land Information New Zealand. Retrieved 2010-04-23.
- Geology of the Raglan-Kawhia Area: Institute of Geological & Nuclear Sciences (N.Z.), Barry Clayton Waterhouse, P. J. White 1994 ISBN 0-478-08837-X
- "A Cultural Health Index for Streams and Waterways | Ministry for the Environment". Mfe.govt.nz. 2013-01-10. Retrieved 2013-01-22.
- "Underwater Life - Macroinvertibrates". Waitakere.govt.nz. Retrieved 2012-12-26.
- "Riffle beetles". Landcare Research. 2012-09-25. Retrieved 2012-12-26.
- "Underwater Life - Macroinvertibrates". Waitakere.govt.nz. Retrieved 2013-01-22.
- Pakoka River 1:50,000 map at NZTopomaps