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The natural environment

Harbour ecologyOhiwamontage
Geology and soils
Landscape

Harbour ecology

The 'wet' part of the Harbour is rich in shellfish and fish and has significant beds of seagrass, a critical habitat for many marine animals. As much of the Harbour bed is exposed at low tide, a rich diversity of wading birds, some migratory and some resident, make their homes here. The lower reaches of the Harbour contain extensive beds of mussels, cockles and pipi. The saltmarshes on the margins of the Harbour are dominated by sea rush and oioi, providing habitat for such birds as fernbird, bittern and banded rail. The muddy upper reaches of the Harbour, home to titiko (mudsnails) and mudcrabs, are being increasingly colonised by mangroves, which are also habitat for banded rail.

Read about the State of the Ohiwa Harbour and Catchment (3.65MB, PDF).

Kiwi population on the riseOhiwakiwi
A kiwi population is gradually increasing in the Whakatane and Ohope reserves at the western end of the Ohiwa Harbour, thanks to the Whakatane Kiwi Project. Since 1999, when four breeding pairs were found by the Department of Conservation in the Ohope reserves, 173 North Island brown kiwi chicks were raised or released back into the Ohope and Whakatane reserves, and the adjacent Ngati Awa Farm. It is the only place in the country where kiwi live in such numbers so close to an urban area. Many of the birds are now migrating south-east from Whakatane and Ohope as far as Stanley Road and sometimes beyond. The Whakatane Kiwi Project is working closely with several landowners, foresters and residents in these areas, so that kiwi are afforded greater protection in their travels. Long-term, the Project hopes to bring more landowners on board and extend predator control activities to their land, so that kiwi have safe havens all around Ohiwa.

Whakatanekiwi

Read more about kiwi management around Ohiwa Harbour in the case study - Kiwi management around Ohiwa Harbour.



Streams and reserves
The streams feeding the Harbour are home to significant numbers of native freshwater fish such as inanga (adult whitebait). While most of the flat and rolling land in the catchment is cleared for farming, there are many important remnants of coastal forest, dominated by pohutukawa and puriri. Many of these special places are set aside as reserves and managed by either the Department of Conservation or District Councils. Community groups help to look after some of these reserves.

Pests
OhiwaStoatThere are the usual threats to native birds (some quite rare) such as rats and stoats. Various invasive weeds, too many to list, compete with native vegetation from the edge of the mudflats to the hills. Some of these pests are controlled by landowners in terms of their obligations under the Regional Pest Management Plan. The Ohiwa Strategy partners are working towards better protection of all the ecological values of the Harbour and better coordination of pest control work.

 

Several aspects of the Harbour ecology are monitored by the Regional Council; you can find out more about this research here.

Geology and soilsOhiwaMap

The Harbour itself is unusual in that it has a spit on either side of the entrance. These spits are subject to regular changes according to currents and tides. The Harbour was once fed by a much larger river; it is slowly filling with sediment and will one day become dry land. This is a natural process which is accelerated by human activities which result in increased sediment entering the Harbour.

Effects of natural disasters
Evolution of the Ohiwa Harbour, in response to earthquakes and tsunami, is explained in this Waikato University podcast at 23:59. 

The spits at the mouth of the Harbour are constantly changing and in the 1970s a number of houses on the Ohiwa spit were lost to the encroaching sea, which has since retreated and left a wide band of sand dunes. The site where the hotel and wharf once stood is now in the middle of the Harbour entrance.

Volcanic history
Geologically, the area is predominantly greywacke of Late Jurassic to Late Cretaceous age, draped by loess (wind-blown silt) during the Pleistocene Ice Ages and more recently covered in volcanic ash and pumice from the Rotorua and Taupo volcanic centres.

It is from this air-fall rhyolitic volcanic ash that most of the soils of the Ohiwa Harbour catchment are derived. However, there are also other parent materials and processes that have formed soils in different parts of the catchment. Soils on the floodplains and lower flats are formed from a mixture of colluvium and alluvial rhyolitic ash and greywacke. Soils in the dunes are formed from air-fall tephra on windblown sand. The soil in the hills and steep headwater areas are Whakatane Hill soils and associated steep land soils, formed from Tarawera ash, Kaharoa ash on Taupo pumice, and Whakatane ash over sandstone or greywacke.

Landscape

The Ohiwa Harbour is a visually spectacular landscape covering approximately 26 square kilometres. The tidal waters, estuaries, mudflats and islands contrast with the surrounding predominantly rural landscape. There are great views of the Harbour and further afield from Tauwhare Pa and Onekawa Te Mawhai.

OhiwaaerialislandsThere are two main islands in the Harbour; Uretara and Ohakana Islands, plus the four smaller islands of Whangakopikopiko, Te Motuotu, Hokianga and Pataua Islands.