Хауракские равнины: География и история Новой Зеландии

Region of New Zealand

The Hauraki Plains are a geographical feature and non administrative area (though Hauraki Plains County Council existed from 1920 to 1989 and a statistical Area Unit remains) located in the northern North Island of New Zealand, at the lower (northern) end of the Thames Valley. They are located 75 kilometres south east of Auckland, at the foot of the Coromandel Peninsula and occupy the southern portion of a rift valley bounded on the north west by the Hunua Ranges, to the east by the Coromandel and Kaimai ranges and to the west by a series of undulating hills which separate the plains from the much larger plains of the Waikato River. Broadly, the northern and southern parts of the Hauraki Plains are administered by the Hauraki District and the Matamata Piako District respectively. The alluvial plains have been built up by sediment deposited by the Piako and Waihou rivers, which flow north to reach the sea at the Firth of Thames, and earlier by the ancestral Waikato River. The resulting land is flat, peat heavy, and partly swampy, which has been converted into excellent land for dairy farming. Economically, the dairy farming is the leading primary industry, supported by other grassland farming. More recently, tourism in the Hauraki Plains region has been growing and the Hauraki Rail Trail, part of the New Zealand Cycle Trail, has been constructed in the Hauraki Plains. The largest town fully within the Plains is Ngatea, with a smaller settlement of Turua. The larger town of Paeroa is located on the eastern edge of the Hauraki Plains. While there is no defined geographical southern boundary to the Hauraki Plains, this is generally taken as being a line between the towns of Te Aroha and Morrinsville, approximately following State Highway 26.

Around 2–3 million years ago, a large block of the crust slumped down 500–2000 metres, forming in due course the Hauraki 2 to 3 half grabens. The ancestral Waikato River often flowed through the resulting valley into the Hauraki Gulf, most recently through the Hinuera Valley some 20,000 years ago. Over time, the Hauraki Basin slowly filled up with pumice, mud and gravel.

After the last shift of the Waikato River back to the west coast, the Waihou and Piako rivers were formed. These two rivers carried silt out into the Firth of Thames or Tikapa. The plains were full of mangroves, raupo (Typha orientalis), harakeke (Phormium tenax) a dense forest of kahikatea. Most of the land was raw peat, varying in depth from a metre to more than twenty metres. It was a morass, the home of wild ducks and eels. Nevertheless, the rich flora and fauna of the plains amply provided the staples of the Māori people who lived in the region. Many areas on the banks of the Waihou River were settled by Hauraki Māori, such as Oruarangi pā and Paterangi pā near Matatoki, and the Te Raupa pā and Waiwhau pā near Paeroa.

Ships of all sizes plied the rivers of the Hauraki Plains, from tiny row boats to huge barques although, most of the boats were steamers and the engines were made at A & G Price in Thames. As industries progressed (like the mining in Waihi) bigger ships were required to carry the bigger loads. The majority of the boats were steamers, but some were paddle steamers. Larger passenger ships had luxurious lounges for men and women decorated with velvet upholstery and paintings on the walls. There were even brass bands on some boats and room for dancing on the decks. There was also room for horses and general cargo. Some cargo boats and punts were designed with drop sides to assist in loading and unloading on the river banks. This was especially useful when animals were being loaded. During the mining strike the hotels were closed by the government, but you could still drink on a moving boat. So people would get on the boats and take a trip for the day just to use the bar. In 1877, massive timber ships called barques travelled up to Bagnalls' mill in Turua to collect the kahikatea logs and transport them to Auckland and Australia. You can still see the remains of the wharf where the ships berthed. When the Bagnalls first arrived in Turua and wanted to go to church in Thames, they rowed to Kopu then walked the last 5 mile (8 km) to Thames. At Orchard (now called Ngatea), Pipiroa, Kopu and Paeroa there were punts (floating platforms) that carried people, horses and carts across the rivers for a small fee. At Te Aroha, there was a wire rope stretched across the river which originally had a Māori canoe tied to it on which people could pull themselves across and was later replaced by a punt with a crank and for two shillings people could crank themselves across.

Geologists have shown that a very long time ago, the Waikato river came through the Hinurea valley and filled the Hauraki Basin with pumice, mud, drift wood and gravel to a depth of over 1200 ft. You can still see evidence of sea beaches between Shelly Beach and Maukoro. Before the arrival of the European settlers, the Hauraki Plains was 400 km2 of peat and swamp land which acted as a big ponding area, through which ran two main rivers – the Waihou and Piako. Māori used the rivers for hundreds of years to get to the rich food resources in the swamp. When the Europeans came they also used the rivers for transport. Because the Hauraki Plains were swamp land and there were no roads the easiest way to transport people, supplies, food and produce was by boat. Gold brought many ships up the Waihou and Ohinimuri rivers with heavy machinery and miners aboard. There was even a special hard wharf built at Paeroa for fear of a conventional one collapsing while the machines were unloaded. Bagnells' mill at Turua was established to mill the tall kahikatea trees growing there. Huge barques (sailing ships) came up the river on flood tides to collect the wood, some of which would be taken to Australia and be made into butter boxes. After the scrub and kahikatea had been cleared farming was taken up and the farmers needed everything from food to animals and boats and the rivers carried it all in. In pioneer days the rivers were the lifelines of the Hauraki Plains, but as roads improved and bridges were built the need for river transport diminished. Today it has all died away except the ferry that goes up the Waihou to Paeroa from Auckland, and the metal barge that comes into Kopu to pick up a load.

In 1769 Captain James Cook travelled up the Waihou River to look at the "lofty trees which adorn its banks". He was the first European to travel up the river. The Waihou reminded him of the River Thames in London so he named it the River Thames. Although this name stuck for quite some time, now it is known as the Waihou. His discovery of the kahikatea tree later brought many ships to the area looking for masts and spars. In the 1900s the Waihou was navigable right up to Matamata, because development had not yet silted up the river. Travelling up stream you would pass Kopu on the left then Turua on the right, Matatoki, Puriri, Hikutaia, Paeroa and Te Aroha on the left and eventually Matamata on the right.

The Piako River is much smaller than the Waihou, but it was just as important in the development of the Hauraki Plains. Travelling up the Piako you would see Pipiroa, then Ngatea, both on the right, followed by Kerepehi, and the last town accessible by boat was Patetonga. Supplies were brought up the Piako by a small yacht and later by a launch. The boat was the main outlet to civilisation for the settlers who were mostly male bachelors and it was easier for them to eat stale bread brought up by the boat weekly than to make it themselves. It also brought mail and took cream back to Kopu which took four hours. The rivers were a major lifeline for the plains in the early days and they are still a part of everyday life, though not nearly as much as they used to be.

Dairy farming is the most important industry on the Hauraki Plains, providing the most income for the region. The sizes of dairy farms range from around 100 cows to over 500. 66% of the total land area of the plains is used in dairy farming. This equates to 779.34 km2 of land.

Although dairy farming is the main industry it is not the only farming industry. Sheep and dry stock farming are beginning to catch on with farmers. There is still the demand for wool and meat, which the Hauraki Plains region helps to provide. An ostrich farm has been developed near Turua which deals in tourism, meat sales and gifts.

There are primary schools in Ngatea, Kaihere, Pipiroa, Waitakaruru and Turua. Secondary education options include Hauraki Plains College in Ngatea, Paeroa College, and Thames High School.

At 9,238.44 hectares, the Kopuatai Peat Dome is New Zealand's largest unaltered restiad peat bog, and is also globally unique. The area is protected by the Wetland Management Reserve under the Conservation Act 1987 and is managed by the Department of Conservation. Fifty four species of birds have been recorded in the Kopuatai Peat Dome. Twenty seven are protected, 17 are unprotected and 10 are game birds. The endangered Australasian bittern (Botaurus poiciloptilus) is found in the wetland with other endangered birds such as the banded rail (Rallus philipensis assimillis), marsh crake (Porzana pusilla affinis) and the North Island fernbird (Bowdleria punctata vealeae).