Hamilton, New Zealand
Hamilton, also known colloquially as The Tron, is an inland city in the North Island of New Zealand. Located on the banks of the Waikato River, it is the seat and most populous city of the Waikato region. With a territorial population of, it is the country's fourth most-populous city. Encompassing a land area of about, Hamilton is part of the wider Hamilton Urban Area. In 2020, Hamilton was awarded the title of most beautiful large city in New Zealand. Hamilton is now considered the fastest growing city in the country.
The area now covered by the city began as the site of several Māori villages, including Kirikiriroa, from which the city takes its Māori name. By the time English settlers arrived, most of these villages, which sat beside the Waikato River, were abandoned as a result of the Invasion of Waikato and land confiscation by the Crown.
The settlers developed the city as an agricultural service centre, but it now has a diverse economy. Hamilton Gardens is the region's most popular tourist attraction. Education and research and development play an important part in Hamilton's economy, as the city is home to approximately 40,000 tertiary students and 1,000 PhD-qualified scientists.
Etymology
The settlement was named by Colonel William Moule after Captain John Fane Charles Hamilton, the commander of HMS Esk, who was killed in the battle of Gate Pā, Tauranga.History
Pre-European settlement
The area now covered by the city was originally the site of several Māori villages, including Te Parapara, Pukete, Miropiko and Kirikiriroa, from which the city takes its Māori name. Local Māori were the target of raids by Ngāpuhi during the Musket Wars, and several pā sites from this period can still be found beside the Waikato River. In December 2011 several rua or food storage pits were found near the Waikato River bank, close to the Waikato museum.In 1822, Kirikiriroa Pa was briefly abandoned to escape the Musket Wars. However, by the 1830s Ngāti Wairere's principal pa was Kirikiriroa, where the missionaries, who arrived at that time, estimated 200 people lived permanently. A chapel and house were built at Kirikiriroa for visiting clergy, presumably after Benjamin Ashwell established his mission near Taupiri.
Between 1845 and 1855, crops such as wheat, fruit and potatoes were exported to Auckland, with up to 50 canoes serving Kirikiriroa. Imports included blankets, clothing, axes, sugar, rum, and tobacco. Millstones were acquired and a water wheel constructed, though possibly the flour mill wasn't completed. However, one article said Kirikiriroa flour was well known.
Magistrate Gorst, estimated that Kirikiriroa had a population of about 78 before the Invasion of Waikato via the Waikato Wars of 1863–64. The government estimated the Waikato area had a Māori population of 3,400 at the same time. After the war in the Waikato, large areas of land, including the area of the present city of Hamilton were confiscated by the Crown under the New Zealand Settlements Act 1863. Over the next year, most of these villages were abandoned as a result of the land confiscation, also known as Raupatu.
Pākehā settlement
After the Invasion of the Waikato and confiscation of the invaded land, militia-settlers were recruited in Melbourne and Sydney. On 10 August 1864 the government advertised for tenders to build 10 huts and a hospital at Kirikiriroa. Hamilton was settled by the 4th Waikato Regiment Militia, led by Captain William Steele. The 1st Regiment was at Tauranga, the 2nd at Pirongia, the 3rd at Cambridge and the 4th at Kirikiriroa. The first military settlers arrived on the Rangiriri on 24 August 1864. Members of Ngāti Wairere assembled on the banks of the river as the Rangiriri arrived and threw peaches at her. One of the passengers, Teresa Vowless, passed her baby to another passenger and leapt overboard in order to be the first settler ashore.Many of the soldier/settlers who intended to farm after the 1863 war, walked off their land in 1868 due to its poor quality. Much of the land was swampy or under water. In 1868 Hamilton's population, which was about 1,000 in 1864, dropped to 300 as farmers left. On 22 December 1875 the first brickworks opened in Hamilton.
19th century development
The road from Auckland reached Hamilton in 1867 and the railway in December 1877. That same month, the towns of Hamilton West and Hamilton East merged under a single borough council. The first traffic bridge between Hamilton West and Hamilton East, known as the Union Bridge, opened in 1879. It was replaced by the Victoria Bridge in 1910.The first railway bridge, the Claudelands Bridge, was opened in 1884. It was converted to a road traffic bridge in 1965. Hamilton reached 1,000 people in 1900, and the town of Frankton merged with the Hamilton Borough in 1917. Between 1912 and 1936, Hamilton expanded with new land in Claudelands, Maeroa, and Richmond – modern day Waikato Hospital and northern Melville. Hamilton was proclaimed a city in 1945.
In the latter 19th century, the areas of Te Rapa and Pukete were important sites for the kauri gum trade of the late 19th/early 20th centuries, being some of the southern-most locations where gum could be found.
Beale Cottage is an 1872 listed building in Hamilton East.
Contemporary history
From 1985 MV Waipa Delta provided excursions along the river through the town centre. In 2009 Waipa Delta was moved to provide trips on Waitematā Harbour in Auckland, but replaced by a smaller boat. That too ceased operation and the pontoon at Parana Park was removed in 2013. The Delta moved to Taupō in 2012. The former Golden Bay vessel, Cynthia Dew, ran 4 days a week on the river from 2012, but was in liquidation in December 2022.File:HoodStHamilton.jpg|thumb|right|Hood Street in Hamilton Central, with two heritage buildings: [|former Bank of New Zealand] and the former Post Office
As of 2016, the city continues to grow rapidly. Development is focused on the northern end of the city although in 2012 the council made a decision to balance the city's growth by approving an urban development to the south. Traffic congestion is increasing due to population growth, though the council has undertaken many road development projects to try to keep up with the rapid growth. The Hamilton City Council is building a 2/4-lane arterial road, Wairere Drive, through the northern and eastern suburbs to form a 25 km suburban ring road with State Highway 1, which is due for completion in early 2015, while the New Zealand Transport Agency plans to complete the Hamilton section of the Waikato Expressway by 2019, easing congestion taking State Highway 1 out of the city and bypassing it to the east.
The rapid growth of Hamilton has brought with it the side effects of urban sprawl especially to the north east of the city in the Rototuna area. Further development is planned in the Rototuna and Peacocke suburbs. There has been significant development of lifestyle blocks adjacent to the Hamilton Urban Area, in particular Tamahere, and Matangi.
Geography
Hamilton's geography is largely the result of successive volcanic ash falls, plus debris, which swept down the Waikato River in at least two massive floods, created by ash blocking the outlet of Lake Taupō. In its present form the landscape originated around 20,000 years ago, after the Oruanui eruption of the Taupō Volcano. The dates given for the eruption vary. A 2007 study said it was between 22.5 and 14 kya. Another in 2004 put it 26.5 kya. After the eruption Lake Taupō rose to about above the present lake. Around 20 kya. the ash dam eroded and the lake rapidly fell some, creating massive floods. The ash they carried formed the main Hinuera Surface into an alluvial fan of volcanic ash, which extends north of Hamilton and drops about from Karapiro. The Waikato changed its course from flowing into the sea at Thames at about that time, possibly just because sediment built up. The peat lakes and bogs also formed about that time; carbon dating gives maximum ages of 22.5 to 17 kya. Due to an ice age, vegetation was slow to restabilise the ash, so dunes formed up to above the local Hinuera surface. The current Waikato valley had cut into the debris by about 12 kya. and was further modified by the 181 CE Hatepe eruption, when again Lake Taupō level fell, generating a flood, equivalent to 5 years' normal flow in just a few weeks. About 800 years ago, aggradation began raising the river bed by about.With the exceptions of the many low hills such as those around the University of Waikato, Hamilton Lake, Beerescourt, Sylvester Road, Pukete, and to the west of the city, and an extensive network of gullies, the terrain of the city is relatively flat. In some areas such as Te Rapa, one old path of an ancient river can be traced. The relatively soft and unconsolidated soil material is still being actively eroded by rain and runoff.
In its natural state, Hamilton and environs was very swampy in winter with 30 small lakes connected to surrounding peatlands. Hamilton was surrounded by 7 large peat bogs such as Komakorau to the North and Rukuhia and Moanatuatua to the South, as well as many smaller ones all of which have now been drained with only small remnants remaining. The total area of peat bog was about 655 km2. Early photos of Hamilton East show carts buried up to their axles in thick mud. Up until the 1880s it was possible to row and drag a dinghy from the city to many outlying farms to the North East. This swampy, damp environment was at the time thought to be an ideal breeding ground for the TB bacillus, which was a major health hazard in the pioneering days. The first Hamilton hospital was constructed on a hill to avoid this problem. One of the reasons why population growth was so slow in Hamilton until the 1920s was the great difficulty in bridging the many arms of the deep swampy gullies that cross the city. Hamilton has 6 major dendritic gully complexes with the 15 km long, 12 branch, Kirikiriroa system being in the north of the city and the southern Mystery creek-Kaipaki gully complex being the largest. Others are Mangakotukutuku, Mangaonua and Waitawhiriwhiri.
In the 1930s, Garden Place Hill, one of the many small hills sometimes referred to as the Hamilton Hills, was removed by unemployed workers working with picks and shovels and model T Ford trucks. The Western remains of the hill are retained by a large concrete wall. The original hill ran from the present Wintec site eastwards to the old post office. The earth was taken 4 km north to partly fill the Maeroa gully adjacent to the Central Baptist Church on Ulster Street, the main road heading north.
Lake Rotoroa began forming about 20,000 years ago. Originally it was part of an ancient river system that was cut off by deposition material and became two small lakes divided by a narrow peninsula. With higher rainfall and drainage from the extensive peat land to the west, the water level rose so the narrow peninsula was drowned so forming one larger lake. To the north the lake is 8 m deep and in the southern end 6 m deep. The old dividing peninsula, the start of which is still visible above water on the eastern side, is only 2 m below the surface. Lake Rotoroa offers a diverse range of recreational activities, including walking trails, picnic areas, and water sports, making it a popular destination for both locals and tourists. The well-maintained paths around the lake are ideal for jogging, walking, and cycling. These trails offer stunning views of the lake and surrounding landscapes, providing a tranquil setting for exercise enthusiasts and nature lovers alike.