Te Tai Rāwhiti
|Region of New Zealand|
|Territorial authority||Gisborne District Council|
|• Mayor||Meng Foon|
|• Deputy Mayor||Rehette Stoltz|
|• Territorial||8,355 km2 (3,226 sq mi)|
|Population (June 2013 estimate)|
|• Density||5.6/km2 (14/sq mi)|
The Gisborne District or Gisborne Region (Māori: Te Tai Rāwhiti) is an area of northeastern New Zealand governed by the Gisborne District Council. It is named after its largest settlement, the city of Gisborne.
It is also known as the East Coast region, although it is often divided into the East Coast proper, also known as East Cape, north of the city, and Poverty Bay, the area including and surrounding the city. The region is also sometimes referred to as the East Cape, although that also refers specifically to the promontory at the northeastern extremity. More recently, it has been called Eastland, although that can also include Opotiki in the eastern Bay of Plenty to the northwest, and Wairoa to the south.
Its Māori name, Te Tai Rāwhiti, means the Coast of the Sunrise, reflecting the fact that it is the first part of the New Zealand mainland to see the sun rise.
The district is located in the northeastern corner of the North Island. It ranges from the Wharerata Hills in the south, which divide it from the Wairoa district in the Hawke's Bay region, to Lottin Point in the north. The western boundary runs along the Raukumara Range, which separates it from the Opotiki district. In the southwest, its boundary runs along the western edge of Te Urewera National Park.
It is sparsely inhabited and isolated, with small settlements mainly clinging to small bays along the eastern shore including Tokomaru Bay and Tolaga Bay. Its population is 46,700 (June 2013 estimate). Three-quarters of the population – 34,800 (June 2013 estimate) – lives in the city of Gisborne. No other settlement has a population of over 1000. The largest other settlements are the towns of Tolaga Bay and Ruatoria, each with populations of over 800 in 2001.
Inland, the land is rough, predominantly forested, hill country. A spine of rough ridges dominates the centre of the region, culminating in the impressive bulk of the 1752 metre Mount Hikurangi in Waiapu Valley in the region's northeast. This mountain is the fifth highest mountain in the North Island, and the highest that is not a volcano. Regarded as sacred by the Māori, there is some justification to the claims that this is the first mountain to see the sun in summer.
The region's population has higher than the national average proportion of Māori - over 50% in some areas - and still maintains strong ties to both Māori tradition and the iwi and marae structure. The predominant iwi are Ngāti Porou, Rongowhakaata, Ngai Tamanuhiri, Te Aitanga a Mahaki.
Gisborne District Council is a unitary territorial authority, which means that it performs the functions of a regional council as well as those of a territorial authority (a district or city). It includes a mayor, 14 elected councillors, an appointed chief executive officer, 4 department managers and approximately 250 staff. Its headquarters are in the city of Gisborne. The area it governs is constituted as both the Gisborne District and the Gisborne Region.
Gisborne District Council was created as part of a major nationwide reform of local government in 1989. It replaced the councils of Gisborne City, Cook County, Waiapu County and Waikohu County, East Cape United Council, East Cape Catchment Board and Regional Water Board, East Coast Pest Destruction Board, two harbour boards, and several noxious plants authorities and recreation reserve boards. It was the only unitary authority in New Zealand until three others were created in 1992.
The sub-national GDP of the Gisborne region was estimated at US$1.031 billion in 2003, 1% of New Zealand's national GDP.
The region is sheltered by high country to the west and has a dry, sunny climate. It has a yearly average of 2,200 sunshine hours. The annual rainfall varies from about 1000mm near the coast to over 2500mm in higher inland country.
|Climate data for Gisborne|
|Average high °C (°F)||24.9
|Average low °C (°F)||13.6
|Precipitation mm (inches)||54
|Source: NIWA Climate Data|
At 8.55pm (NZDT) on 20 December 2007, the Gisborne region was hit by an earthquake of Richter magnitude 6.8, centred in the Hikurangi Trench, 50 km southeast of Gisborne at a depth of 40 km. Mercalli intensities of 7-8 were experienced, with three buildings substantially collapsed in the CBD and others experiencing some structural damage. One death was reported (a heart attack of an elderly woman, sustained during the quake) plus minor injuries.
- 2006 Tonga earthquake
- List of marae in the Gisborne District
- List of schools in the Gisborne District
- "Subnational Population Estimates: At 30 June 2013 (provisional)". Statistics New Zealand. 22 October 2013. Retrieved 4 November 2013. Also "Infoshare; Group: Population Estimates - DPE; Table: Estimated Resident Population for Urban Areas, at 30 June (1996+) (Annual-Jun)". Statistics New Zealand. 19 November 2013. Retrieved 28 November 2013.
- "The Local Government (Gisborne Region) Reorganisation Order 1989". New Zealand Gazette. 9 June 1989. pp. 2328 ff. Retrieved 5 June 2014.
- Soutar, Monty (13 July 2012). "East Coast region – Overview". Te Ara – the Encyclopedia of New Zealand. Retrieved 31 May 2014.
- Cowan, James (1926). The Maoris in the Great War. pp. 179–80. Retrieved 7 June 2014.
- "Regional Gross Domestic Product". Statistics New Zealand. 2007. Retrieved 18 February 2010.
- "Climate Data". NIWA. Retrieved 25 February 2009.
- GeoNet – New Zealand Earthquake Report - Dec 20 2007 at 8:55 pm (NZDT)
- Binning, Elizabeth (21 December 2007). "Quake damage extensive as massive clean-up begins". The New Zealand Herald. NZPA. Retrieved 1 October 2011.
|Wikivoyage has a travel guide for East Coast (New Zealand).|
|Wikimedia Commons has media related to Gisborne Region.|