Cromwell, New Zealand

Cromwell
Town
Cromwell
Coordinates: 45°02′S 169°12′E / 45.04°S 169.20°E / -45.04; 169.20
Country New Zealand
Region Otago Region
Territorial authority Central Otago District Council
Population (June 2016)[1]
  Total 4,670
Time zone NZST (UTC+12)
  Summer (DST) NZDT (UTC+13)
Postcode(s) 9310
Aerial view of Cromwell from the south

Cromwell is a town in Central Otago in the Otago region of New Zealand.

It is situated between State Highway 6 (linking to Wanaka, 50 km north, and Queenstown, 60 km west) and State Highway 8 leading to the Lindis Pass, 75 km northeast, and Alexandra, 33 km south. The road to Alexandra winds through the Cromwell Gorge. A point near Cromwell lies 119 kilometres from the sea, the farthest from the sea anywhere in New Zealand.[2] A prominent feature surrounding much of the town is the man-made Lake Dunstan. Cromwell also has the newly constructed Highlands Motorsport Park. Nearby settlements are at Bannockburn, Lowburn, Tarras, and Ripponvale.

Cromwell is also the home of the Cromwell Chafer Beetle (Prodontria lewisi).

The 45th parallel south runs just North of the township.

History

Cromwell was originally known as "The Junction", being at the confluence of the Clutha and Kawarau Rivers. In 1862, gold was discovered below the Junction by two miners, Hartley and Reilly. Once the word of a gold strike was out, there was an influx of several thousand miners to the area.

As gold ran out, Cromwell became the service centre for an extensive farming and stone fruit growing area. It has a strategic location between the Lindis and the Haast passes, and acts as a hub between the towns of Wanaka, Queenstown and Alexandra. The former is commemorated with the giant sculpture of stone fruit which stands outside the northern end of the town.

Cromwell lay at the confluence of the Clutha River and Kawarau River, which was noted for the difference between the colours of the waters of the two rivers and also for the historic bridge at the convergence of the two. Since the construction of the Clyde Dam and the filling of Lake Dunstan in the early 1990s the river confluence was drowned, as was the old town centre.

The decision to build Clyde Dam and use Cromwell as the accommodation base brought many changes to the town. Approximately one-third of the town was rebuilt on higher ground. The changes included the doubling of the residential area, relocation of the old town centre (now called "Old Cromwell Town"), upgrading of services, and the provision of modern educational and sports facilities, and a new bridge. The relocated town centre, or "The Mall," now houses the main retail, service and civic buildings in Cromwell. Several of the old buildings of the town which escaped the flooding have been retained as a historic precinct close to the shore of the Kawarau.

The town was named after Oliver Cromwell and, as well as "The Junction", the town was previously known as "The Point" and "Kawarau".

Cromwell is nicknamed the "Fruit Bowl of the South".

Education

Cromwell has five pre-school facilities, two primary schools and a co- educational secondary school. An Otago Polytechnic campus specialises in horticulture, catering and tourism. Its crop centre provides advisory services to horticulturalists on commercially viable new crops.

Climate

Cromwell receives around 400 mm of rain a year due to its inland location. Although it is widely believed to have a continental climate, the town officially has an oceanic climate (Cfb) with rainfall just enough to escape the semi-arid climate classification.

Climate data for Cromwell
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) 24.4
(75.9)
24.2
(75.6)
21.3
(70.3)
17.3
(63.1)
12.7
(54.9)
8.7
(47.7)
8.0
(46.4)
11.4
(52.5)
15
(59)
17.6
(63.7)
20.3
(68.5)
22.5
(72.5)
17.0
(62.6)
Daily mean °C (°F) 17.7
(63.9)
17.3
(63.1)
14.6
(58.3)
10.8
(51.4)
7.2
(45)
4.1
(39.4)
3.2
(37.8)
5.6
(42.1)
8.9
(48)
11.3
(52.3)
13.7
(56.7)
16.1
(61)
10.9
(51.6)
Average low °C (°F) 11
(52)
10.4
(50.7)
7.9
(46.2)
4.2
(39.6)
1.7
(35.1)
−0.6
(30.9)
−1.5
(29.3)
−0.2
(31.6)
2.8
(37)
5.0
(41)
7.1
(44.8)
9.7
(49.5)
4.8
(40.6)
Average precipitation mm (inches) 48
(1.9)
41
(1.6)
38
(1.5)
38
(1.5)
28
(1.1)
30
(1)
23
(0.9)
20
(0.8)
28
(1.1)
36
(1.4)
30
(1.2)
36
(1.4)
391
(15.4)
Source: NIWA [3]
The town of Cromwell and Lake Dunstan

Cromwell Mayors

Former mayors of the Borough of Cromwell were as follows

  • WJ Barry 1866-1868
  • W Whetter 1868-1869
  • GW Goodger 1869-1870
  • W Smitham 1870-1871
  • JD Taylor 1871-1872
  • M Fraer 1872-1873
  • J Dawkins 1873-1874
  • DA Jolly 1874-1877
  • SN Brown 1877-1878
  • C Colclough 1878-1881
  • M Behrens 1881-1883
  • J Marsh 1883-1885
  • SH Turton 1885-1889
  • T McCracken 1889-1891
  • DA Jolly 1891-1892
  • JL Scott 1892-1895
  • T Rooney 1895-1897
  • K Pretsch 1897-1899
  • E Murrell 1899-1905
  • J Little 1905-1909
  • E Murrell 1905-1913
  • E Jolly 1913-1915
  • AM Brodrick 1915-1921
  • DC Jolly 1921-1927
  • CC Sanders 1927-1929
  • CWJ Roberts 1929-1937
  • JC Parcell 1937-1943
  • RE Austin 1943-1944
  • W Partridge 1944-1950
  • JR Munro 1950-1951
  • FG Dunn 1951-1956
  • LR Skinner 1956-1958
  • LA Jelley 1958-1960
  • IG Anderson 1960-1980
  • PJ Mead 1980-1986
  • DA Butcher 1986-1989

Historic places

Bannockburn Bridge

The sign on the south side was reconstructed from the original suspension bridge's pillars.

Bannockburn

An historic town which was once the centre of a thriving and successful gold mining industry. Remnants include the hotel, Post Office, Stewart's store, and many old dwellings. Now a restful area centred on viticulture and agriculture.

The Bannockburn Sluicings

Walk through an incredible landscape changed by hand in the pursuit of gold. The round trip is full of history and interest.

Bendigo Goldfields

Bendigo was a successful quartz mining area for over half a century. From the site of the old Bendigo township at the top of the Bendigo Loop Road a steep, narrow vehicle track winds up into the hills to Logantown and even further up to Welshtown, where some of the most striking remains of old stone cottages can be found.

Carrick Goldfields

The ruins of Carricktown are 4 km up a 4WD track from the old mining area of Quartzville (near the end of Quartzville Road), and the Young Australian 6m overshot water-wheel can be found a further 3 km on. The track continues up to Duffer's Saddle. Return down Nevis Road to Bannockburn.

Cromwell Gorge

Hartley and Reilly first discovered gold at the beginning of this rugged and spectacular gorge.

Old Cromwell Town

Old Cromwell Town's historic street (Melmore Terrace), 2014

The construction of the Clyde Dam created Lake Dunstan, which consumed part of the old Cromwell town. The deep river gorge, famed for its picturesque beauty, lined with orchards and vineyards, and especially the meeting point of two distinct rivers, was reformed with an artificially constructed shoreline. Though the original orchards were lost, Cromwell's climate has allowed it to maintain its reputation for wine and fruit production.

References

Notes
  1. "Subnational Population Estimates: At 30 June 2016 (provisional)". Statistics New Zealand. 21 October 2016. Retrieved 21 October 2016. For urban areas, "Subnational population estimates (UA, AU), by age and sex, at 30 June 1996, 2001, 2006-16 (2017 boundary)". Statistics New Zealand. 21 October 2016. Retrieved 21 October 2016.
  2. Cook, Marjorie (11 February 2009). "Revealed: New Zealand's furthest inland point". Otago Daily times.
  3. . NIWA. 2014 http://cliflo.niwa.co.nz/. Missing or empty |title= (help) Retrieved on 22 March 2015.
Sources
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Coordinates: 45°02′S 169°12′E / 45.04°S 169.20°E / -45.04; 169.20

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