HOME
*





Kakanui
The small town of Kakanui lies on the coast of Otago, in New Zealand, fourteen kilometres to the south of Oamaru. The Kakanui River and its estuary divide the township in two. The part of the settlement south of the river, also known as Kakanui South, formerly "Campbells Bay", was developed as a collection of Bach (New Zealand), cribs (holiday homes). A recent increase in the development of Subdivision (land), subdivisions has increased the density of dwellings within South Kakanui. The Kakanui River reaches the sea near the town, and the low range known as the Kakanui Mountains stretches inland from south of Oamaru towards the Maniototo. Kai Tahu used to temporarily occupy Kakanui as they travelled north and south, as evidenced by the midden on the north side of the estuary. The area around Kakanui has a reputation for its limestone formations, and produces many fossils. Quarrying formerly took place. The rich and fertile soil of the area around the river has physical propertie ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


All Day Bay
The small town of Kakanui lies on the coast of Otago, in New Zealand, fourteen kilometres to the south of Oamaru. The Kakanui River and its estuary divide the township in two. The part of the settlement south of the river, also known as Kakanui South, formerly "Campbells Bay", was developed as a collection of Bach (New Zealand), cribs (holiday homes). A recent increase in the development of Subdivision (land), subdivisions has increased the density of dwellings within South Kakanui. The Kakanui River reaches the sea near the town, and the low range known as the Kakanui Mountains stretches inland from south of Oamaru towards the Maniototo. Kai Tahu used to temporarily occupy Kakanui as they travelled north and south, as evidenced by the midden on the north side of the estuary. The area around Kakanui has a reputation for its limestone formations, and produces many fossils. Quarrying formerly took place. The rich and fertile soil of the area around the river has physical propertie ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Kakanui Mountains
The Kakanui Range is a range of high hills located inland from Oamaru in the South Island of New Zealand. The range forms a boundary between the valley of the Waitaki River to the north and the high plateau known as the Maniototo and the upper watershed of the Taieri River to the southwest. The highest point in the Kakanui Range is Mount Pisgah, at 1643 m (5394 ft). The Kakanui Range is crossed by road at Danseys Pass, which has a saddle at 935 m (3070 ft). The southwestern slopes of the Kakanui Range were a major goldfield during the Central Otago goldrush of the 1860s. Relics from this goldrush can be found at Kyeburn and Naseby. The Kakanuis continue as the Horse Range to the Pacific at Shag Point Shag Point / Matakaea is a headland and township in East Otago, New Zealand. It is located close to State Highway 1 nine kilometres to the northeast of Palmerston, at the southern end of a long open bay known as Katiki Beach. The point itsel .... Mo ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Oamaru
Oamaru (; mi, Te Oha-a-Maru) is the largest town in North Otago, in the South Island of New Zealand, it is the main town in the Waitaki District. It is south of Timaru and north of Dunedin on the Pacific coast; State Highway 1 and the railway Main South Line connect it to both cities. With a population of , Oamaru is the 28th largest urban area in New Zealand, and the third largest in Otago behind Dunedin and Queenstown. The town is the seat of Waitaki District, which includes the surrounding towns of Kurow, Weston, Palmerston, and Hampden. which combined have a total population of 23,200. Friendly Bay is a popular recreational area located at the edge of Oamaru Harbour, south to Oamaru's main centre. Just to the north of Oamaru is the substantial Alliance Abattoir at Pukeuri, at a major junction with State Highway 83, the main route into the Waitaki Valley. This provides a road link to Kurow, Omarama, Otematata and via the Lindis Pass to Queenstown and Wanaka. Oamaru serv ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Kakanui River
The Kakanui River is a river of North Otago, New Zealand, bridged by Highway 1 at Maheno and flowing into the Pacific Ocean at Kakanui. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Otago Rivers of New Zealand {{Otago-river-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Waitaki District
Waitaki District is a territorial authority district that is located in the Canterbury and Otago regions of the South Island of New Zealand. It straddles the traditional border between the two regions, the Waitaki River, and its seat is Oamaru. History Waitaki District is made up of the former Waitaki County, Waihemo County and Oamaru Borough, which were amalgamated in 1989. It is governed by the Waitaki District Council. Name During the colonial period, the area was also known as ''Molesworth''. However, the Maori name ''Waitaki'' eventually prevailed. Geography It has a land area of , of which or 59.02% is in the Canterbury Region and or 40.98% in the Otago Region. It is the only district in the South Island that lies in two regions.Siobhan Downes"Why Waitaki wants its name on the tourism map" stuff.co.nz, 19 May 2021. A major reason for this split was the governance of the Waitaki River which forms a political boundary between Canterbury and Otago. With major hydro sch ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Maheno, New Zealand
Maheno is a small North Otago township south of Oamaru in New Zealand. The area has 75 residents. A number of the town's streets are named after places in Tyne and Wear, England, such as Whickham, Felling, Heworth and Jarrow. One of two New Zealand's hospital ships in World War I, the SS ''Maheno'', was named after this town. Demographics Maheno is described as a rural settlement by Statistics New Zealand, and covers . It is part of a larger statistical area also called Maheno. Maheno settlement had a population of 126 at the 2018 New Zealand census, an increase of 18 people (16.7%) since the 2013 census, and a decrease of 18 people (−12.5%) since the 2006 census. There were 54 households. There were 66 males and 60 females, giving a sex ratio of 1.1 males per female. The median age was 54.7 years (compared with 37.4 years nationally), with 12 people (9.5%) aged under 15 years, 21 (16.7%) aged 15 to 29, 63 (50.0%) aged 30 to 64, and 30 (23.8%) aged 65 or older. Ethniciti ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Maniototo
The Maniototo Plain, usually simply known as The Maniototo, is an elevated inland region in Otago, New Zealand. The region roughly surrounds the upper reaches of the Taieri River and the Manuherikia River. It is bounded by the Kakanui Range to the north and the Rock and Pillar Range to the southeast. It has a harsh, dry climate, ranging from over 30 °C in mid-summer to -15 °C in mid-winter. The region is sparsely populated, with the largest centres being Ranfurly, New Zealand, Ranfurly, Naseby, New Zealand, Naseby, Wedderburn and Oturehua. Part of the Canterbury-Otago tussock grasslands the land surrounding the plain is hilly, with many outcrops of rock which also break up the plain in places. During the 1860s the region was one of the sites of the Central Otago goldrush, and relics from that era can still be seen around the towns of Kyeburn, Naseby, New Zealand, Naseby, and Saint Bathans, New Zealand, St. Bathans. Sheep farming is the major source of income. The a ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Dunedin (ship)
The ''Dunedin'' (1876–90) was the first ship to successfully transport a full cargo of refrigerated meat from New Zealand to England. In this capacity, it provided the impetus to develop the capacity of New Zealand as a major provider of agricultural exports, notwithstanding its remoteness from most markets. ''Dunedin'' disappeared at sea in 1890, and neither the ship nor her crew has ever been seen or heard from since. Ship origins Robert Duncan and Co built the 1,320-ton, ''Dunedin'' at Port Glasgow in Scotland in 1874 for the Albion Line (later the Shaw, Savill & Albion Line). Her ship number was 67085, and she cost £23,750 pound sterling, . She was one of six ''Auckland'' class emigrant vessels, each designed to carry 400 passengers. In 1881, still painted in her original colours of a black hull with a gold band and pink boot topping as shown, she was refitted by William Soltau Davidson with a Bell Coleman refrigeration machine, with which she took the first load of fro ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Main South Line
The Main South Line, sometimes referred to as part of the South Island Main Trunk Railway, is a railway line that runs north and south from Lyttelton in New Zealand through Christchurch and along the east coast of the South Island to Invercargill via Dunedin. It is one of the most important railway lines in New Zealand and was one of the first to be built, with construction commencing in the 1860s. At Christchurch, it connects with the Main North Line to Picton, the other part of the South Island Main Trunk. Construction Construction of the Main South Line falls into two main sections: from Christchurch through southern Canterbury to Otago's major city of Dunedin; and linking the southern centres of Dunedin and Invercargill, improving communication in southern Otago and large parts of Southland. Construction of the first section of the line began in 1865 and the whole line was completed on 22 January 1879. Christchurch-Dunedin section The Canterbury provincial government ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Potato
The potato is a starchy food, a tuber of the plant ''Solanum tuberosum'' and is a root vegetable native to the Americas. The plant is a perennial in the nightshade family Solanaceae. Wild potato species can be found from the southern United States to southern Chile. The potato was originally believed to have been domesticated by Native Americans independently in multiple locations,University of Wisconsin-Madison, ''Finding rewrites the evolutionary history of the origin of potatoes'' (2005/ref> but later genetic studies traced a single origin, in the area of present-day southern Peru and extreme northwestern Bolivia. Potatoes were domesticated there approximately 7,000–10,000 years ago, from a species in the ''Solanum brevicaule'' complex. Lay summary: In the Andes region of South America, where the species is indigenous, some close relatives of the potato are cultivated. Potatoes were introduced to Europe from the Americas by the Spanish in the second half of the 16 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Chinese New Zealander
Chinese New Zealanders ( mi, Tāngata Hainamana o Aotearoa; ) or Sino-New Zealanders are New Zealanders of Chinese ancestry. The largest subset of Asian New Zealanders, many of the Chinese immigrants came from Mainland China, Hong Kong, Taiwan, or other countries that have large populations of Chinese diaspora. Today's Chinese New Zealand group is composed of diasporic communities from Indonesia, Malaysia, Cambodia, Vietnam and Singapore. As of 2018, Chinese New Zealanders account for 4.9% of the population of New Zealand, and are the largest Asian ethnic group in New Zealand, accounting for 36.3% of Asian New Zealanders. In the 1860s goldrush immigrants from Guangdong arrived. Due to this historical influx, there is still a distinct Chinese community in Dunedin, whose mayor Peter Chin is of Chinese descent. However, most Chinese New Zealanders live in the North Island, and are of more recent migrant heritage. Chinese people historically faced severe discrimination in New Zealan ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]