Kā Tiritiri O Te Moana
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Kā Tiritiri O Te Moana
The Southern Alps (; officially Southern Alps / Kā Tiritiri o te Moana) are a mountain range extending along much of the length of New Zealand's South Island, reaching its greatest elevations near the range's western side. The name "Southern Alps" generally refers to the entire range, although separate names are given to many of the smaller ranges that form part of it. The range includes the South Island's Main Divide, which separates the water catchments of the more heavily populated eastern side of the island from those on the west coast. Politically, the Main Divide forms the boundary between the Marlborough, Canterbury and Otago regions to the southeast and the Tasman and West Coast regions to the northwest. Names The Māori name of the range is , meaning "the Mirage of the Ocean". The English explorer James Cook bestowed the name ''Southern Alps'' on 23 March 1770, admiring their "prodigious height". p. 384. They had previously been noted by Abel Tasman in 1642, w ...
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South Island, New Zealand
The South Island ( , 'the waters of Pounamu, Greenstone') is the largest of the three major islands of New Zealand by surface area, the others being the smaller but more populous North Island and Stewart Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, to the south by the Foveaux Strait and Southern Ocean, and to the east by the Pacific Ocean. The South Island covers , making it the List of islands by area, world's 12th-largest island, constituting 56% of New Zealand's land area. At low altitudes, it has an oceanic climate. The most populous cities are Christchurch, Dunedin, Nelson, New Zealand, Nelson and Invercargill. Prior to European settlement, Te Waipounamu was sparsely populated by three major iwi – Kāi Tahu, Kāti Māmoe, and the historical Waitaha (South Island iwi), Waitaha – with major settlements including in Kaiapoi Pā near modern-day Christchurch. During the Musket Wars expanding iwi colonised Te Tau Ihu Māori, Te Tau Ihu, ...
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James Cook
Captain (Royal Navy), Captain James Cook (7 November 1728 – 14 February 1779) was a British Royal Navy officer, explorer, and cartographer famous for his three voyages of exploration to the Pacific and Southern Oceans, conducted between 1768 and 1779. He completed the first recorded circumnavigation of the main islands of New Zealand and was the first known European to visit the eastern coastline of Australia and the Hawaiian Islands. Cook joined the British merchant navy as a teenager before enlisting in the Royal Navy in 1755. He served during the Seven Years' War, and subsequently surveyed and mapped much of the entrance to the St. Lawrence River during the Battle of the Plains of Abraham, siege of Quebec. In the 1760s, he mapped the coastline of Newfoundland (island), Newfoundland and made important astronomical observations which brought him to the attention of the Admiralty (United Kingdom), Admiralty and the Royal Society. This acclaim came at a crucial moment in Brit ...
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Mount Cook Village
Mount Cook Village, officially Aoraki / Mount Cook, is located within New Zealand's Aoraki / Mount Cook National Park at the end of , only south of the summit of the country's highest mountain, also called Aoraki / Mount Cook, in the Southern Alps. Because it is situated inside a national park, it is not possible to own property in Mount Cook Village; however, because of the year-round operation of the hotel and motels, the village has a small permanent population of around 250. All buildings and facilities operate on concessions and leases from the government. The village has no grocery stores apart from a small in-hotel convenience store. The nearest supermarket is away in Twizel, the closest town. There is a self-service petrol pump behind the hotel complex; however, the fuel price reflects the remote location. Mount Cook Village operates a small school with a roll as low as a dozen children, the only school in New Zealand inside a national park. History The first bu ...
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Arthur's Pass
Arthur's Pass, previously called Camping Flat then Bealey Flats, and for some time officially Arthurs Pass, is a township in the Southern Alps of the South Island of New Zealand, located in the Selwyn district. It is a popular base for exploring Arthur's Pass National Park. Arthur's Pass township is about south of the mountain pass with the same name. At an elevation of above sea level, the settlement is surrounded by beech forest. The Bealey River runs through the township. The town is located from Christchurch, a two-hour drive on State Highway 73. Naming and history The township and the pass take their names after Arthur Dudley Dobson (1841–1934, Sir Arthur from 1931). The Chief Surveyor of Canterbury Province, Thomas Cass, had tasked Arthur Dobson to find out if there was an available pass out of the Waimakariri watershed into valleys running to the West Coast. In 1864, Arthur's brother Edward Henry Dobson joined him and accompanied him over the watershed into ...
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Lewis Pass
Lewis Pass is the northernmost of the three main mountain passes through the Southern Alps in the South Island of New Zealand. With an elevation of 907 metres, it is slightly lower than Arthur's Pass and higher than Haast Pass. The pass is the saddle between the valleys of the Maruia River to the northwest in the West Coast Region and the Lewis River to the southeast in north Canterbury. The small spa of Maruia Springs is close to the saddle, on the West Coast side. Lewis Pass is named after Henry Lewis who, together with Christopher Maling, was the first European to discover the pass, in April 1860 while working as a surveyor of the Nelson Provincial Survey Department. Before this time the pass was used by the Ngāi Tahu Māori of Canterbury to transport pounamu (greenstone) from the west coast. State Highway 7 traverses the pass. The road officially opened on Saturday 30 October 1937. It had a regular bus route over it until Intercity's service was replaced by a ...
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Stuff (website)
Stuff is a New Zealand news media website owned by newspaper conglomerate Stuff Ltd (formerly called Fairfax). As of early 2024, it is the most popular news website in New Zealand, with a monthly unique audience of more than 2 million. Stuff was founded in 2000, and publishes breaking news, weather, sport, politics, video, entertainment, business and life and style content from Stuff Ltd's newspapers, which include New Zealand's second- and third-highest circulation daily newspapers, ''The Post'' and '' The Press'', and the highest circulation weekly, '' Sunday Star-Times'', as well as international news wire services. Stuff has won numerous awards at the Newspaper Publishers' Association awards including 'Best News Website or App' in 2014 and 2019, and 'Website of the Year' in 2013 and 2018, 'Best News Website in 2019', and 'Digital News Provider of the Year' in 2024 and 2025. History Independent Newspapers Ltd, 2000–2003 The former New Zealand media company Independ ...
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Tasman Glacier
Tasman Glacier (officially Haupapa / Tasman Glacier) is the largest glacier in New Zealand, and one of several large glaciers which flow south and east towards the Mackenzie Basin from the Southern Alps in New Zealand's South Island. Geography At in length, Tasman Glacier is still New Zealand's longest glacier, despite shrinking considerably from the 1990s onwards. It is as much as wide and thick, and lies entirely within the borders of Aoraki / Mount Cook National Park. The glacier covers an area of and starts at a height of above sea level. Snowfall during the winter and spring seasons may accumulate up to . After the summer melt, may remain in the high altitude glacier head. The Tasman flows south west from Hochstetter Dome and Mount Elie De Beaumont alongside the southern slopes of The Minarets and south along the eastern flank of New Zealand's two highest mountains, Mount Tasman and its higher southern neighbour Aoraki / Mount Cook. Although its upper reaches ...
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Glacier
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on ever ...
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Lake Wakatipu
Lake Wakatipu () is an inland lake (finger lake) in the South Island of New Zealand. It is in the southwest corner of the Otago region, near its boundary with Southland, New Zealand, Southland. ''Lake Wakatipu'' comes from the original Māori language, Māori name . With a length of , it is New Zealand's longest lake, and, at , its List of lakes in New Zealand#Largest lakes, third largest. The lake is also very deep, its floor being below sea level (−110 metres), with a maximum depth of . It is at an altitude of , towards the southern end of the Southern Alps / Kā Tiritiri o te Moana. The general topography is a reversed "N" shape or "dog leg". The Dart River / Te Awa Whakatipu flows into the northern end, the lake then runs south for 30 kilometres before turning abruptly to the east. further along, it turns sharply to the south, reaching its southern end further south, near Kingston, New Zealand, Kingston. At the north end of the lake is the settlement of Glenorchy, New Ze ...
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Lake Coleridge
Lake Coleridge () is in inland Canterbury, New Zealand's South Island. It is located northwest of Methven and has a surface area of . The lake is situated in an over-deepened valley formed by a glacier over 20,000 years ago in the Pleistocene era. It currently has no natural outflows. There is a small settlement at the lake. Ecology Early colonial explorers found the shores of the lake covered in mānuka (or kānuka), kōwhai, cabbage trees, flax and general swamp plants. The lake was also surrounded by southern rātā trees and native beech trees. The lake itself was fairly lacking in aquatic plants because of a lack of nutrients. It was known for a population of large eels. Human activity has significantly changed the ecology. Colonial settlers introduced game fish, including rainbow trout, brown trout, Atlantic salmon and Chinook salmon. Changing water levels caused by the operation of the Coleridge Power Station killed most of the kānuka in 1914 and rata in 1923. In ...
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List Of Mountains Of New Zealand By Height
The following are lists of mountains in New Zealand ordered by height. Names, heights, topographic prominence and isolation, and coordinates were extracted from the official Land Information New Zealand (LINZ) Topo50 topographic maps at thinteractive topographic map of New Zealandsite. Mountains are referred to as ''maunga'' in the Māori language. Named summits over 2,900 m All summits over are within the Southern Alps, a chain that forms the backbone of the South Island, and all but one ( Mount Aspiring / Tititea) are within a radius of Aoraki / Mount Cook. Some of these summits are mere shoulders on the ridges of Aoraki and Mount Tasman. Gordon Hasell was the first person who, by 1960, had climbed all New Zealand's peaks above . The achievement mentions 27 peaks and it thus counts individual peaks that may make up one mountain, e.g. Mount Haast (Westland District), Mount Haast has three individual peaks that are all above that height. The 100 highest mountains Thes ...
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Mountains In New Zealand
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
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