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McKinnon Pass

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46-516: Omanui / McKinnon Pass (previously spelt Mackinnon Pass ) is an alpine pass between Mount Hart and Mount Balloon in Fiordland , New Zealand. The pass is at an elevation of 1,154 metres (3,786 ft) and is located 19 kilometres (12 mi) southwest of Milford Sound / Piopiotahi . The pass is the highest point of the famous Milford Track connecting Lake Te Anau and the Clinton River valley with

92-490: A month slashing a track through the forest and eventually made their way across the pass to reach the existing track to Sutherland Falls . The McKinnon Memorial, a large cairn , is located at the pass commemorating the traverse of the route by McKinnon. The pass was known for a number of years as Mackinnon Pass although it later was agreed that the correct spelling was McKinnon. The name was officially changed in July 2022, correcting

138-663: A population of 111 at the 2018 New Zealand census , a decrease of 12 people (−9.8%) since the 2013 census , and a decrease of 33 people (−22.9%) since the 2006 census . There were 3 households, comprising 54 males and 60 females, giving a sex ratio of 0.9 males per female. The median age was 28.2 years (compared with 37.4 years nationally), with 3 people (2.7%) aged under 15 years, 69 (62.2%) aged 15 to 29, 39 (35.1%) aged 30 to 64, and 3 (2.7%) aged 65 or older. Ethnicities were 73.0% European/ Pākehā , 8.1% Māori , 24.3% Asian , and 2.7% other ethnicities. People may identify with more than one ethnicity. The percentage of people born overseas

184-613: A small island at the head of Doubtful Sound / Patea . Except for electricity generation (at the Manapouri Power Station and a smaller hydroelectric power station at Lake Monowai) and some agriculture, tourism is the only other major economic factor in the region. Visitor spending was NZ$ 92 million in 2003, and 1,017 people were employed full-time in the tourism industry, with an additional 1,900 people considered to be employed in tourism industry support services. Most tourists visit Milford Sound / Piopiotahi , though walking in

230-463: A surface area of 25 square miles (65 km ). The lake surface is about 155 metres (509 ft) above sea level. One of the country's southernmost lakes, it is only 13 km from the southern coast of the South Island . It sits between the similarly-sized lakes Monowai and Poteriteri . According to the 1925 New Zealand Official Yearbook, it drains about 1,800 cu ft (51 m )/sec via

276-586: A very wet climate with annual average of 200 rainy days and annual rainfall varying from 1,200 millimetres (47 in) in Te Anau to 8,000 millimetres (310 in) in Milford Sound. The prevailing westerly winds blow moist air from the Tasman Sea onto the mountains, resulting in high amounts of precipitation as the air rises and cools down. Fiordland has never had any significant permanent population. Māori knew

322-464: Is Invercargill , about 80 kilometres (50 mi) east of the southern end of Fiordland. The only major road in Fiordland is State Highway 94 , also referred to as Milford Road, connecting Te Anau with Milford Sound. Blanket Bay Hotel, not an actual hotel , may be the westernmost inhabited locality of New Zealand. The fishermen's refuelling and supply depot with a small jetty and helipad is located on

368-494: Is 462 metres deep, is located in a mountain valley in Fiordland National Park . "Hauroko" translates from te reo Māori as " soughing of the wind" or "sounding wind". Prior to 1930, the lake was also called "Lake Hauroto". Lake Hauroko is 462 metres (1,516 ft) deep; sources range from calling it the 16th deepest lake in the world to the 23rd deepest. The S-shaped lake is 20 miles (32 km) long and has

414-421: Is also a tourist destination, but is less accessible as it requires both a boat trip over Lake Manapouri and bus transfer over Wilmot Pass . Also situated within Fiordland are Browne Falls and Sutherland Falls , which rank among the tallest waterfalls in the world, and New Zealand's three deepest lakes, Lake Hauroko , Lake Manapouri, and Lake Te Anau . Several other large lakes lie nearby, and Fiordland and

460-412: Is from introduced species , especially red deer , but these are now being hunted out of the area, and furthermore, the park includes a number of small offshore islands which are free from introduced species and are designated Specially Protected Areas. Ten marine reserves have been established in Fiordland to protect a wide variety of species and habitats. The original two reserves were established at

506-404: Is one of the few not yet colonised by invasive water weeds, except the bulbous rush, Juncus bulbosus , so it retains plants such as Nitella stuartii algae, Callitriche petriei water-starwort, Isoetes kirkii quillwort, Pilularia novaezelandiae pillwort fern , Trithuria inconspicua waterlilies and Charales fibrosa . Pests include stoats and possums , which arrived in

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552-802: Is situated on Caroline Peak, which only reaches 1,704 metres (5,591 ft), and in the southwest of Fiordland the altitude for permanent snowfields lowers to under 1,500 metres (4,900 ft). The past glaciation's deep carving out of the landscape has also resulted in fiord-like arms in Lake Manapouri and Lake Te Anau, and on the coast managed to cause several large chunks of the mainland becoming cut off. The largest of these uninhabited offshore islands are Resolution Island and Secretary Island , and are important conservation sites, particularly as sanctuaries for endangered native birds. Twelve fiords, some stretching up to 40 kilometres (25 mi) inland, and two inlets leading to three more fiords, extend along

598-610: The Arthur River valley and Milford Sound / Piopiotahi. The pass was known to local Māori as Omanui meaning "the great running" or "the great escape". Europeans did not discover the pass until October 1888 when Quintin McKinnon and Ernest Mitchell made their way over the pass from the Clinton Valley. McKinnon had been commissioned by the chief surveyor of Otago to find a route from Te Anau to Milford Sound. McKinnon and Mitchell spent

644-495: The 20 km (12 mi)-long Wairaurāhiri River into Foveaux Strait 10 kilometres to the west of Te Waewae Bay . The largest island in Lake Hauroko is Mary Island, named in 1883 after the wife of the government surveyor John Hay. A smaller island is adjacent to Teal Bay at the southern end of the lake. There are also a few other smaller islets and rocks in the lake. Traditionally, Ngā Puna Wai Karikari o Rakaihautu say

690-678: The Department of Conservation, trapping stoats and controlling deer, helping takahē numbers in the area to increase to over 200 and remain at that level. There are also a high number of insects and one indigenous reptile, the Fiordland skink (Oligosoma acrinasum) . There are around 300 insect species endemic to the Fiordland region, many of them sizeable, such as weta, large caddis, and giant weevils, and some of them unusual, such as egg-laying worms, alpine cicadas, and brightly coloured alpine moths. There are six species of native sandflies (blackfly, Simuliidae) with one endemic to Fiordland. Most of

736-656: The Fiordland National Park for all but the northernmost end. This area contains all the fiords as well as the Hollyford Valley and also includes the area around Big Bay , which lies to the north outside of the Fiordland National Park, but still belongs to the Southland Region. Tourism organisations and the Department of Conservation use this definition of the Fiordland region. New Zealanders generally regard

782-457: The Fiordland National Park, and is marked by U-shaped valleys and fiords along the coast and steep mountains with foundations of hard rocks like gneiss , schist , granite and diorite , with the softer rock having been carved out by multiple glaciations. Fiordland contains New Zealand's oldest known plutonic (igneous) rocks and is dominated by the southernmost extent of the Southern Alps, as

828-586: The South Fiord of Lake Te Anau, before veering northwest and ending with the southern side of Te Houhou / George Sound . By that definition, the Fiordland region is almost entirely within the Fiordland National Park, except for small pockets near the two southernmost lakes, but the area does not include the three northernmost fiords (Milford Sound / Piopiotahi, Te Hāpua / Sutherland Sound , and Hāwea / Bligh Sound ). The much more widespread definition of "Fiordland" has an eastern boundary that roughly follows that of

874-595: The ancestral bones possessed. This led to the belief that this woman was of high-ranking status, and it was later discovered through an archaeological investigation that she was a chieftain of the Ngāti Moimoi tribe. The burial remains on the island today, with a grille made of steel and wire mesh ensuring that people can still view the burial, but the woman will remain untouched. Trees are mainly matai , totara , rimu , tawhai pango , tawhai , Pseudopanax linearis and rautawhiri ( Pittosporum Colensoi ). The lake

920-443: The area attracted whalers and seal hunters, but only in the mid-19th century did surveyors and prospectors begin exploring Fiordland's interior. Between 1897 and 1908, two attempts at establishing a mining operation in the remote area of Rakituma / Preservation Inlet failed, and by 1914 the isolated small settlement of Cromartie (or Cromarty) there had been abandoned. The area was administered as Fiord County from 1876 until it

966-603: The area falls under the protection of the Fiordland National Park , part of the Te Wahipounamu World Heritage Site . Fiordland National Park has an area of 12,600 square kilometres, making it the largest national park in New Zealand and one of the larger parks in the world, containing many tourist attractions, such as Milford Sound, Doubtful Sound and the Milford Track . The main threat to natural habitats

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1012-402: The area well but only visited seasonally, for hunting, fishing and to collect the precious stone pounamu (New Zealand jade) from Anita Bay at the mouth of Milford Sound / Piopiotahi . In Māori mythology , Fiordland is described as being created by the demigod Tū-te-raki-whānoa, who carved the fiords from rock using his adze . As he moved northwards, he perfected his techniques, and considered

1058-458: The coast from Piopiotahi in the north to Rakituma / Preservation Inlet in the south. In general, the fiords become wider from north to south as the height of the mountains decreases. The outlets of the southernmost fiords have a character more akin to inlets, with only the inner arms such as Long Sound resembling fiords. A further sound, Kaikiekie / Bradshaw Sound , is basically an extension of Thompson and Doubtful Sounds after their junction at

1104-455: The east and the 1,769-metre-high (5,804 ft) Mount Hart to the west. Fiordland Fiordland ( Māori : Te Rua-o-te- Moko , "The Pit of Tattooing", and also translated as "the Shadowlands"), is a non-administrative geographical region of New Zealand in the south-western corner of the South Island , comprising the western third of Southland . Most of Fiordland is dominated by

1150-468: The eastern end of Secretary Island . The area has been categorised as the Fiordland temperate forests ecoregion , having a variety of habitats and, due to its isolation, a high number of endemic plants. Much of Fiordland is heavily forested, except for locations where surface rock exposures are extensive. The natural habitats are almost completely unspoilt. Nothofagus beech trees are dominant in many locations, silver beech ( Nothofagus menziesii ) in

1196-450: The fiords and red beech ( Nothofagus fusca ) in the inland valleys. In the understory there are a wide variety of shrubs and ferns , including crown fern ( Blechnum discolor ), areas of scrubby herbs above the treeline, patches of bog next to mountain streams and finally an area of rimu ( Dacrydium cupressinum ) -dominated dunes in the Waitutu area on the south coast. Despite a latitude in

1242-415: The island is subject to a Māori curse. Such stories are dismissed by local Māori. The island is famous for the discovery of a burial site of a Māori woman in 1967, who is known as "the lady of the lake" by Southland locals. The burial site is in a cave on the eastern side of the island. Believed to have been placed on the burial site sometime between the late 16th century and 17th century, possibly around 1660,

1288-637: The lake was dug by rangatira Rākaihautū on his journey south with his ko . The lake is a Statutory Acknowledgement site under the Ngāi Tahu Claims Settlement Act 1998 . Geologists say it's a glacial lake , formed near the Hauroko Fault (it and other faults in the area have slipped several kilometres) in early carboniferous granites and metamorphic rocks, on the higher ground, with much more recent Hauroko Formation Eocene - Oligocene sediments such as calcareous sandstone , on

1334-560: The last fiord, Milford Sound / Piopiotahi , his greatest achievement. The name Te Rua-o-te- Moko ("The Pit of Tattooing") is a reference to the visit of the Tākitimu migratory waka to the area. Traditional histories recall the captain of the waka, Tamatea, lost his tattooing ink in Taiari / Chalky Inlet . After the Tākitimu was wrecked at Te Waewae Bay , the crew decided to walk overland to

1380-403: The lower ground, towards the southeast. Hauroko granite is about 358 million years old, medium grained, white, granodiorite and granite , with red-brown biotite . It has intruded dikes , plugs and xenoliths into metasediment . Albert Edward Granite is coarser, with pink K-feldspar megacrysts and green-brown biotite. There are also small amounts of carboniferous diorite . Towards

1426-558: The mid-40s, the treeline is generally below 1,000 metres (3,300 ft) because of the cool summers and the influence of the Southern Ocean on the climate. The area is home to threatened native bird species, such as the flightless takahē and kiwi , blue duck (whio), and yellowhead (mōhua). The takahē was presumed to have been extinct for 50 years before a small remaining population was discovered in Fiordland's Murchison Mountains in 1948. Since then, that area has been managed by

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1472-494: The more accessible eastern parts of the alps is a popular activity. Nonetheless, the remoteness of the region limits even tourism , and after short visits to the major sites, most tourists return to other areas, such as Queenstown or Invercargill. 45°24′S 167°12′E  /  45.4°S 167.2°E  / -45.4; 167.2 Lake Hauroko Lake Hauroko is the deepest lake in New Zealand . The lake, which

1518-585: The north of the South Island. While stopping at Te Anau , Tamatea decided to dig a pit where wood could be burnt to create soot for tattoo ink. Over time, the name grew to refer to the wider Fiordland area. In 1770, Captain James Cook and his crew became the first Europeans to sight Fiordland . Cook returned and anchored in Tamatea / Dusky Sound for five weeks in 1773. The expeditions' maps and descriptions of

1564-569: The northwest of the lake, the area between the Hauroko Burn and the Hay River has dioritic, felsic dykes. A 30 km (19 mi) road from Clifden to the lake was built in about 1909 and improved in the 1960s. A water taxi runs to the Dusky Track , which starts at the north end of the lake and leads to Lake Manapouri . Mary Island is the subject of several local myths, including one that

1610-538: The often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of unmodified vegetation in New Zealand and significant populations of endemic plants and threatened animals, in some cases

1656-402: The only remaining wild populations. Fiordland features a number of fiords , which in this area are typically named sounds , reflecting the fact that sometimes fiords are considered to be a type of narrow sound. Of the twelve major fiords on Fiordland's west coast, Milford Sound / Piopiotahi is the most famous and the only one accessible by road. Doubtful Sound / Patea , which is much larger,

1702-541: The peaks reduce in height from north to south. The tallest mountain in the Fiordland region is Mount Tūtoko at 2,723 metres (8,934 ft), one of several peaks over 2,000 metres in the Darran Mountains . Southeast of this area, there are only a handful of peaks reaching 2,000 metres, however due to the rainy weather with cold winters and lack of hot summer temperatures, even these mountains contain glaciers and peaks with permanent snow cover. The southernmost glacier

1748-525: The request of the New Zealand Federation of Commercial Fishermen in 1993: An additional eight reserves were established on the recommendation of Fiordland Marine Guardians in 2005: The Fiordland statistical area covers 12,064.68 km (4,658.20 sq mi) and had an estimated population of 90 as of June 2024, with a population density of 0.007 people per km . Almost the entire population lives at Milford Sound (village) . Fiordland had

1794-489: The spelling and adding the Māori name to form the dual name Omanui / McKinnon Pass. Today, the pass is crossed by thousands of hikers every year on the Milford Track . There is a day shelter at the top of the pass for hikers to use as a rest point and for use in emergencies. Although often clouded in, the pass offers spectacular 360-degree views. The pass is on the ridge between the 1,857-metre-high (6,093 ft) Mount Balloon to

1840-464: The steep sides of the snow-capped Southern Alps , deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" derives from an alternate spelling of the Scandinavian word for steep glacial valleys, " fjord ". The geographic area of Fiordland is dominated by, and roughly coterminous with, Fiordland National Park , New Zealand's largest national park . Due to

1886-465: The surrounding parts of Southland and Otago Regions are often referred to as the Southern Lakes . Only a handful of Fiordland's lakes are accessible by road - Lake Poteriteri is the largest lake in New Zealand with no road access. Many of the region's lakes are not even accessible via tramping tracks. This part of New Zealand, especially to the west of the mountain divide of the Southern Alps, has

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1932-470: The towns of Te Anau and Manapouri as part of the Fiordland region, even though they lie outside of the boundary of the national park. In geographical terms, the Fiordland region contains the huge mountainous regions west of the line from Te Waewae Bay to Monowai to Te Anau, and includes the valleys of the Eglinton River and Hollyford River / Whakatipu Kā Tuka . The area is almost identical to that of

1978-477: The woman was laid to rest wearing a flax cloak and a dog skin collar with weka feather edging around her neck, and was seated upright on a bier made of sticks and leaves. The reasons for the burial in this manner are uncertain, although it has been suggested that these burials were to either make sure the remains were protected from desecration by enemies, or to protect living descendants from a dangerous " tapu " (sacred, forbidden or taboo ) that Māori may have believed

2024-542: Was 62.2, compared with 27.1% nationally. Although some people chose not to answer the census's question about religious affiliation, 67.6% had no religion, 21.6% were Christian , 2.7% were Muslim and 5.4% had other religions. Of those at least 15 years old, 27 (25.0%) people had a bachelor's or higher degree, and 9 (8.3%) people had no formal qualifications. The median income was $ 34,000, compared with $ 31,800 nationally. 3 people (2.8%) earned over $ 70,000 compared to 17.2% nationally. The employment status of those at least 15

2070-460: Was absorbed into neighbouring Wallace County in 1981. Since 1989, it has formed part of Southland District and of the wider Southland Region . There are currently varying definitions for the boundary of the Fiordland region. The eastern boundary of Fiordland according to Statistics New Zealand stretches from Sand Hill Point on the western end of Te Waewae Bay more or less straight north, cutting through Lakes Hauroko, Monowai , Manapouri, and

2116-438: Was that 102 (94.4%) people were employed full-time, and 3 (2.8%) were part-time. Apart from the areas around the townships of Te Anau and Manapouri , which are not included in the Fiordland statistical area, the Fiordland region has never had more than a few human inhabitants and is the least-populated area of the South Island, with no villages or towns, and many areas almost inaccessible except by boat or air. The nearest city

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