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Mount Belle
Mount Belle is a mountain in Fiordland, New Zealand. Description Mount Belle is part of the Wick Mountains and is situated above the east portal of Homer Tunnel in the Southland Region of the South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu United Nations Educational, Scientific and Cultural Organization, UNESCO World Heritage Site. Precipitation runoff from the mountain's north slope drains into the headwaters of the Hollyford River, whereas the south slope drains into Neale Burn which is a tributary of the Clinton River (New Zealand), Clinton River. Topographic relief is significant as the summit rises over above State Highway 94 (New Zealand), State Highway 94 in one kilometre, and the south face rises in one-half kilometre. The nearest higher neighbour is Mount Talbot (New Zealand), Mount Talbot, 2.8 kilometres to the north. History The first ascent of the summit was made in 1931 by Scott Gilkison and Norman Davis.
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Wick Mountains
The Wick Mountains are a range within New Zealand's Fiordland National Park, the country's biggest national park. Their highest peak is Mount Elliot , and this can be seen in fine weather from the Milford Track, a popular tourist walking track. Geography The range is bounded by the Arthur River (New Zealand), Arthur River to the west, Milford Sound (Piopiotahi) and the valley of the Cleddau River to the west, the Homer Saddle, which separates them from the Darren Mountains to the north west and the valleys of the Neil Burn and Clinton River (New Zealand), Clinton River to the south. The Homer Tunnel lies under the north eastern extreme of the range.Dowling, P. (ed.) (2004). ’’Reed New Zealand atlas’’. Auckland: Reed Publishing. Map 89. Sheerdown Peak in the range is at the southern end of Milford Sound rising above the airport flat. The mountains were named by Donald Sutherland (explorer), Donald Sutherland after his birthplace in Caithness, Scotland. Geology The Wi ...
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Clinton River (New Zealand)
The Clinton River is a river in the Southland Region of the South Island of New Zealand. There is also a Clinton River in Canterbury, which is a tributary of the Puhi Puhi River. The river lies completely within the Fiordland National Park and feeds into Lake Te Anau Lake Te Anau () is in the southwestern corner of the South Island of New Zealand. The lake covers an area of , making it the second-largest lake by surface area in New Zealand (after Lake Taupō) and the largest in the South Island. It is the .... The Milford Track follows the river from Lake Te Anau and then up the west branch of the river. Lake Mintaro is a small lake on the west branch of the river. Gallery Charles Howorth - Clinton Canyon - Sarjeant Gallery.jpg, Charles Howorth - Clinton Canyon - showing the Clinton River. Clinton canyon from mckinnon's pass.jpg, Clinton Canyon Milford Track Clinton River 1.jpg, The Clinton River seen from the Milford Track Clinton River Dore Pass.jpg, Dore Pass Cr ...
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Mount Christina
Mount Christina is a mountain in Fiordland, New Zealand. Description Mount Christina is the southernmost peak of the Darran Mountains and is situated in the Southland Region of South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. Precipitation runoff from the mountain drains into tributaries of the Hollyford River. Topographic relief is significant as the summit rises nearly above the Hollyford Valley in two kilometres. The mountain was named in 1870 by James McKerrow for Christina McKerchar (1838–1928), who later became the wife of George Gillow.''Mount Christina''
New Zealand Gazetteer, Retrieved 19 December 2024.
Christina was believed to be a friend of McKerrow's wife, Martha. McKerrow had first seen the mountain from
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Mount Crosscut
Mount Crosscut is a mountain in Fiordland, New Zealand. Description Mount Crosscut is part of the Darran Mountains and is situated in the Southland Region of South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. Precipitation runoff from the mountain drains into tributaries of the Hollyford River. Topographic relief is significant as the summit rises above Lake Marian in 2.5 kilometres and above Cirque Creek in one kilometre. The nearest higher peak is Mount Christina, three kilometres to the south-southeast. The mountain was named in 1924 by Dr. D. Jennings on account that the jagged peaks resemble the teeth of the crosscut saw that his party of students was using for clearing tracks.''Mount Crosscut''
New Zealand Gazetteer, Retrieved 20 December 2024.
The



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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Glacieret
A glacieret is a very small glacier, with a surface area less than . The term is sometimes incorrectly used to refer to a large, persistent snow patch of firn or névé. Characteristics Sometimes hardly larger than snowfields and perennial firn patches, glacierets tend to have little ice movement, with accumulation and ablation zones difficult to detect. During the last ice age, glacierets were an intermediate stage between firn patches and fully fledged glaciers, but in the present day, glacierets are usually remnants of larger glaciers that existed. Due to their small size, they are at a higher risk of melting due to climate change than larger glaciers. Examples * Snezhnika in the Pirin range of Bulgaria was the southernmost glacial mass in Europe before the discovery of glaciers on Mount Bazardüzü. * The Banski Suhodol Glacieret, also in the Pirin, is the only other surviving glacial mass in Bulgaria. * There are some glacierets in the range of the Pyrenees. * The Red ...
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Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California. * The western slope of the Wasatch Range in Utah. Specifically the Little and Big Cottonwood Canyons. * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which rece ...
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Marine West Coast
An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 40 and 60 degrees latitude, with subpolar versions extending to 70 degrees latitude in some coastal areas. Other varieties of climates usually classified together with these include subtropical highland climates, represented as ''Cwb'' or ''Cfb'', and subpolar oceanic or cold subtropical highland climates, represented as ''Cfc'' or ''Cwc''. Subtropical highland climates occur in some mountainous parts of the subtropics or tropics, some of which have monsoon influence, while their cold variants and subpolar oceanic climates occu ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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First Ascent
In mountaineering and climbing, a first ascent (abbreviated to FA in climbing guidebook, guide books), is the first successful documented climb to the top of a mountain or the top of a particular climbing route. Early 20th-century mountaineers and climbers focused on reaching the tops of iconic mountains (e.g. the eight-thousanders) and climbing routes (e.g. the great north faces of the Alps) by whatever means possible, often using considerable amounts of aid climbing, and/or with large expedition style support teams that laid "siege" to the climb. As all the key tops were summited, the manner in which each top was reached became important, particularly the ability to complete the ascent without artificial aid, which is called free climbing. In free climbing, the term first free ascent (abbreviated FFA) is used where a mountain or climbing route is ascended without any artificial aid (devices for climbing protection, protection in the event of a fall could be used as long as the ...
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Mount Talbot (New Zealand)
Mount Talbot is a mountain in Fiordland, New Zealand. Description Mount Talbot is part of the Darran Mountains and is situated above the Homer Tunnel in the Southland Region of South Island. It is set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. Precipitation runoff from the mountain drains north into the headwaters of the Gulliver River and south into the headwaters of the Hollyford River. Topographic relief is significant as the summit rises above the Gulliver River in two kilometres and above Gertrude Valley in one kilometre. The nearest higher peak is Mount Crosscut, 3.8 kilometres to the east-southeast. History The mountain was named to honour Arthur Ernest Talbot (1876–1917), a New Zealand mountaineer and alpine explorer who was well known for explorations in northern Fiordland, particularly in 1910 discovering a route to Milford near this mountain.
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State Highway 94 (New Zealand)
State Highway 94 is a New Zealand state highway network, New Zealand state highway connecting the large Southland, New Zealand, Southland town of Gore, New Zealand, Gore with one of New Zealand's most popular destinations, Milford Sound. It also passes the significant townships of Lumsden, New Zealand, Lumsden and Te Anau as well going through the Homer Tunnel (in this area it is also called the 'Milford Road', with the section from Te Anau up to the Sound being ). The road also goes through Fiordland and crosses the Main Divide of the Southern Alps (New Zealand), Southern Alps. It is regarded as one of the most scenic roads in New Zealand, and with a peak elevation of , the country's third highest highway after the Desert Road () and the Lindis Pass (). However, the "Milford Road" part is also one of the more dangerous public roads in New Zealand, with injury crash rates around 65% higher than the rest of New Zealand's network, and a fatality crash rate of almost twice average ...
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