|
Mount D'Archiac
Mount D'Archiac is a mountain in the Canterbury Region of New Zealand. Description Mount D'Archiac is the highest peak in the Two Thumb Range which is a subrange of the Southern Alps. It is situated west of the city of Christchurch and is set on the eastern boundary of Aoraki / Mount Cook National Park in the Canterbury Region of South Island. Precipitation runoff from the mountain drains east to the Havelock River and west to the Godley River. Topographic relief is significant as the summit rises in two kilometres. The first ascent of the summit was made in March 1910 by Jim Dennistoun, Laurence Earle, and Jack Clarke via the East Ridge and Forbes Glacier. The nearest higher peak is Mount Annan, 20 km to the west-southwest. Etymology The mountain was named by Julius von Haast to honour Vicomte d'Archiac (1802–1868), a French geologist and professor of palaeontology at the Paris Museum of Natural History. The Māori name for this mountain is "Kāhuikaupeka" which mea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wolseley
Mount Wolseley is a mountain in the Canterbury Region of New Zealand. Description Mount Wolseley is situated less than one kilometre east of the crest of the Southern Alps in Aoraki / Mount Cook National Park. It is located west of the city of Christchurch in the Mackenzie District of the Canterbury Region in the South Island. Precipitation runoff from the mountain drains into headwaters of the Godley River. Topographic relief is significant as the summit rises in two kilometres. The first ascent of the summit was made in December 1920 by Will Kennedy and Jack Lippe.''Mt Wolseley'' New Zealand Alpine Club, Climbnz.org, Retrieved 22 December 2024. The nearest higher peak is Mount Loughnan, three kilometres ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Forbes (New Zealand)
Mount Forbes is a mountain in the Canterbury Region of New Zealand. Description Mount Forbes is located at the northern end of the Sibbald Range which is a subrange of the Southern Alps.''Sibbald Range'' New Zealand Gazetteer, Retrieved 23 December 2024. It is situated west of the city of and is set on the northeastern boundary of in the of |
Te Kahui Kaupeka Conservation Park
Te Kahui Kaupeka Conservation Park is a protected area in the Timaru District and Canterbury Region of New Zealand's South Island. The park is managed by the New Zealand Department of Conservation The Department of Conservation (DOC; Māori language, Māori: ''Te Papa Atawhai'') is the public service department of New Zealand charged with the conservation of New Zealand's natural and historical heritage. An advisory body, the New Zealand .... Geography The park covers . History The park was established in 2008. References Forest parks of New Zealand Parks in the Canterbury Region Timaru District 2008 establishments in New Zealand Protected areas established in 2008 {{CanterburyNZ-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McClure Peak
McClure Peak is a mountain in New Zealand. Description McClure Peak is located on the crest or Main Divide of the Southern Alps, with the summit set on the boundary shared by the Canterbury and West Coast Regions of the South Island. It is situated west of the city of Christchurch on the northeastern boundary of Aoraki / Mount Cook National Park. Precipitation runoff from the mountain drains east to the Havelock River via St Winifred Stream, southwest into the headwaters of the Godley River, and northwest to the Perth River via Bettison Stream. Topographic relief is significant as the summit rises above Bettison Stream in approximately two kilometres, and above St Winifred Glacier in one kilometre. The nearest higher neighbour is Mount D'Archiac, 4.6 km to the southwest. The first ascent of the summit was made in February 1925 by Jack Lippe and Will Kennedy. Etymology The mountain was originally named Mount Tyndall by Julius von Haast, but this toponym was transferred ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tundra Climate
The tundra climate is a polar climate sub-type located in high latitudes and high mountains. It is classified as ET according to the Köppen climate classification. It is a climate which at least one month has an average temperature high enough to melt snow (), but no month with an average temperature in excess of . If the climate occurs at high elevations, it is known as alpine climate. Despite the potential diversity of climates in the ''ET'' category involving precipitation, extreme temperatures, and relative wet and dry seasons, this category is rarely subdivided. Rainfall and snowfall are generally slight due to the low vapor pressure of water in the chilly atmosphere, but as a rule potential evapotranspiration is extremely low, allowing soggy terrain of swamps and bogs even in places that get precipitation typical of deserts of lower and middle latitudes. The amount of native tundra biomass depends more on the local temperature than the amount of precipitation. Tundra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Language
Māori (; endonym: 'the Māori language', commonly shortened to ) is an Eastern Polynesian languages, Eastern Polynesian language and the language of the Māori people, the indigenous population of mainland New Zealand. The southernmost member of the Austronesian language family, it is related to Cook Islands Māori, Tuamotuan language, Tuamotuan, and Tahitian language, Tahitian. The Māori Language Act 1987 gave the language recognition as one of New Zealand's official languages. There are regional dialects of the Māori language. Prior to contact with Europeans, Māori lacked a written language or script. Written Māori now uses the Latin script, which was adopted and the spelling standardised by Northern Māori in collaboration with English Protestant clergy in the 19th century. In the second half of the 19th century, European children in rural areas spoke Māori with Māori children. It was common for prominent parents of these children, such as government officials, to us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
