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Mauka Atua
Mauka Atua is a mountain in the Canterbury Region of New Zealand. Description Mauka Atua is located southwest of Christchurch and set between the Dobson Valley and Tasman Valley in the South Island. It is the highest peak in the Ben Ohau Range of the Southern Alps. Precipitation runoff from the mountain drains east to Lake Pukaki and west into the Dobson River. Topographic relief is significant as the summit rises above the Dobson Valley in four kilometres. The nearest higher peak is Mount Hopkins, 11 kilometres to the north-northwest. The mountain's name Mauka Atua means "to stand apart" in the Māori language and the toponym has been officially approved by the New Zealand Geographic Board.''Mauka Atua'' New Zealand Gazetteer, Retrieved 26 February 2025. Climbing Climbing routes with first ascents:[...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] |
Mount Hopkins (New Zealand)
Mount Hopkins is located in the Southern Alps of New Zealand's South Island. It lies to the southwest of Aoraki / Mount Cook, and rises to . Several rivers have their sources on or close to the slopes of Mount Hopkins, notably the Landsborough River to the west, the Dobson River to the east, and Hopkins River to the south. At Mount Hopkins, the traditional boundaries of the former Otago, Westland, and Canterbury Provinces meet, these boundaries survive today as provincial districts, and only serve for the purposes of determining anniversary days. However, the modern day boundaries of the Otago region, the West Coast region and the Canterbury region Canterbury () is a region of New Zealand, located in the central-eastern South Island. The region covers an area of , making it the largest region in the country by area. It is home to a population of The region in its current form was estab ... meet further south at Mt Strauchon, which is also on the Main Divide. Refere ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Sealy
Mount Sealy is a mountain in Canterbury Region of New Zealand. Description Mount Sealy is located in the Southern Alps and the Canterbury Region of South Island. This peak is situated southwest of Mount Cook Village and set within Aoraki / Mount Cook National Park. Precipitation runoff from the mountain drains south into the headwaters of the Dobson River, and north to the Hooker River. Topographic relief is significant as the summit rises above the Dobson headwaters in one kilometre. The nearest higher neighbour is Mount Burns, three kilometres to the west-northwest. The mountain's toponym was applied by Julius von Haast to honour Edward Sealy (1839–1903), a New Zealand surveyor, photographer, and explorer.''Mount Sealy'' New Zealand Gazetteer, Retrieved 1 January 2025. Climbing The |
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] |
Oceanic Climate
An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen climate classification, 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 an ... [...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] |
Norman Hardie
Norman David Hardie (28 December 1924 – 31 October 2017) was a New Zealand climber who was one of the climbers on the 1955 British Kangchenjunga expedition who first reached the summit of the 8,586-metre (28,169 ft) mountain, the third-highest mountain in the world. Early life Hardie was born in Timaru in 1924. He left school early and, encouraged by his father, spent two seasons hunting deer in the Boyle and Hurunui River valleys. Encouraged by a local Timaru engineer, in 1943 Hardie enrolled at Canterbury University College for a degree in civil engineering. He continued hunting to finance his studies, but became increasingly involved in tramping (the New Zealand term for hiking) and mountaineering. He graduated from Canterbury in 1947 and worked at Lake Pukaki on the hydroelectricity scheme. He first met Edmund Hillary during a rescue mission for an injured climber on La Perouse in 1948 described as "the most arduous rescue in New Zealand's climbing history". A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geographic Board
The New Zealand Geographic Board Ngā Pou Taunaha o Aotearoa (NZGB) is the authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local Māori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The board was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (Ngā Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The NZGB secretariat is part of Toitū Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geogra ... [...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] |
Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drainage characteristics, drainage systems, groundwater systems, water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Alps
The Southern Alps (; officially Southern Alps / Kā Tiritiri o te Moana) are a mountain range extending along much of the length of New Zealand, 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 drainage basin, 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 Region, Marlborough, Canterbury Region, Canterbury and Otago regions of New Zealand, regions to the southeast and the Tasman Region, Tasman and West Coast, New Zealand, West Coast regions to the northwest. Names The Māori language, Māori name of the range is , meaning "the Fata Morgana (mirage), Mirage of the Ocean". The English people, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
