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Karetai Peak
Karetai Peak is a mountain in Fiordland, New Zealand. Description Karetai Peak is part of the Darran Mountains and it is situated nine kilometres east of Milford Sound 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 southwest slope drains into the headwaters of the Donne River, whereas the east slope drains to Chasm Creek and the northwest slope to Cleft Creek which are both tributaries of the Hollyford River. Topographic relief is significant as the summit rises above the Donne Valley in one kilometre. The nearest higher neighbour is Te Wera Peak, 1.67 kilometre to the north. This mountain's toponym has been officially approved by the New Zealand Geographic Board. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Wera Peak
Te Wera Peak, also known as Mount Te Wera, is a mountain in Fiordland, New Zealand. Description Te Wera Peak is the fourth-highest peak of the Darran Mountains. It is situated in the Southland Region of the South Island, and set within Fiordland National Park which is part of the Te Wahipounamu UNESCO World Heritage Site. Precipitation runoff from the mountain drains into Cleft Creek and Chasm Creek which are tributaries of the Hollyford River. Topographic relief is significant as the summit rises above the Hollyford Valley in four kilometres, and above Cleft Creek in two kilometres. The nearest higher neighbour is Mount Madeline, five kilometres to the north. The first ascent of the summit was made in 1938 by David Lewis and Lindsay Stewart. This mountain's toponym has been officially approved as Te Wera Peak by the New Zealand Geographic Board. "Te Wera" is a Māori term meaning "the burning" or "the heat." Climate Based on the Köppen climate classification, Te Wera Peak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Site
World Heritage Sites are landmarks and areas with legal protection under an treaty, international treaty administered by UNESCO for having cultural, historical, or scientific significance. The sites are judged to contain "cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site is nominated by its host country and determined by the UNESCO's World Heritage Committee to be a unique landmark which is geographically and historically identifiable, having a special cultural or physical significance, and to be under a sufficient system of legal protection. World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains or wilderness areas, and others. A World Heritage Site may signify a remarkable accomplishment of humankind and serve as evidence of humanity's intellectual history on the planet, or it might be a place of grea ... [...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] |
Underwood And Karetai
Underwood may refer to: People *Underwood (surname), people with the surname Places Australia *Underwood, Queensland, a suburb of Logan City, Australia *Underwood, Tasmania, a locality United Kingdom * Underwood, Devon, a location * Underwood, Newport, village in Wales *Underwood, Nottinghamshire, village in England * Underwood, Pembrokeshire, a location *Weston Underwood, Buckinghamshire, village in England *Weston Underwood, Derbyshire, village in England *Wotton Underwood, village in England Canada * Underwood, Markham, Ontario, an unincorporated community now within the city of Markham * Underwood, Bruce County, Ontario, a village United States * Underwood, Shelby County, Alabama, a place in Alabama *Underwood-Petersville, Alabama, a census-designated place * Underwood, Indiana, an unincorporated community *Underwood, Iowa, a city *Underwood, Minnesota, a city * Underwood Township, Redwood County, Minnesota, a township *Underwood, New York, a hamlet within the town of Nor ... [...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] |
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 People
Māori () are the Indigenous peoples of Oceania, indigenous Polynesians, Polynesian people of mainland New Zealand. Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of Māori migration canoes, canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed Māori culture, a distinct culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Early contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi, Treaty of Waitangi/Te Tiriti o Waitangi in 1840, the two cultures coexisted for a generation. Rising ten ... [...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] |
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] |
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] |
Hollyford River
The Hollyford River / Whakatipu Kā Tuka is in the southwest of the South Island of New Zealand. It runs for through Fiordland, its sources being close to the Homer Tunnel and in Gertrude Valley in the southern Darran Mountains. At first, the river flows southeast and east, coming as close as 1 km to the east–west divide of the South Island, before continuing north through the glacier-formed Hollyford Valley. Near the end, the river passes through Lake McKerrow before reaching Martins Bay on the coast of the Tasman Sea north of Milford Sound. The Hollyford Track follows the river's course. Part of the river's course is traditionally regarded as the boundary between the Southland and Otago regions, however, current maps show the entirety of the Hollyford Valley contained within the Southland Region. In January 1863, Patrick Caples explored the river, naming it after his home town of Hollyford, County Tipperary in Ireland. Following the passage of the Ngāi Tahu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
