Mount Rudolf
Mount Rudolf is a mountain in New Zealand. Description Mount Rudolf is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of the South Island. This peak is located northeast of Aoraki / Mount Cook and set on the boundary shared by Aoraki / Mount Cook National Park and Westland Tai Poutini National Park. Precipitation runoff from the mountain drains north to the Waiho River and south to the Tasman River. Topographic relief is significant as the summit rises above the Rudolf Glacier in two kilometres. The nearest higher peak is The Minarets, 1.66 kilometre to the east. The toponyms of the mountain and glacier were applied by Dr. Robert von Lendenfeld to honour Rudolf, Crown Prince of Austria (1858–1889), the son of Emperor Franz Josef.''The New Zealand Alpine Journal'', Volume 6, New Zealand Alpine Club, 1935, p. 127. [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rudolf, Crown Prince Of Austria
Rudolf, Crown Prince of Austria (Rudolf Franz Karl Josef; 21 August 1858 – 30 January 1889) was the only son and third child of Franz Joseph I of Austria, Emperor Franz Joseph I and Empress Elisabeth of Austria. He was heir apparent to the imperial throne of the Austro-Hungarian Empire from birth. In 1889, he died in a suicide pact with his mistress (lover), mistress Baroness Mary Vetsera at the Mayerling incident, Mayerling hunting lodge. The ensuing scandal made international headlines. Background Rudolf was born at Schloss Laxenburg,"Crown Prince Rudolf (1858–1889)" (museum notes), Natural History Museum, Vienna, 2006. a castle near Vienna, as the son of Franz Joseph I of Austria, Emperor Franz Joseph I and Elisabeth of Bavaria, Empress Elisabeth. He was named after the first Habsburg King of Germ ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Alec And Peter Graham
Alexander Carter Graham (1881–1957) and Peter Graham (1878–1961) were mountaineers Mountaineering, mountain climbing, or alpinism is a set of outdoor activities that involves ascending mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas that have become sports ..., Mountain guide, guides and hotel operators in New Zealand. They were instrumental in the establishment of the early New Zealand tourist industry and earned themselves worldwide reputations as climbers and guides. Graham family of Ōkārito Alec and Peter Graham were born at Three Mile Beach, Ōkārito, the fifth and sixth children of nurse and midwife Isabella and her husband from Paisley, Scotland, David Graham, West Coast gold rush, a goldminer, storekeeper, Three Mile River ferryman and later a baker. The family made a farm at Franz Josef, New Zealand, Waiho by Franz Josef Glacier. After their father died in October 1900 four of the s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of The Canterbury Region
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Jervois
Mount Jervois is a mountain in New Zealand. Description Mount Jervois is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of the South Island. This peak is located northeast of Aoraki / Mount Cook and set on the boundary shared by Aoraki / Mount Cook National Park and Westland Tai Poutini National Park. Precipitation runoff from the mountain drains north to the Waiho River and south to the Tasman River. Topographic relief is significant as the summit rises above the Rudolf Glacier in one kilometre, and above the Tasman Glacier in four kilometres. The Centennial Hut is perched on the northwest ridge of this peak. Mount Jervois was named by Robert von Lendenfeld to honour the then-Governor of New Zealand, William Jervois, who served in that role from 1883 to 1889. Climbing The first ascent of the summit was made in April 1916 by Alex Graham and B. Marsden. [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tasman Glacier
Tasman Glacier (officially Haupapa / Tasman Glacier) is the largest glacier in New Zealand, and one of several large glaciers which flow south and east towards the Mackenzie Basin from the Southern Alps in New Zealand's South Island. Geography At in length, Tasman Glacier is still New Zealand's longest glacier, despite shrinking considerably from the 1990s onwards. It is as much as wide and thick, and lies entirely within the borders of Aoraki / Mount Cook National Park. The glacier covers an area of and starts at a height of above sea level. Snowfall during the winter and spring seasons may accumulate up to . After the summer melt, may remain in the high altitude glacier head. The Tasman flows south west from Hochstetter Dome and Mount Elie De Beaumont alongside the southern slopes of The Minarets and south along the eastern flank of New Zealand's two highest mountains, Mount Tasman and its higher southern neighbour Aoraki / Mount Cook. Although its upper reaches ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Green (New Zealand)
Mount Green is a mountain in New Zealand. Description Mount Green is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of South Island. This peak is located northeast of Aoraki / Mount Cook and set on the boundary shared by Aoraki / Mount Cook National Park and Westland Tai Poutini National Park. Precipitation runoff from the mountain drains north to the Callery River and south to the Tasman River. Topographic relief is significant as the summit rises above the Tasman Glacier in one kilometre, and above the Edwards Glacier in 0.5 kilometre. The nearest higher peak is Mount Walter, one kilometre to the northeast. The mountain's toponym was applied by Dr. Robert von Lendenfeld to honour William Spotswood Green (1847–1919), who made the first recorded attempt to climb Aoraki / Mount Cook with two companions in 1882, but less than 100 metres from the summit they were forced to turn back due ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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De La Beche (New Zealand)
De La Beche, also known as Mount De la Bêche, is a mountain in New Zealand. Description De La Beche is set on the crest or Main Divide of the Southern Alps and is situated on the boundary shared by the West Coast and Canterbury Regions of South Island. This peak is located northeast of Aoraki / Mount Cook and set on the boundary shared by Aoraki / Mount Cook National Park and Westland Tai Poutini National Park. Precipitation runoff from the mountain drains north to the Waiho River and south to the Tasman River. Topographic relief is significant as the summit rises above the Tasman Glacier in three kilometres. The mountain's toponym was applied by Julius von Haast to honour Henry De la Beche (1796–1855), an English geologist and the first director of the Geological Survey of Great Britain, who helped pioneer early geological survey methods. The first ascent was made in February 1894 by Tom Fyfe and George Graham via De La Beche Ridge. [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |