My Notebook
The World's 14 Highest Mountain Peaks (above 8,000 meters)
See Named Summits in the U.S. Over 14,000 Feet Above Sea Level for U.S. Peaks.
See also Climbing the World's 14 8,000-meter Peaks, The Seven Summits, Mortals on Mount Olympus: A History of Climbing Everest, and the Everest Almanac.
All 14 of the world's 8,000-meter peaks are located in the Himalaya or the Karakoram ranges in Asia. According to Everestnews.com, only 13 climbers have reached the summits of all 14: Reinhold Messner (Italy) was first, followed by Jerzy Kukuczka (Poland), Ehardt Loretan (Switzerland), Carlos Carsolio (Mexico), Krzysztof Wielicki (Poland), Juan Oiarzabal (Spain), Sergio Martini (Italy), Park Young Seok (Korea), Hang-Gil Um (Korea), Alberto Inurrategui (Spain), Han Wang Yong (Korea), Ed Viesturs (U.S.), and Alan Hinkes (British).
Mountain | Location | Height | First to summit (nationality) | Date | |
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Meters | Feet | ||||
1. Everest1 | Nepal/Tibet | 8,850 | 29,035 | Edmund Hillary (New Zealander, UK), Tenzing Norgay (Nepalese) | May 29, 1953 |
2. K2 (Godwin Austen) | Pakistan/China | 8,611 | 28,250 | A. Compagnoni, L. Lacedelli (Italian) | July 31, 1954 |
3. Kangchenjunga | Nepal/India | 8,586 | 28,169 | G. Band, J. Brown, N. Hardie, S. Streather (UK) | May 25, 1955 |
4. Lhotse | Nepal/Tibet | 8,516 | 27,940 | F. Luchsinger, E. Reiss (Swiss) | May 18, 1956 |
5. Makalu | Nepal/Tibet | 8,463 | 27,766 | J. Couzy, L. Terray, J. Franco, G. Magnone-Gialtsen, J. Bouier, S. Coupé, P. Leroux, A. Vialatte (French) | May 15, 1955 |
6. Cho Oyu | Nepal/Tibet | 8,201 | 26,906 | H. Tichy, S. Jöchler (Austrian), Pasang Dawa Lama (Nepalese) | Oct. 19, 1954 |
7. Dhaulagiri | Nepal | 8,167 | 26,795 | A. Schelbert, E. Forrer, K. Diemberger, P. Diener (Swiss), Nyima Dorji, Nawang Dorji (Nepalese) | May 13, 1960 |
8. Manaslu | Nepal | 8,163 | 26,781 | T. Imamishi, K. Kato, M. Higeta, (Japanese) G. Norbu (Nepalese) | May 9, 1956 |
9. Nanga Parbat | Pakistan | 8,125 | 26,660 | Hermann Buhl (Austrian) | July 3, 1953 |
10. Annapurna | Nepal | 8,091 | 26,545 | M. Herzog, L. Lachenal (French) | June 3, 1950 |
11. Gasherbrum I | Pakistan/China | 8,068 | 26,470 | P. K. Schoeing, A. J. Kauffman | July 4, 1958 |
12. Broad Peak | Pakistan/China | 8,047 | 26,400 | M. Schmuck, F. Wintersteller, K. Diemberger, H. Buhl (Austrian) | June 9, 1957 |
13. Gasherbrum II | Pakistan/China | 8,035 | 26,360 | F. Moravec, S. Larch, H. Willenpart (Austrian) | July 7, 1956 |
14. Shisha Pangma | Tibet | 8,013 | 26,289 | Hsu Ching and team of 9 (Chinese) | May 2, 1964 |
念青唐古拉山,藏语意为“灵应草原神”,位于拉萨以北100公里处,屹立在西藏高原中部,自西向东约600公里,它是雅鲁藏布江和怒江两条大水系的分水岭,同时将西藏自治区分为藏北、藏南、藏东南三大地域。山顶最高处海拔7117米,终年白雪皑皑,云雾缭绕,雷电交加,神秘莫测。山势笔直,险要壮观。主峰顶部形似鹰嘴,多断岩峭壁。白天云雾缭绕,常年为冰雪覆盖。它有三条主要山脊:西山脊、东山脊和南山脊。北坡附近,主要以横向的山谷冰川和悬冰川为主,悬冰川冰舌末端往往高达5700米。念青唐古拉山在宗教上是全藏著名的护法神,也是北部草原众神山的主神。本教和佛教信徒都敬奉此山。念青唐古拉山和纳木错是西藏最引人注目的神山圣湖,成为世界屋脊上最大的宗教圣地和旅游景观。
A multitude of enormous mountain ranges stretch on the Plateau including the Himalayas in the southwest, the Kunlun Mountains in the north, the Karakorum Mountains in the northwest, the Hengduan Mountains in the southeast, and the Danggula Mountains, the Gandise Mountains as well as the Nyainqentanglha Mountains in the middle. These towering mountain ranges form the geomorphologic framework of Tibet and are the development center of both ancient and modern glaciers. Glaciers are widely dispersed over mountains that are over 5,000 meters high and covered with snow all the year round, which is a grand spectacle. Besides many secondary mountain chains, between these above-mentioned lofty mountain systems are mainly basins, highlands and wide ravines such as the North Tibet Plateau and the South Tibet Valley in the south. The deeply-cut Hengduan Mountains in the southeast with parallel hills and gorges running hem north to south are the transitional region from the Plateau to the Sichuan Basin and Yunnan-Guizhou Highland.
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The Himalayas Mountain System Stretching on the southern margin of Tibet Autonomous Region in China, the towering Himalayas mountain range, which is about 2,400 kilometers long and 200 to 300 kilometers wide and whose elevation averages 6,200 meters, is the highest and youngest mountain system on the earth. The word "Himalayas" comes from Sanskrit with "Hima" meaning snow and "Layas" meaning residence or hometown. Thus its original meaning is the hometown of snow. Stretching roughly from east to west, the mountain chain looks like an arc curving southward, with Mt. Kangchenjunga at 8,585 meters as the salient. Geologically speaking, the existence of the Himalayas has an extremely significant influence on the geomorphologic contour of the whole Qinghai-Tibet Plateau and even of Asia.
The Himalayas mountain system comprising many parallel mountain chains is divided into the Greater Himalayas, Lesser Himalayas and foothills from north to south. As the main body of the entire mountain system, the Greater Himalayas that is 50 to 90 kilometers wide is mainly located at the boundary between China and its southern neighboring countries. The Greater Himalayas is habitually divided into three parts: the east Himalayas between Namjagbarwa and Chomolhali Peak in Yadong, middle Himalayas between Chomolhali and Namonanyi peaks (in Burang), and west Himalayas between Namonanyi and Namgyia Palbate peaks in the west. Snow-capped mountains stand in great numbers on the middle Himalayas that is the highest part of the whole Himalayas mountain system. There are more than 40 mountains over 7,000 meters high and many mountain peaks over 8,000 meters high including Mt. Qomolangmo (8,848 meters), Lozi Peak (8,5l6 meters), Markalu Peak (8,463 meters), Qowowuyag Peak (8,20l meters) and Xixiabangma (8,0l2 meters), all of which are at or within China's boundary.
The dissymmetrical topography of the Himalayas mountain system from north to south is mainly caused by the rising southern side of the Himalayas during the course of the drastic uplift of the Plateau. On the sheer southern side of the Himalayas mountain system a majestic slope has been formed from the mountain downward to the Gangetic Plain with a sharp drop of around 6,000 meters. Due to abundant rainfall as well as the consequent strong erosion of the torrents, many deeply cut gorges are usually formed in the trunk stream. In most cases, valleys of branches with weak downward erosion take the form of hanging valleys halfway up the mountain with a drop of tens of meters. Spectacular waterfalls or cascades can be seen in these hanging valleys. The northern side of the Himalayas mountain system is relatively smooth, descending as stairs to the highlands and lake basins at the foot of the mountain range with a drop of only 1,500 meters or so. Accumulative topography is developed in broad and level valleys formed by streams with weak erosion on the northern side of the mountain system where rainfall is little and the erosive datum plane is quite high. Conditioned by the geological structure, the Himalayas mountain chain is transversely cut by many rivers rising on the northern side, shaping up deep and great canyons in which rushing currents are like waterfalls. Both the well-known Yarlung Zangbo Grand Canyon at the eastern end of the Himalayas mountain range and the Xiangquan Ravine in the upper reaches of the Indus River are good examples.
The Gandise-Nyainqentanglha Mountain System The Gandise-Nyainqentanglha mountain system between the Shiquan River in the west and the Boshula range in the Hengduan mountainous area in the east looks like an arc chain stretching continuously from east to west, which is about l, 600 kilometers long and 80 kilometers wide from north to south. Its elevation averages 5,800 to 6000 meters. The two ends of this mountain chain are relatively high with the middle sector more or less low The southern side is very precipitous with a relative altitude of around 2,000 meters, while the terrain on the northern side is quite level with a relative altitude of l,000 meters or so.
The word "Gandise" stems from Tibetan and Sanskrit, meaning "snowy mountain." The Gandise-Nyainqentanglha mountain system is marked by widely distributed extremely high mountains. Except for Norbogangri (7,095 meters), Kangrinboqe (6,638 meters) - the highest peak of the Gandise Mountains, and Mt. Nyainqentanglha (7, 162 meters) – the highest peak of the Nyainqentanglha Mountains, there are not many mountain peaks with elevations of over 6,500 meters here. Nevertheless, as far as the whole mountain body is concerned, the topography comprising large numbers of mountains over 5,500 meters high looks more complete than that of the Himalayas. This is related to its location in the interior of the Plateau. In other words, the Gandise-Nyainqentanglha is a colossal mountain system in the world where extremely high mountains are relatively concentrated. Located in the middle and south of the Qinghai-Tibet Plateau, the Gandise-Nyainqentanglha mountain system is an important geographical boundary. Its main body is the watershed between the inland rivers and outflowing rivers on the Plateau. On the southern side of the mountain system are the Shiquan River in the upper reaches of the Indus River and the Yarlung Zangbo river system. Most streams on the northern side that are much smaller in terms of their development empty into the lakes on the North Tibet Plateau.
There is snow-covering over large areas in the eastern sector of the Nyainqentanglha Mountains - one of the developmental centers of modern glaciers on the Plateau-where the longest modem marine glacier in China lies. Modern glaciers on the Gandise Mountains in the west are poorly developed, such as the glacier on Kangrinboqe that is only 4,000 meters long.
The Karakorum-Danggula Mountain System The Karakorum-Danggula mountain system comprising many parallel mountain ranges extends from east to west. Its altitude averages 5,000 to 6,000 meters. The Karakorum Mountains are part of the so-called Congling Range described in ancient Chinese books. There are three mountains with elevations of over 8,000 meters here, including the famous world's second highest peak-Mt. Chogori (i.e. Mt. Godwin Austen, 8,611 meters high), all of which stand at China's boundary The relatively complete western body of the Karakorum Mountains with ample rainfall is one of the distribution centers of modem glaciers on the Plateau where glaciation is very well developed. The eastern mountain body with gentle slopes is somewhat broken. Both the scope and the intensity of glaciation are much smaller here. The Danggula Mountains that are l60 kilometers wide from north to south are composed of many broad mountains. The Greater Danggula Mountains, the main body, stand lofty and steep with cone-shaped peaks. Mt. Geladaindong, the highest peak with an elevation of 6,62l meters, is the source of the Yangtze River. The Danggula Mountains are also the watershed between the Yangtze and Nujiang River (or Salween River). The total area of modem glaciers in the entire mountain range reaches 2,082 km2.
The Kunlun Mountain System The endless Kunlun mountain chain meandering between the Pamirs in the west and northwest Sichuan in the east is the boundary mountain between Tibet Autonomous Region and Xinjiang Uygur Autonomous Region, which is 2,500 kilometers long. Due to its colossal height and length, the Kunlun Mountains traversing Central Asia have long been known as the "Backbone of Asia." The western Kunlun mountainous region that is l50 kilometers wide and with an average altitude of some 6,000 meters is higher than the Tarim Basin by 4,000 to 5,000 meters. Cut by tributaries of the Tarim River, valleys in the western Kunlun mountainous region usually take the form of gorges, while wide ravines and basins parallel to the mountain ranges are situated up stream. The western Kunlun Mountains with ample rainfall are called the "Wet Island in the Desert." Main peaks include Mt. Gonggar (7,7l9 meters), Mt. Muztagata (7,546 meters) and Mt Muz (6,638 meters) where modern glaciers are developed. Melting glacial water converges into rivers, which are the precious source of water supply to oases in the Tarim Basin. Stretches of woods can be seen around the gorges whose elevations are from 3,200 to 3,700 meters. Glaciation is diminishing eastward markedly while glacial fringe topography is becoming widespread.
The eastern Kunlun Mountains are beyond Tibet Autonomous Region. Following the southern margin of the Qaidam Basin and then turning southeast, the eastern Kunlun Mountains are divided from north to south into three branches. The northern branch is composed of the Qimantage Mountains; the middle branch comprises Alge Mountains that extend eastward into Bokarlaiketage, Bolhanboda and Nganimaqen Mountains (i.e. Stone Piling Mountains); the southern branch includes the Hoh Xil and Bayankela Mountains. Maqengangri Peak, the highest peak of the Nganimaqen, rises 6,289 meters above sea level. Mozetage, the highest peak of the eastern Kunlun mountain range, is 6,973 meters high. The word "Bayankela" stems from Mongolian, meaning "green and gorgeous mountains." It is translated as "Mobilichiba" in Tibetan, meaning "the boundary between the Yellow River and the Tongtian River."
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lthough golf has been played for centuries throughout the world, the sport is still relatively new in China. China’s first golf club was established in 1984 and over the past 23 years, has expanded into over 300 golf courses and millions of people who now play the game. As China’s development continues to expand in the 21st century, golf’s popularity will increase as more and more Chinese begin to play a game that was once reserved only for society’s elite.
Nowhere is the popularity of golf more evident than in China’s largest city, Shanghai. With over 25 golf courses and numerous driving ranges, Shanghai has become one of China’s leading destinations to enjoy the game. The international golf scene in Shanghai has exploded in recent years and now hosts a variety of international golf tournaments bringing the best players in the world to Shanghai. The annual HSBC Champions and BMW Asian Open are two of Asia’s largest tournaments and are conducted annually in Shanghai.