| Baekdu Mountain | |
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Baekdu Mountain volcano, April 2003 |
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| Location of Baekdu Mountain in North Korea (on Chinese border) | |
| Elevation | 2,744 metres (9,003 ft) |
| Location | Ryanggang, ( Jilin, ( |
| Prominence | 2,593 metres (8,507 ft) |
| Coordinates | 42°00′20″N 128°03′19″E / 42.00556°N 128.05528°E / 42.00556; 128.05528Coordinates: 42°00′20″N 128°03′19″E / 42.00556°N 128.05528°E / 42.00556; 128.05528 |
| Type | Stratovolcano |
| Last eruption | 1903[1] |
| Listing | Country high point Ultra |
Baekdu Mountain, also known as Changbai Mountain in China, is a volcanic mountain on the border between North Korea and China, located at 42°00′24″N 128°03′18″E / 42.00667°N 128.055°E / 42.00667; 128.055. At 2,744 m (9,003 ft), it is the highest mountain of the Changbai mountain range to the north and Baekdudaegan mountain range to the south. It is also the highest mountain on the Korean peninsula and Manchuria.
The Korean name, Baekdu-san (백두산, 白頭山), means "white-headed mountain". The Chinese name, Changbai Shan (長白山/长白山),means"perpetually white mountain" and the Manchu name, Golmin Šanggiyan Alin mean "perpetually white mountain"as well. English-language volcanology resources often refer to the mountain as Baitoushan from the Chinese pinyin rendering of the Korean Hanja 白頭山. Other alternative names include Paektu-san and Bai Yun Feng.
A large crater lake, called Heaven Lake (천지, 天池), is located within the caldera atop of the mountain.
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| Baekdu Mountain
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| Chinese name | |||||||||
| Traditional Chinese: | 長白山 | ||||||||
| Simplified Chinese: | 长白山 | ||||||||
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| Korean name | |||||||||
| Chosŏn'gŭl: | 백두산 | ||||||||
| Hancha: | 白頭山 | ||||||||
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| Manchu name | |||||||||
| Manchu: | Golmin Šanggiyan Alin | ||||||||
Baekdu Mountain is stratovolcano whose cone is truncated by a large caldera, about 5 km (3.1 miles) wide and 850 m (2,789 ft) deep, partially filled by the waters of Heaven Lake.[1] The caldera was created by a major eruption in 969 AD (± 20 years).[2] Volcanic ash from this eruption has been found as far away as the southern part of Hokkaidō of Japan. The lake has a circumference of 12 to 14 kilometres (7.5-8.7 miles), with an average depth of 213 m (699 ft) and maximum depth of 384 m (1,260 ft). From mid-October to mid-June, the lake is typically covered with ice.
The central section of the mountain rises about 3 mm every year, due to rising levels of magma below the central part of the mountain. Sixteen peaks exceeding 2,500 m (8,200 ft) line the caldera rim surrounding Heaven Lake. The highest peak, called Janggun Peak, is covered in snow about eight months of the year. The slope is relatively gentle until about 1,800 metres (5,905 ft).
Water flows north out of the lake, and near the outlet there is a 70 metre (230 ft) waterfall. The mountain is the source of the Songhua, Tumen (Duman) and Yalu (Amnok) rivers.
The weather on the mountain can be very erratic. The annual average temperature at the peak is about -8.3 degrees Celsius (17 degrees Fahrenheit). During summer, temperatures of about 18 degrees Celsius can be reached, and during winter temperatures can drop to -48 degrees Celsius (-54 degrees Fahrenheit). Average temperature is -24 degrees Celsius (-11 degrees Fahrenheit) in January, 10 degrees Celsius (50 degrees Fahrenheit) in July, remaining below freezing for eight months of the year. Average wind speed is 11.7 metres per second, reaching an average of 17.6 m/s in December. Relative humidity averages 74%. In recent decades, there has been significant climate warming on the mountain. Summer snow cover on the peak has reduced dramatically during that time.
There are five known species of plants in the lake on the peak, and some 168 were counted along its shores. The area is a known habitat for tigers, bears, leopards, wolves, and wild boars. Deer in the mountain forests, which cover the mountain up to about 2000 metres, are of the Paekdusan roe deer kind. Many wild birds such as black grouse, owls, and woodpecker are known to inhabit the area. The forest on the Chinese side is ancient and almost unaltered by humans. Birch predominates near the tree line, and pine lower down, mixed with other species. In recent decades, significant climate warming has resulted in changes in the structure of the ancient forests on the upper slopes, with a change over from birch to more pine, and a thickening of the forest canopy. There has been extensive deforestation on the lower slopes on the North Korean side of the mountain.
The Baekdu Mountain has been worshipped by the surrounding peoples throughout history. Both the Koreans and Manchus (an ethnic group in China) consider it the place of their ancestral origin.
Koreans consider Mount Baekdu as the place of their ancestral origin and as a sacred mountain, one of the three “spirited” mountains; the one contained in the legendary foundation of Korea. From the beginning of history through the Three Kingdoms period, to the Goryeo and Joseon Dynasties, Koreans have spiritually depended upon the “divine” mountain.
The mountain was considered sacred by Koreans throughout history. The legendary beginning of Korea's first kingdom, Gojoseon (2333 BC–108 BC), takes place here. Many subsequent kingdoms of Korea, such as Buyeo, Goguryeo, Balhae, Goryeo and Joseon, considered the mountain sacred and held worshipping rituals for the mountain.[3][4]
The Goryeo dynasty (935–1392) first called the mountain Baekdu [5], recording that the Jurchens across the Yalu River were made to live outside of Baekdu Mountain. The Joseon Dynasty (1392–1910) recorded volcanic eruptions in 1597, 1668, and 1702. The 15th century, King Sejong the Great strengthened the fortification along the Tumen and Yalu rivers, making the mountain a natural border with the northern peoples.[6]
Dense forest around the mountain provided bases for Korean armed resistance against the Japanese occupation, and later communist guerrillas during the Korean War. North Korea claims that Kim Il-sung organized his resistance against the Japanese forces there and that Kim Jong-il was born there, although records outside of North Korea show that these events took place a short distance within the borders of the Soviet Union.
It was first recorded in the Chinese classic text Shan Hai Jing with the name Buxian Shan (不咸山,即神仙山, the Mountain with God). It's also called Shanshan Daling (單單大嶺, the Big Big Big Mountain. 《說文》:“單,大也。”) in the Canonical Book of the Eastern Han Dynasty. In the Canonical Book of the Tang Dynasty, it was called Taibai Shan (太白山, the Grand Old White Mountain)[7]. The current Chinese name Changbai Shan(長白山, Perpetually White Mountain)was first used in the Liao Dynasty (907-1125)[8] and then the Jurchen Jin Dynasty (1115-1234)[9].
The Jurchen Jin Dynasty (1115–1234) bestowed the title "the King Who Makes the Nation Prosperous and Answers with Miracles" (興國靈應王, Xingguo Lingying Wang) on the mountain god in 1172 and it was promoted to "the Emperor Who Cleared the Sky with Tremendous Sagehood" (開天宏聖帝, Kaitian Hongsheng Emperor) in 1193. During the Manchu Qing Dynasty, the Kangxi Emperor designated Changbai Mountain as the legendary birthplace of the imperial family Aisin Gioro following a survey, although it is no longer supported. He set a forbidden zone around the mountain, although it was still in dispute whether it was part of Korea (Joseon) or China. The Qing Dynasty held annual rites for the mountain, as did the earlier Jin Dynasty.
Because of the continuous entry of Korean people into Gando, a region in Manchuria that lay between the Tumen and Yalu Rivers, in 1712, Manchu and Korean officials surveyed the area and negotiated a border agreement. To mark the agreement, they built a monument describing the boundary at a watershed, near the south of the crater lake at the mountain peak. The interpretation of the inscription caused a territorial dispute from the late 19th century to the early 20th century, and is still disputed by academics today. The 1909 Gando Convention between Qing and Japan (Japan responsible for Korea’s foreign affairs according to Eulsa Treaty, later declared null and void by Korea) recognized the area north and east as Chinese territory. The border was further clarified in 1962, when China and North Korea negotiated a border treaty on the mountain border in response to minor disputes. The two countries agreed to share the mountain and the lake at the peak, with Korea controlling approximately 60% and gaining approximately 230 km² in the treaty.[10]
Some South Korean groups argue that recent activities conducted on the Chinese side of the border, such as economic development, cultural festivals, infrastructure development, promotion of the tourism industry, attempts at registration as a World Heritage Site, and bids for a Winter Olympic Games, are an attempt to claim the whole mountain as Chinese territory. These groups object to China's use of Changbai Mountain, which has been used since Liao Dynasty[8] and the earlier Jin Dynasty (1115-1234)[9]. However, in more pre-modern eras[citations needed] this mountain was known and referred to as BaiTou Mountain (the Chinese literation of "Baekdu Mountain") by the Chinese residents of the mountain themselves, some even claim that Changbai mountain seems to be a more recent (mere decades ago) renaming of Baekdu (BaiTou) Mountain, even though Changbai is found and used in Qing dynasty records. Some groups also regard the entire mountain as Korean territory that was given away by North Korea, when the Japanese sold this land without any Korean consent in the deal of 1909. Both European maps and Chinese maps dating before the annexation of Baekdu Mountain and Gando show these areas to be under Korean Joseon Dynasty control.[11][12][13][14]
During the 2007 Asian Winter Games, which were held in Changchun, China, a group of South Korean athletes held up signs during the award ceremony which stated "Mount Baekdu is our territory". Chinese sports officials delivered a letter of protest on the grounds that political activities violated the spirit of the Olympics and were banned in the charter of the International Olympic Committee and the Olympic Council of Asia. The head of the Korea Olympic Committee responded by stating that the incident was accidental and held no political meaning.[15][16][17][18] South Korea has attempted to avoid having this issue become a source of friction between South Korea and China. The athletes' gesture did not become as big an issue as Liancourt Rocks and the Sea of Japan naming dispute. The 2007 official National Atlas of Korea [19] clearly shows the boundary as per the 1962 agreement, roughly splitting the mountain and the caldera lake. Nevertheless, there will remain Korean citizens who will continue to claim that the mountain should be returned to Korean dominion.[20][21]
Foreign visitors, mostly South Koreans, usually climb the mountain from the Chinese side, although Baekdu Mountain is a common tourist destination for the few foreign tourists in North Korea.
There are a number of monuments on the North Korean side of the mountain. Baekdu Spa is a natural spring and is used for bottled water. Pegae Hill is a famous camp site of the Korean People’s Revolutionary Army during their struggle against Japanese colonial rule. There are also a number of secret camps which are now open to the public. There are several waterfalls, including the Hyongje Falls which splits into two separate falls about a third from the top.
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v • d • e
Territorial disputes in East, South, and Southeast Asia |
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|---|---|---|---|
| Type | Territory | Currently Administered by | Claimants |
| Land: | Aksai Chin | ||
| Arunachal Pradesh | |||
| Baekdu Mountain | |||
| Heixiazi/Bolshoy Ussuriysky (Eastern part)2 | |||
| Indo-Bangladesh enclaves3 | |||
| Kashmir3 | |||
| Kachin State | |||
| Kayin State | |||
| Korean Peninsula and its adjacent islands3 | |||
| Mainland China2 | |||
| Mongolia2 | |||
| Pamir Mountains3 | |||
| Pattani | |||
| North Borneo (Sabah)2 | |||
| Shan State | |||
| Sixty-Four Villages East of the River2 | |||
| Tannu Uriankhai (now Tuva Republic of Russia)2 | |||
| Tibet | |||
| Trans-Karakoram Tract | |||
| Wa State | |||
| Islands and Waters: | Kinmen | ||
| Liancourt Rocks | |||
| Macclesfield Bank | |||
| Matsu | |||
| Paracel Islands | |||
| South Ledge | |||
| Pratas Islands | |||
| Scarborough Shoal | |||
| Senkaku Islands | |||
| Sir Creek3 | |||
| Socotra Rock | |||
| Southern Kuril Islands | |||
| Spratly Islands3 | |||
| Taiwan and Penghu2 | |||
| Notes: | 1Government in exile/exiled group. 2Inactive dispute. 3Divided among multiple claimants. |
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