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Feng Jinglan
Feng Jinglan (9 March 1898 – 29 September 1976), courtesy name Huaixi (), was a Chinese mineralogist and geologist. He was one of the founders of mineralogy in China. He was an academician of the Chinese Academy of Sciences. Biography Feng was born into a landlord's family in the town of , in Tanghe County, Hebei, on 9 March 1898, to Feng Taiyi (), an assistant to the Qing government official Zhang Zhidong, and Wu Qingzhi (). His elder brother Feng Youlan (1895–1990) was a philosopher. His younger sister Feng Yuanjun (1900–1974) was a writer. He secondary studied at Henan Provincial Second School in Kaifeng. In 1916, he was admitted to Peking University. In 1918, he pursued advanced studies in the United States on government scholarships, first studying mine geology in Colorado School of Mines and then studying mineralogy, petrology and physiography in Columbia University with a master's degree in 1923. He returned to China in 1923 and that same year became an ...
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Féng
Féng () is a Chinese surname. It is 9th on in the Song Dynasty ''Hundred Family Surname'' poem and is reported as the 31st most common Chinese last name in 2006. Unlike the less common Feng name "phoenix" (fourth tone) it is a rising second tone féng in modern Mandarin. The character itself, is made up of the character for "wikt:馬, Horse" with an wikt:冰, ice Radical (Chinese character), radical consisting of two strokes to the left that is meant to suggest speed or galloping. Historical roots The surname descended from the 15th son of King Wen of Zhou, Gao, Duke of Bi, Gao the Duke of Bi (畢公高), whose last name was Ji (surname), Ji. During the Spring and Autumn period, an official of the Zheng kingdom, Feng Jian Zi was awarded the land of Feng (Henan province). The Jin kingdom besieged Feng and gave it to Wei Zhang Qing. Thus descendants of Wei Zhang Qing also have the last name of Feng. The surname originates from the southeast of Chang'an in Shaanxi Province. Va ...
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Kaifeng
Kaifeng () is a prefecture-level city in east-central Henan province, China. It is one of the Eight Ancient Capitals of China, having been the capital eight times in history, and is best known for having been the Chinese capital during the Northern Song dynasty. As of 31 December 2018, around 4,465,000 people lived in Kaifeng's Prefecture, of whom 1,652,000 lived in the built-up (or metro) area made of Xiangfu, Longting, Shunhe Hui, Gulou and Yuwantai Districts. Located along the Yellow River's southern bank, it borders the provincial capital of Zhengzhou to the west, Xinxiang to the northwest, Shangqiu to the east, Zhoukou to the southeast, Xuchang to the southwest, and Heze of Shandong to the northeast. Kaifeng is also a major city in the world by scientific research outputs as tracked by the Nature Index. The city is home to a campus of Henan University, one of the national key universities in the Double First Class University Plan. Names The postal romanization for the ...
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Tsinghua University
Tsinghua University (; abbreviation, abbr. THU) is a National university, national Public university, public research university in Beijing, China. The university is funded by the Ministry of Education of the People's Republic of China, Ministry of Education. The university is a member of the C9 League, Double First Class University Plan, Project 985, and Project 211. Since its establishment in 1911, it has produced many notable leaders in science, engineering, politics, business, academia, and culture. As of 2022, Tsinghua University ranked 14th in the world by the 2023 QS World University Rankings and 16th globally by the 2022 ''Times Higher Education World University Rankings''. In 2021, Tsinghua ranked first in the Asia-Pacific region by ''Times Higher Education World University Rankings#Asia, THE Asia University Rankings'' and the U.S. News & World Report Best Global Universities Ranking, ''U.S. News & World Report''. History Early 20th century (1911–1949) ...
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Shaanxi
Shaanxi (alternatively Shensi, see #Name, § Name) is a landlocked Provinces of China, province of China. Officially part of Northwest China, it borders the province-level divisions of Shanxi (NE, E), Henan (E), Hubei (SE), Chongqing (S), Sichuan (SW), Gansu (W), Ningxia (NW) and Inner Mongolia (N). Shaanxi covers an area of over with about 37 million people, the 16th highest in China. Xi'an – which includes the sites of the former Capitals of China, Chinese capitals Fenghao and Chang'an – is the Xi'an, provincial capital as well as the largest city in Northwest China and also one of the oldest cities in China and the oldest of the Historical capitals of China, Four Great Ancient Capitals, being the capital for the Western Zhou, Western Han, Sima Jin, Jin, Sui dynasty, Sui and Tang dynasty, Tang List of Chinese dynasties, dynasties. Xianyang, which served as the Qin dynasty capital, is just north across Wei River. The other Prefectures of China, prefecture-level pr ...
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Liaoning
Liaoning () is a coastal province in Northeast China that is the smallest, southernmost, and most populous province in the region. With its capital at Shenyang, it is located on the northern shore of the Yellow Sea, and is the northernmost coastal province of the People's Republic of China. Historically a gateway between China proper and Manchuria, the modern Liaoning province was established in 1907 as Fengtian or Fengtien province and was renamed Liaoning in 1929. It was also known at that time as Mukden Province for the Manchu name of ''Shengjing'', the former name of Shenyang. Under the Japanese-puppet Manchukuo regime, the province reverted to its 1907 name, but the name Liaoning was restored for a brief time in 1945 and then again in 1954. Liaoning borders the Yellow Sea ( Korea Bay) and Bohai Sea in the south, North Korea's North Pyongan and Chagang provinces in the southeast, Jilin to the northeast, Hebei to the southwest, and Inner Mongolia to the northwest. The ...
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Peiyang University
National Peiyang University (北洋大学堂), originally Imperial Tientsin University, was established in Tianjin in October 1895 by Sheng Xuanhuai, the official of the Tianjin Customs, with the approval of the Guangxu Emperor of Qing dynasty. It was the first government-run university in modern China where western science & technology was its main focus. The school motto was "Seeking truth from facts"(实事求是). In 1951, by Chinese government's order, the university was renamed as Tianjin University. In 1912, it was renamed National Peiyang University, and the following year it was renamed National Peiyang University. In 1917, Peiyang University merged into Peking University. By 1920, Peiyang University began to specialize in engineering education. In 1928, the National Government promoted the university district system. During this period, the school was renamed as the Second Institute of Engineering at National Peiping University. The following year the university dist ...
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Renhua County
Renhua ( postal: Yanfa; ) is a county of northernmost Guangdong province, China, bordering Jiangxi to the northeast and Hunan to the northwest. It is under the administration of Shaoguan City. History Renhua County has a long history, as it was established in AD 479, dating back more than 1500 years. Renhua GovernmenOfficial County PortalAccessed Nov.11.2015. * In 1949, Renhua County was liberated, as Beijiang zone of Guangdong, and established People's Government of Renhua County (Renhua Ren Min Zheng Fu). * In 1956, it belonged to Shaoguan zone of Guangdong. * In 1968, it withdraws people's committee and established revolutionary committee, which belongs to revolutionary committee of Shaoguan District.Shaoguan InformatioGuangdong Government InformationAccessed Nov.11.2015. * In 1980, People's Government of Renhua County was restored and belongs to Shaoguan District. * In 1983, Shaoguan City was established and Shaoguan District merged with it, and Renhua County is belonging to it, ...
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Mount Danxia
Mount Danxia () is a noted scenic mountainous area in Renhua County, in the northern part of Guangdong province. It is described on the local signage as a "world famous UNESCO geopark of China". It was inscribed as part of the China Danxia World Heritage Site in 2010 because of its unique geographical in formations and spectacular scenery. Description The Danxia area is formed from a reddish sandstone which has been eroded over time into a series of outcrops surrounded by spectacular cliffs and many unusual rock formations known as Danxia landform. There are a number of temples located on the mountains and many scenic walks can be undertaken. There is also a river winding through the mountains on which boat trips can be taken. Rock formations Among other attractions that make the Danxia range interesting, the area has the following characteristic stone formations: *Yang Yuan Stone, (' "male/father stone") bearing a remarkable resemblance to a phallus *Yin Yuan Stone or ' hole ...
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Danxia Landform
The Danxia landform () refers to various landscapes found in southeast, southwest and northwest China that "consist of a red bed characterized by steep cliffs". It is a unique type of petrographic geomorphology found in China. Danxia landform is formed from red-coloured sandstones and conglomerates of largely Cretaceous age. The landforms look very much like karst topography that forms in areas underlain by limestones, but since the rocks that form danxia are sandstones and conglomerates, they have been called "pseudo-karst" landforms. They were formed by endogenous forces (including uplift) and exogenous forces (including weathering and erosion). The first studies on what are now referred to as Danxia landforms were conducted at Mount Danxia near Shaoguan, China. In the 1920s and 1930s Chinese geologists made an effort to learn more about these interesting geomorphic structures. Danxia landforms are made up of uplifted continental crust that has been faulted and eroded, exposing ...
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Changping District
Changping District (), formerly Changping County (), is a district situated in the suburbs of north and northwest Beijing. History Changping County and Jundu County which administered the area were established in the Han Dynasty. Changping was incorporated into Jundu when the Northern Wei dominated; however, the condition was reversed since the Eastern Wei. The county was promoted as Changping subprefecture had jurisdiction over Miyun, Shunyi and Huairou, in the era of Zhengde during the Ming Dynasty. These three counties were transferred to Shuntian Prefecture in the era of Yongzheng during the Qing Dynasty. Changping became a county again after the Xinhai Revolution, and it was transferred to Beijing from Hebei in 1956. Geography Changping District, covering an area of , contains two subdistricts of the city of Changping and 15 towns (five of which are suburbs of Beijing) with total population of 1.83 million (2012), a rapid increase from the 614,821 recorded in the 2000 c ...
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Yellow River
The Yellow River or Huang He (Chinese: , Standard Beijing Mandarin, Mandarin: ''Huáng hé'' ) is the second-longest river in China, after the Yangtze River, and the List of rivers by length, sixth-longest river system in the world at the estimated length of . Originating in the Bayan Har Mountains in Qinghai province of Western China, it flows through nine provinces, and it empties into the Bohai Sea near the city of Dongying in Shandong province. The Yellow River basin has an east–west extent of about and a north–south extent of about . Its total drainage area is about . The Yellow River's basin was the Yellow River civilization, birthplace of ancient Chinese, and, by extension, Far East, Far Eastern civilization, and it was the most prosperous region in early Chinese history. There are frequent devastating natural disasters in China, floods and course changes produced by the continual elevation of the river bed, sometimes above the level of its surrounding farm fi ...
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Dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented sa ...
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