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Youtiao (traditional Chinese: 油條; simplified Chinese: 油条; pinyin: Yóutiáo), known in Southern China as yu char kway, is a long golden-brown deep-fried strip of wheat flour dough of Chinese origin and (by a variety of other names) also popular in other East and Southeast Asian cuisines.
Cifantuan, also known simply as chi faan or fantuan, is a glutinous rice dish in Chinese cuisine originating in the Jiangnan area of eastern China which encompasses Shanghai and surrounding regions.
The Chinese Daoists that he recruited used "alchemical" methods to make both soy milk and bean curd, perhaps as a medicine for eternal life. As the only powerful noble at that time, Liu An could order the (relative) mass-production of such items and spread them around, thus making him famous for soy milk and bean curd. [ 7 ]
A meal of bak kut teh served with youtiao.. Bak kut teh is commonly consumed in both Malaysia and Singapore. [3] The origin of bak kut teh is unclear, but it is believed to have been brought over from Fujian, China [4] [1] [2] said to be based on a Quanzhou dish of beef ribs stewed with herbs known as niu pai ("beef steak").
Ting Yao-tiao was born on December 21, 1927, as the fourth of ten children. After graduating from National Tainan Girls' Senior High School in 1945, she started working at the post office. [1] [2] In 1951, when Kuo Chen-chun (Chinese: 郭振純; pinyin: Guō Zhènchún) helped Yeh Ting-kuei to run for the mayor of Tainan, he met Ting. The two ...
Doujiang (traditional Chinese: 豆漿; simplified Chinese: 豆浆; pinyin: dòujiāng) is fresh soy milk in Chinese cuisine.It can be served hot or cool, sweet or savoury. [1]
In the myths and folk religion of Chinese culture, the Jade Emperor or Yudi [1] is one of the representations of the primordial god.. In Taoist theology, he is the assistant of Yuanshi Tianzun, who is one of the Three Pure Ones, the three primordial emanations of the Tao.
The earliest evidence for life on Earth includes: 3.8 billion-year-old biogenic hematite in a banded iron formation of the Nuvvuagittuq Greenstone Belt in Canada; [30] graphite in 3.7 billion-year-old metasedimentary rocks in western Greenland; [31] and microbial mat fossils in 3.48 billion-year-old sandstone in Western Australia.