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Concept
Heian period
Summary
The Heian period is the last division of classical Japanese history, running from 794 to 1185. It followed the Nara period, beginning when the 50th emperor, Emperor Kammu, moved the capital of Japan to Heian-kyō (modern Kyoto). 平安 means "peace" in Japanese. It is a period in Japanese history when the Chinese influences were in decline and the national culture matured. The Heian period is also considered the peak of the Japanese imperial court and noted for its art, especially poetry and literature. Two types of Japanese script emerged, including katakana, a phonetic script which was abbreviated into hiragana, both unique alphabets distinctive to Japan. This gave rise to Japan's famous vernacular literature, with many of its texts written by court women who were not as educated in Chinese compared to their male counterparts.
Although the Imperial House of Japan had power on the surface, the real power was in the hands of the Fujiwara clan, a powerful aristocratic family who had intermarried with the imperial family. Many emperors had mothers from the Fujiwara family. The economy mostly existed through barter and trade, while the shōen system enabled the accumulation of wealth by an aristocratic elite. Even though the Heian period was one of national peace, the government failed to effectively police the territory, leading to frequent robberies of travellers.
The Heian period was preceded by the Nara period and began in 794 AD after the movement of the capital of Japan to Heian-kyō (modern Kyoto), by the 50th emperor, Emperor Kammu. Kammu first tried to move the capital to Nagaoka-kyō, but a series of disasters befell the city, prompting the emperor to relocate the capital a second time, to Heian. A rebellion occurred in China in the last years of the 9th century, making the political situation unstable. The Japanese missions to Tang China were suspended and the influx of Chinese exports halted, a fact which facilitated the independent growth of Japanese culture called kokufu bunka.
Official source
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