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Historic Eruptions Of Mount Fuji
Mount Fuji is the tallest volcano in Japan, and also the highest peak. The latest eruption of Mount Fuji was in 1707, and it was triggered by an earthquake. The mountain as it appears now is the "New Fuji volcano", which began to erupt about 10,000 years ago. Under the "New Fuji volcano" lies the "Old Fuji volcano", which was active between 100,000 years ago and 10,000 years ago, and the "Komitake volcano", which became active 700,000 years ago. Prehistory Komitake and Old Fuji There has been volcanic activity in the vicinity of Mount Fuji for several million years. The earliest geologically known volcano was that became active 700,000 years ago. Another volcano to the south-east of Mount Fuji—known as —was also highly active throughout the period. The peak of Komitake is about above sea-level on the north face of Mount Fuji (at the fifth station). Komitake entered another period of activity around 100,000 years ago. This created a new volcano known as that r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aokigahara
Aokigahara (), also known as the , is a forest on the northwestern flank of Mount Fuji on the island of Honshu in Japan, thriving on of hardened lava laid down by the last major eruption of Mount Fuji in 864 CE. The western edge of Aokigahara, where there are several caves that fill with ice in winter, is a popular destination for tourists and school trips. Parts of Aokigahara are very dense, and the porous lava rock absorbs sound, contributing to a sense of solitude that some visitors attribute to the forest. The forest has a historical reputation as a home to '' yūrei'': ghosts of the dead in Japanese mythology. At least since the 1960s, Aokigahara has become associated with suicide, eventually becoming known in English by the nickname "Suicide Forest" and gaining a reputation as one of the world's most-used suicide sites. Because of this, signs at the head of some trails urge suicidal visitors to think of their families and contact a suicide prevention association. Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hayashi Gahō
, also known as Hayashi Shunsai, 林 春斎, , was a Japanese Neo-Confucian philosopher and writer in the system of higher education maintained by the Tokugawa ''bakufu'' during the Edo period. He was a member of the Hayashi clan of Confucian scholars. Following in the footsteps of his father, Hayashi Razan, Gahō (formerly Harukatsu) would devote a lifetime to expressing and disseminating the official neo-Confucian doctrine of the Tokugawa shogunate. Like his distinguished father, Gahō's teaching and scholarly written work emphasized Neo-Confucianist virtues and order. Academician Gahō became the unofficial rector of what would become Edo’s Confucian Academy, the Shōhei-kō (afterwards known as the Yushima Seidō).Nussbaum, Louis Frédéric ''et al.''. (2005). ''Japan Encyclopedia,'' p. 300. This institution stood at the apex of the country-wide educational and training system which was created and maintained by the Tokugawa shogunate. Gahō's hereditary title wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Japan
This is a list of active and extinct volcanoes in Japan. An Orange background indicates a volcano considered active by the Japan Meteorological Agency. Hokkaido Honshū Izu Islands Ogasawara Archipelago The Ogasawara Archipelago include the Bonin Islands and Volcano Islands. Kyūshū Ryūkyū Islands See also * Notes and references Notes References External links Quaternary Volcanoes of Japan- Geological Survey of Japan - Geological Survey of Japan * ttp://www.data.jma.go.jp/svd/vois/data/tokyo/STOCK/souran_eng/souran.htm The National Catalogue of the Active Volcanoes in Japan- Japan Meteorological Agency 日本の主な山岳標高 (Elevation of Principal Mountains in Japan)- Geospatial Information Authority of Japan {{Asia topic, List of volcanoes in Japan Lists of coordinates Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heian Era
The is the last division of classical Japanese history, running from 794 to 1185. It followed the Nara period, beginning when the 50th emperor, Emperor Kanmu, moved the capital of Japan to Heian-kyō (modern Kyoto). 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, a cursive alphabet with a unique writing method 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 aristocrat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Musashi Province
was a province of Japan, which today comprises Tokyo Metropolis, most of Saitama Prefecture and part of Kanagawa Prefecture. It was sometimes called . The province encompassed Kawasaki and Yokohama. Musashi bordered on Kai, Kōzuke, Sagami, Shimōsa, and Shimotsuke Provinces. Musashi was the largest province in the Kantō region. History Musashi had its ancient capital in modern Fuchū, Tokyo, and its provincial temple in what is now Kokubunji, Tokyo. By the Sengoku period, the main city was Edo, which became the dominant city of eastern Japan. Edo Castle was the headquarters of Tokugawa Ieyasu before the Battle of Sekigahara and became the dominant city of Japan during the Edo period, being renamed Tokyo during the Meiji Restoration. ''Hikawa-jinja'' was designated as the chief Shinto shrine (''ichinomiya'') of the province; and there are many branch shrines. The former province gave its name to the battleship of the Second World War. Timeline of important even ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sagami Province
was a province of Japan located in what is today the central and western Kanagawa Prefecture. Nussbaum, Louis-Frédéric. (2005). "''Kanagawa''" at . Sagami Province bordered the provinces of Izu, Musashi, and Suruga. It had access to the Pacific Ocean through Sagami Bay. However, most of the present-day cities of Yokohama and Kawasaki, now part of Kanagawa Prefecture, were not in Sagami, but rather, in Musashi Province. Its abbreviated form name was . History Sagami was one of the original provinces of Japan established in the Nara period under the Taihō Code. The area has been inhabited since prehistoric times. Although remnants from the Japanese Paleolithic and Yayoi periods are scarce, remains from the Jōmon period are relatively plentiful. Kofun period remains are generally from the 1st – 4th centuries AD. Whether or not Sagami was originally part of Musashi prior to the Nara period is still a topic of controversy. The original capital of the province may have be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Izu Province
was a province of Japan in the area of Shizuoka Prefecture. Nussbaum, Louis-Frédéric. (2005). "''Izu''" in . Izu bordered on Sagami and Suruga Provinces. Its abbreviated form name was . The mainland portion of Izu Province, comprising the Izu Peninsula, is today the eastern portion of Shizuoka Prefecture and the Izu Islands are now part of Tokyo. History In 680 A.D., two districts of Suruga Province, Tagata District and Kamo District, were separated into the new Izu Province. At some point between the year 701 and 710, Naka District was added. The capital of the new province was established at Mishima, which also had the ''Kokubun-ji'' and the Ichinomiya (Mishima Taisha) of the province. Under the '' Engishiki'' classification system, Izu was ranked as a "lesser country" (下国). Under the ''ritsuryō'' legal system, Izu was one of the preferred locations for exile for those convicted of political crimes by the Heian period court. In the Kamakura period, Izu was rul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1703 Genroku Earthquake
The occurred at 02:00 local time on December 31 (17:00 December 30 UTC). The epicenter was near Edo, the forerunner of present-day Tokyo, in the southern part of the Kantō region, Japan. An estimated 2,300 people were killed by the shaking and subsequent fires. The earthquake triggered a major tsunami which caused many additional casualties, giving a total death toll of at least 5,233, possibly up to 10,000. Genroku is a Japanese era spanning from 1688 through 1704. Tectonic setting The Kantō Region lies at the complex triple junction, where the convergent boundaries between the subducting Pacific and Philippine Sea Plates and the overriding North American and Eurasian Plates meet. Earthquakes with epicenters in the Kanto region may occur within the Eurasian Plate, at the Eurasian Plate/Philippine Sea Plate interface, within the Philippine Sea Plate, at the Philippine Sea Plate/Pacific Plate interface or within the Pacific Plate. In addition to this set of major plates it h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1707 Hōei Earthquake
The struck south-central Japan at 14:00 local time on 28 October. It was the largest earthquake in Japanese history until it was surpassed by the 2011 Tōhoku earthquake. It caused moderate to severe damage throughout southwestern Honshu, Shikoku and southeastern Kyūshū. The earthquake, and the resulting destructive tsunami, caused more than 5,000 casualties. This event ruptured all of the segments of the Nankai megathrust simultaneously, the only earthquake known to have done this, with an estimated magnitude of 8.6 or 8.7 . It possibly also triggered the last eruption of Mount Fuji 49 days later. Hōei (宝永) was the era spanning the years from March 1704 through April 1711. Tectonic setting The southern coast of Honshu runs parallel to the Nankai Trough, which marks the subduction of the Philippine Sea Plate beneath the Eurasian Plate. Movement on this convergent plate boundary leads to many earthquakes, some of them of megathrust type. The Nankai megathrust has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
