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Kagoshima Bay
also known as Kinkō Bay, is a deep inlet of the East China Sea on the coast of Japan.''Merriam Webster's Geographical Dictionary, Third Edition'', p. 562. Kagoshima Bay is on the south coast of the island of Kyūshū. The port city of Kagoshima and its well-protected harbor lie on the bay's western coast, just opposite the former island (now peninsula) of Sakurajima. Geology The bay itself is partially volcanic in origin, with two massive submarine calderas shaping part of the bay's shoreline: The younger Aira Caldera in the northernmost part of the bay, and the older Ata Caldera at the mouth of the bay where it meets the East China Sea. Both calderas formed during the Pleistocene from highly explosive Ultra-Plinian volcanic eruptions, Aira approximately 22,000 years ago and Ata approximately 105,000 years ago. Though such enormous eruptions are extremely infrequent, both volcanoes have remained active with much smaller eruptions in historic times, with Sakurajima in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kaimon
, or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small complex central lava dome – which rises to a height of 924 metres above sea level near the city of Ibusuki, Kagoshima, Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as "the Fuji of Satsuma Province, Satsuma". It is one of the 100 Famous Japanese Mountains. Geography Mt. Kaimon is located in the south of Kagoshima prefecture, Kyushu and is an important reference point for marine traffic because it is the southernmost prominence of the Satsuma Peninsula. This is one entrance marker to Kinko Bay (Kagoshima Bay) complimentary to the Ōsumi Peninsula. Together with Bōnoma Prefectural Natural Park, Mt. Noma and Mt. Kinpo, it is used by marine traffic. Geology Part of the Ibusuki volcanic field, Mt. Kaimon defines the eastern margin of the old Ata Caldera. The total eruptive volume ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jesuits
The Society of Jesus (; abbreviation: S.J. or SJ), also known as the Jesuit Order or the Jesuits ( ; ), is a religious order (Catholic), religious order of clerics regular of pontifical right for men in the Catholic Church headquartered in Rome. It was founded in 1540 by Ignatius of Loyola and six companions, with the approval of Pope Paul III. The Society of Jesus is the largest religious order in the Catholic Church and has played significant role in education, charity, humanitarian acts and global policies. The Society of Jesus is engaged in evangelization and apostolic ministry in 112 countries. Jesuits work in education, research, and cultural pursuits. They also conduct retreats, minister in hospitals and parishes, sponsor direct social and humanitarian works, and promote Ecumenism, ecumenical dialogue. The Society of Jesus is consecrated under the patron saint, patronage of Madonna della Strada, a title of the Blessed Virgin Mary, and it is led by a Superior General of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Francis Xavier
Francis Xavier, Jesuits, SJ (born Francisco de Jasso y Azpilicueta; ; ; ; ; ; 7 April 15063 December 1552), venerated as Saint Francis Xavier, was a Kingdom of Navarre, Navarrese cleric and missionary. He co-founded the Society of Jesus and, as a representative of the Portuguese Empire, led the first Christian mission to Japan. Born in the town of Xavier, Spain, Xavier, Kingdom of Navarre, he was a companion of Ignatius of Loyola and one of the first seven Jesuits who took vows of poverty and chastity at Montmartre, Paris in 1534. He led an extensive mission into Asia, mainly the Portuguese Empire in the East, and was influential in evangelization work, most notably in early modern India. He was extensively involved in the missionary activity in Portuguese India. In 1546, Francis Xavier proposed the establishment of the Goan Inquisition in a letter addressed to King John III of Portugal. While some sources claim that he actually asked for a special minister whose sole of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kinai
is a Japanese term denoting an ancient division of the country. ''Kinai'' is a name for the ancient provinces around the capital Nara and Heian-kyō. Nussbaum, Louis-Frédéric. (2005). "''Kinai''" in . The five provinces were called ''go-kinai'' after 1760.Nussbaum, "''Gokishichidō''" in . The name is still used to describe part of the Kansai region, but the area of the Kinai corresponds only generally to the land of the old provinces. The region was established as one of the ''Gokishichidō'' ("Five provinces and seven roads") during the Asuka period (538-710). It consisted of Yamashiro, Yamato, Settsu, Kawachi, and Izumi provinces. See also * Comparison of past and present administrative divisions of Japan * References * Nussbaum, Louis-Frédéric and Käthe Roth. (2005) ''Japan encyclopedia.''Cambridge: Harvard University Press Harvard University Press (HUP) is an academic publishing house established on January 13, 1913, as a division of Harvard Universi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hayato Rebellion
The (720–721) was a rebellion of the Hayato of southern Kyushu against the imperial dynasty of Japan during the Nara period. After a year and a half of fighting, the Hayato were defeated, and the Imperial court established its rule over southern Kyushu. Background In the latter half of the 7th century, the imperial court's influence extended to southern Kyushu, but the scattered Kumaso and Hayato populations held their ground. The court was attempting to introduce its own Ritsuryō system throughout its sphere of influence, but the populations of southern Kyushu resisted. This was because Ritsuryō was based on rice cultivation, to which the volcanic soil of southern Kyushu was unsuited. On the other hand, the court was also expanding its intercourse with mainland China through the Ryukyu Islands. It organized an investigative expedition called the to survey southern Kyushu and the Ryukyu Islands, but in 700 the ''bekkokushi'' were threatened by the local inhabitants in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hayato People
The , which is Japanese for "falcon-people", were a people of ancient Japan who lived in the Satsuma province, Satsuma and Ōsumi Province, Ōsumi regions of southern Kyushu during the Nara period. They frequently resisted Imperial House of Japan, Yamato rule. After their subjugation they became subjects of the government under Ritsuryō, and the Ministry of War (pre-modern Japan), Ministry of the Military had an office known as the in charge of their governance. The name also came into use by samurai as a title, . In modern times, Hayato is a Japanese male given name. History and culture The Hayato might have been the same as the Kumaso group of around the same time, but while the Kumaso are mentioned in the more legendary portions of the Nihon Shoki, the Hayato are recorded in various historical texts until the beginning of the Heian period. Though the Kumaso are generally portrayed as rebellious, the Hayato are listed among the attendants of emperors and princes from as earl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kumaso
The were a mythical people of ancient Japan mentioned in the ''Kojiki'', believed to have lived in the south of Kyūshū until at least the Nara period. The last leader of the Kumaso, Torishi-Kaya was killed by Yamato Takeru in 397. The name of Kumamoto Prefecture originates from the Kumaso people. Hypothesized Origin Scholars, such as Kakubayashi Fumio, "although information is extremely limited" concluded that they were of Austronesian origin based on some linguistic and cultural evidence, theorising that the word ''kaya'', present in personal names or titles, such as Torishi-Kaya, has the same root as Tagalog ''" kaya"'', meaning "ability; capability; competence; resources; wealth" and Malay and Indonesian ''" kaya"'', meaning "rich, wealthy, having wealth". The ''So'' present in Kumaso was also theorised to have the same origins as ''tsuo, tsau, thau, sau, tau, tao'' supposedly meaning "people" in Austronesian languages. Alexander Vovin defended that the question of wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jōmon Period
In Japanese history, the is the time between , during which Japan was inhabited by the Jōmon people, a diverse hunter-gatherer and early agriculturalist population united by a common culture, which reached a considerable degree of sedentism and cultural complexity. The name "cord-marked" was first applied by the American zoologist and orientalist Edward S. Morse, who discovered Glossary of archaeology#potsherd, sherds of pottery in 1877 and subsequently translated "straw-rope pattern" into Japanese language, Japanese as ''Jōmon''.Mason, 14 The pottery style characteristic of the first phases of Jōmon culture was decorated by impressing cords into the surface of wet clay and is generally accepted to be among the oldest in the world. The Jōmon period was rich in tools and jewelry made from bone, stone, shell and antler; Jōmon pottery, pottery figurines and vessels; and lacquerware.Imamura, K. (1996) ''Prehistoric Japan: New Perspectives on Insular East Asia''. Honolulu: Unive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tsunami
A tsunami ( ; from , ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event. Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide. For this reason, it is often referred to as a tidal wave, although this usage is not favoured by the scientific community because it might give the false impression of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Before Present
Before Present (BP) or "years before present (YBP)" is a time scale used mainly in archaeology, geology, and other scientific disciplines to specify when events occurred relative to the origin of practical radiocarbon dating in the 1950s. Because the "present" time changes, standard practice is to use 1January 1950 as the commencement date (epoch) of the age scale, with 1950 being labelled as the "standard year". The abbreviation "BP" has been interpreted retrospectively as "Before Physics", which refers to the time before nuclear weapons testing artificially altered the proportion of the carbon isotopes in the atmosphere, which scientists must account for when using radiocarbon dating for dates of origin that may fall after this year. In a convention that is not always observed, many sources restrict the use of BP dates to those produced with radiocarbon dating; the alternative notation "RCYBP" stands for the explicit "radio carbon years before present". Usage The BP scale is s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
6th Millennium BC
The 6th millennium BC spanned the years 6000 BC to 5001 BC (c. 8 ka to c. 7 ka). It is impossible to precisely date events that happened around the time of this millennium and all dates mentioned here are estimates mostly based on geological and anthropological analysis. The only exceptions are the Dendrochronology, felling dates for some construction timbers from Neolithic Europe, Neolithic Well#History, wells in Central Europe. This millennium is reckoned to mark the end of the Early Holocene sea level rise, global deglaciation, which had followed the Last Glacial Maximum and caused sea levels to rise by some over a period of about 5,000 years. Overview Neolithic culture and technology had spread from the Near East and into Eastern Europe by 6000 BC. Its development in the Far East grew apace and there is increasing evidence through the millennium of its presence in prehistoric Egypt and the Far East. In much of the world, however, including Northern and Western ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
