Kinko Bay
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Kinko 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 island 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 bay and the Kiris ...
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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 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". 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 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 of tephra has been and of lava. There is a sea scarp which is 7.8km wide and 9.3km long, the shape is similar to ...
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Jesuits
The Society of Jesus ( la, Societas Iesu; abbreviation: SJ), also known as the Jesuits (; la, Iesuitæ), 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 is engaged in evangelization and apostolic ministry in 112 nations. Jesuits work in education, research, and cultural pursuits. Jesuits also give retreats, minister in hospitals and parishes, sponsor direct social and humanitarian ministries, 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 the Society of Jesus, Superior General. The headquarters of the society, its Curia, General Curia, is in Rome. The historic curia of Ignatius is now part of the attached to t ...
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Francis Xavier
Francis Xavier (born Francisco de Jasso y Azpilicueta; Latin: ''Franciscus Xaverius''; Basque: ''Frantzisko Xabierkoa''; French: ''François Xavier''; Spanish: ''Francisco Javier''; Portuguese: ''Francisco Xavier''; 7 April 15063 December 1552), venerated as Saint Francis Xavier, was a Spanish Catholic missionary and saint who was a co-founder of the Society of Jesus. Born in Javier (Xavier in Old Spanish and in Navarro-Aragonese, or Xabier, a Basque word meaning "new house"), in the Kingdom of Navarre (in present-day Spain), 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 evangelisation 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 ...
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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 * Notes References * Nussbaum, Louis-Frédéric and Käthe Roth. (2005) ''Japan encyclopedia.''Cambridge: Harvard University Press Harvard University Press (HUP) is a publishing house established on January 13, 1913, as a division of Harvard University, a ...
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Hayato People
The , which is Japanese for "falcon-people", were a people of ancient Japan who lived in the Satsuma and Ōsumi regions of southern Kyushu during the Nara period. They frequently resisted Yamato rule. After their subjugation they became subjects of the government under Ritsuryō, and the 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 early as Emperor Nintoku's reign. This, along with a mention of Hayato crying before the grave of ...
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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. Origins 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. Overview William George Aston, in his translation of ...
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Jōmon Period
The is the time in Japanese history, traditionally dated between   6,000–300 BCE, during which Japan was inhabited by a diverse hunter-gatherer and early agriculturalist population united through a common Jōmon 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 sherds of pottery in 1877 and subsequently translated it into 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; pottery figurines and vessels; and lacquerware.Imamura, K. (1996) ''Prehistoric Japan: New Perspectives on Insular East Asia''. Honolulu: University of Hawaii Press It is often compared to pre-C ...
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Tsunami
A tsunami ( ; from ja, 津波, lit=harbour wave, ) 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 other 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 ...
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Before Present
Before Present (BP) years, or "years before present", 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 1 January 1950 as the commencement date (epoch) of the age scale. 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 now account for. 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 sometimes used for dates established by means other than radiocarbon dating, such as stratigraphy. This usage differs from t ...
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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 felling dates for some construction timbers from neolithic wells in Central Europe. This millennium is reckoned to mark the end of the 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. Communities 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 north and western Europe, people still lived in scattered Palaeolithic hunter-gatherer communities. The world ...
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