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Mount Hiyori
located in Sendai, Miyagi Prefecture, is Japan's lowest mountain. From 1991 to 1996, 2014年05月20日 Kahoku Shimpō, 河北新報 and again on April 9, 2014, after the Tohoku tsunami, the Geospatial Information Authority of Japan recognized it as "the lowest mountain in Japan". Overview 
The mountain is located on the northeastern edge of Sendai City, facing the Pacific Ocean and Sendai, north of the mouth of the Nanakita River, and west of Gamo Mud ...
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Sendai
is the capital Cities of Japan, city of Miyagi Prefecture and the largest city in the Tōhoku region. , the city had a population of 1,098,335 in 539,698 households, making it the List of cities in Japan, twelfth most populated city in Japan. The modern city was founded in 1600 by the ''daimyō'' Date Masamune. It is nicknamed the ; there are Japanese zelkova trees lining many of the main thoroughfares such as and . In the summer, the Sendai Tanabata Festival, the largest Tanabata festival in Japan, is held. In winter, the trees are decorated with thousands of lights for the , lasting through most of December. The city is also home to Tohoku University, one of the former Imperial Universities. On 11 March 2011, coastal areas of the city suffered catastrophic damage from a 2011 Tōhoku earthquake and tsunami, magnitude 9.0 offshore earthquake,] which triggered a destructive tsunami. History Edo period Although the Sendai area was inhabited as early as 20,000 years ago, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunchū
Bunchū (文中) was a Japanese era name (年号, ''nengō'', lit. year name) of the Southern Court during the Era of Northern and Southern Courts after Kentoku and before Tenju. This period spanned the years from October 1372 to May 1375. The Southern Court emperor in Yoshino during this timeframe was . The Northern court emperor in Kyoto was . Nanboku-chō overview During the Meiji period, an Imperial decree dated March 3, 1911, established that the legitimate reigning monarchs of this period were the direct descendants of Emperor Go-Daigo through Emperor Go-Murakami, whose had been established in exile in Yoshino, near Nara.Thomas, Julia Adeney. (2001) ''Reconfiguring modernity: concepts of nature in Japanese political ideology'', p. 199 n57 citing Mehl, Margaret. (1997). ''History and the State in Nineteenth-Century Japan.'' p. 140-147. Until the end of the Edo period, the militarily superior pretender-Emperors supported by the Ashikaga shogunate had been mist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yomiuri Shimbun
The is a Japanese newspaper published in Tokyo, Osaka, Fukuoka, Fukuoka, Fukuoka, and other major Japanese cities. It is one of the five major newspapers in Japan; the other four are ''The Asahi Shimbun'', the ''Chunichi Shimbun'', the ''Mainichi Shimbun'', and the ''The Nikkei, Nihon Keizai Shimbun''. It is headquartered in Ōtemachi, Otemachi, Chiyoda, Tokyo.'' It is a newspaper that represents Tokyo and generally has a Conservatism, conservative orientation. It is one of Japan's leading newspapers, along with the Osaka-based Liberalism, liberal (Third Way) ''Asahi Shimbun'' and the Nagoya-based Social democracy, social democratic ''Chunichi Shimbun''. This newspaper is well known for its pro-American stance among major Japanese media. It is published by regional bureaus, all of them subsidiaries of #Yomiuri Group, The Yomiuri Shimbun Holdings, Japan's largest media conglomerate by revenue and the second largest media conglomerate by size behind Sony,The Yomiuri Shimbun H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2011 Tōhoku Earthquake And Tsunami
On 11 March 2011, at 14:46:24 Japan Standard Time, JST (05:46:24 UTC), a 9.0–9.1 Submarine earthquake, undersea megathrust earthquake occurred in the Pacific Ocean, east of the Oshika Peninsula of the Tōhoku region. It lasted approximately six minutes and caused a tsunami. It is sometimes known in Japan as the , among other names. The disaster is often referred to by its numerical date, 3.11 (read in Japanese). It was the List of earthquakes in Japan, most powerful earthquake ever recorded in Japan, and the Largest earthquakes by magnitude#Strongest earthquakes by magnitude, fourth most powerful earthquake recorded in the world since modern seismography began in 1900. The earthquake triggered powerful tsunami waves that may have reached heights of up to in Miyako, Iwate, Miyako in Tōhoku's Iwate Prefecture,Yomiuri Shimbun evening edition 2-11-04-15 page 15, nearby Aneyoshi fishery port (姉吉漁港)(Google map E39 31 57.8, N 142 3 7.6) 2011-04-15大震災の津 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heisei
The was the period of Japanese history corresponding to the reign of Emperor Akihito from 8 January 1989 until his abdication on 30 April 2019. The Heisei era started on 8 January 1989, the day after the death of the Emperor Hirohito, when his son, Akihito, acceded to the throne as the 125th Emperor. In accordance with Japanese customs, Hirohito was posthumously renamed "Emperor Shōwa" on 31 January 1989. Thus, 1989 corresponds to Shōwa 64 up until 7 January and from 8 January. The Heisei era ended on 30 April 2019 (Heisei 31), with the abdication of Akihito from the Chrysanthemum Throne. It was succeeded by the Reiwa era as then-crown prince Naruhito ascended the throne on 1 May midnight local time. History and meaning Shortly after the death of Emperor Hirohito on 7 January 1989, Keizō Obuchi, then- Chief Cabinet Secretary and later Prime Minister of Japan, hosted a press conference to announce the new era name "Heisei" for Emperor Akihito, and explained its m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tenpō
located in Minato-ku, Osaka is currently Japan's second lowest mountain. (The lowest mountain title is now held by Mount Hiyori in Sendai, Miyagi Prefecture - like Mount Tenpo, Hiyori is a man-made structure, and gained its title as the shortest mountain following subsidence after the 2011 Tōhoku earthquake and tsunami.) The definition of a "mountain" used here is any elevation described as a mountain on a topographic map published by the Geographical Survey Institute of Japan, though it is disputed that the mountain lacks credibility because it is not a natural part of the landscape. The mountain's peak is 4.53 meters above sea level, and will bear more resemblance to a hill than a mountain to the casual observer. A small port is located nearby, and much of the mountain's surface has been converted into a park. History Mount Tenpō was formed in 1831 ( Tenpō year 2) as the deposit for earth dug up from dredging the Ajigawa river to allow easier access to Osaka for large shi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ōan
, also romanized as Ō-an, was a Japanese era name (年号, ''nengō'', lit. year name) of the Northern Court during the Era of Northern and Southern Courts after '' Jōji'' and before '' Eiwa.'' This period spanned the years from February 1368 through February 1375. The emperors in Kyoto were and Titsingh, Isaac. (1834)''Annales des empereurs du japon'', pp. 310-312./ref> The Southern Court rival in Yoshino during this time-frame was . Nanboku-chō overview During the Meiji period, an Imperial decree dated March 3, 1911 established that the legitimate reigning monarchs of this period were the direct descendants of Emperor Go-Daigo through Emperor Go-Murakami, whose had been established in exile in Yoshino, near Nara.Thomas, Julia Adeney. (2001) ''Reconfiguring modernity: concepts of nature in Japanese political ideology'', p. 199 n57 citing Mehl, Margaret. (1997). ''History and the State in Nineteenth-Century Japan.'' p. 140-147. Until the end of the Edo period, the milit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Court
The , also known as the Ashikaga Pretenders or Northern Pretenders, were a set of six pretenders to the throne of Japan during the Nanboku-chō period from 1336 through 1392. Even though the present Imperial House of Japan is descended from the Northern Court emperors, The Southern Court is considered the legitimate line, with the argument being that it was the Southern court which possessed the Imperial Regalia, which was later handed over to the Northern court, thus making Emperor Go-Komatsu the 100th Emperor of Japan. It was in 1911 that Emperor Meiji passed an edict which made the Southern line the legitimate one. Earlier, it was thought by pre Meiji scholars that It was the Northern line which was the legitimate line. The Northern dynasty is also referred to as the "senior line" or the ; Jimyō-in was a temple and retirement residence of this line's emperors Go-Fukakusa and Fushimi. Nanboku-chō overview The origins of the Northern Court go back to Emperor Go-Sag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Court
The were a set of four emperors ( Emperor Go-Daigo and his line) whose claims to sovereignty during the Nanboku-chō period spanning from 1336 through 1392 were usurped by the Northern Court. This period ended with the Southern Court definitively losing the war, and they were forced to completely submit sovereignty to the Northern Court. This had the result that, while later Japanese sovereigns were descended from the Northern Court, posterity assigns sole legitimacy during this period to the Southern Court. The Southern descendants are also known as the "junior line" and the , Daikaku-ji being the cloistered home of Go-Uda, a Southern ruler. Because it was based in Yoshino, Nara, it is also called the . Nanboku-chō overview The genesis of the Northern Court go back to Emperor Go-Saga, who reigned from 1242 through 1246. Go-Saga was succeeded by two of his sons, Emperor Go-Fukakusa and Emperor Kameyama, who took turns on the throne. This was because on his death bed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miyagi Prefecture
is a Prefectures of Japan, prefecture of Japan located in the Tōhoku region of Honshu. Miyagi Prefecture has a population of 2,265,724 (1 August 2023) and has a geographic area of . Miyagi Prefecture borders Iwate Prefecture to the north, Akita Prefecture to the northwest, Yamagata Prefecture to the west, and Fukushima Prefecture to the south. Sendai is the capital and largest city of Miyagi Prefecture, and the largest city in the Tōhoku region, with other major cities including Ishinomaki, Ōsaki, Miyagi, Ōsaki, and Tome, Miyagi, Tome. Miyagi Prefecture is located on Japan's eastern Pacific coast and bounded to the west by the Ōu Mountains, the longest mountain range in Japan, with 24% of its total land area being designated as List of national parks of Japan, Natural Parks. Miyagi Prefecture is home to Matsushima, Matsushima Islands, a group of islands ranked as one of the Three Views of Japan, near the town of Matsushima, Miyagi, Matsushima. History Miyagi Prefectur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif
A massif () is a principal mountain mass, such as a compact portion of a mountain range, containing one or more summits (e.g. France's Massif Central). In mountaineering literature, ''massif'' is frequently used to denote the main mass of an individual mountain. As a purely scientific term in geology, however, a "massif" is separately and more specifically defined as a section of a planet's crust (geology), crust that is demarcated by geologic fault, faults or lithospheric flexure, flexures. In the plate tectonics, movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. A massif is a smaller structural unit than a tectonic plate and is considered the fourth-largest driving force in geomorphology. The word "massif" originates from French (in which the word also means "massive"), where it is used to refer to a large mountain mass or compact group of connected mountains forming an independent portion of a range. The Cydonia (regi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudflat
Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers. A global analysis published in 2019 suggested that tidal flat ecosystems are as extensive globally as mangroves, covering at least of the Earth's surface. / They are found in sheltered areas such as bays, bayous, lagoons, and estuaries; they are also seen in freshwater lakes and salty lakes (or inland seas) alike, wherein many rivers and creeks end. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and aquatic animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily. A recent global remote sensing analysis estimated that approximately 50% of the global extent of tidal flats occurs within eight countries (Indonesia, China, Au ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
