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Ishi No Hōden
The is a megalithic monument located in the grounds of the , a Shinto shrine located in the city of Takasago, Hyōgo Prefecture in the Kansai region of Japan. Of unknown age, it was designated a National Historic Site of Japan in 1979 collectively with the nearby , which dates from the Kofun period. It is also called the . Ishi no Hōden The Ishi-no-Hōden is made from tuff and is surrounded on three sides by unprocessed bedrock. With a weight estimated at 500 tons, it measures 6.4 meters wide by 5.7 meters high by 7.2 meters in thickness. In shape, it is carved in the form of two flat rectangular parallelepipeds oriented vertically and sandwiching a small rectangular parallelepiped. One of the sides has a protrusion shaped like the top of a pyramid. The space between the surrounding bedrock and the megalith is wide enough for one adult to pass through, and it is possible to go around (admission fee is required). The monolith is situated in a large depression, which forms a po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takasago, Hyōgo
file:Takasago City Office.jpg, 260px, Takasago City Hall is a Cities of Japan, city located in Hyōgo Prefecture, Japan. , the city had an estimated population of 86,888 in 36,828 households and a population density of 2500 persons per km2. The total area of the city is . Geography Takasago is located in southern Hyōgo prefecture facing Harima Bay on the Seto Inland Sea. Most of the city area is located in the alluvial plain formed on the west side of the mouth of the Kako River, Kakogawa River, and the coastline is mostly reclaimed land. Tuffaceous rocky mountains are scattered throughout the city area, and the quarrying of these mountains since prehistoric times has resulted in a characteristic rocky landscape. Neighbouring municipalities Hyōgo Prefecture * Himeji, Hyōgo, Himeji * Kakogawa, Hyōgo, Kakogawa Climate Takasago has a Humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light to no snowfall. The average annual temp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prince Shotoku
A prince is a male ruler (ranked below a king, grand prince, and grand duke) or a male member of a monarch's or former monarch's family. ''Prince'' is also a title of nobility (often highest), often hereditary, in some European states. The female equivalent is a princess. The English word derives, via the French word ''prince'', from the Latin noun , from (first) and (head), meaning "the first, foremost, the chief, most distinguished, noble ruler, prince". In a related sense, now not commonly used, all more or less sovereign rulers over a state, including kings, were "princes" in the language of international politics. They normally had another title, for example king or duke. Many of these were Princes of the Holy Roman Empire. Historical background The Latin word (older Latin *prīsmo-kaps, ), became the usual title of the informal leader of the Roman senate some centuries before the transition to empire, the ''princeps senatus''. Emperor Augustus established the form ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tokyo Imperial Palace
is the main residence of the Emperor of Japan. It is a large park-like area located in the Chiyoda, Chiyoda, Tokyo, Chiyoda district of the Chiyoda, Tokyo, Chiyoda ward of Tokyo and contains several buildings including the where the Emperor has his living quarters, the where various ceremonies and receptions take place, some residences of the Imperial House of Japan, Imperial Family, an archive, museums and administrative offices. The palace grounds and gardens are built on the site of the old Edo Castle. History Edo castle After the capitulation of the Tokugawa shogunate, shogunate and the Meiji Restoration, the inhabitants, including the Shōgun Tokugawa Yoshinobu, were required to vacate the premises of the Edo Castle. Leaving the Kyoto Imperial Palace on November 26, 1868, the Emperor arrived at the Edo Castle, made it to his new residence and renamed it to . At this time, Tōkyō had also been called Tōkei. He left for Kyōto again, and after coming back on May ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Himeji Castle
() is a hilltop Japanese castle complex situated in Himeji, a city in the Hyōgo Prefecture of Japan. The castle is regarded as the finest surviving example of prototypical Japanese castle architecture, comprising a network of 83 rooms with advanced defensive systems from the Feudal Japan, feudal period. The castle is frequently known as ''Hakuro-jō'' or ''Shirasagi-jō'' ("White Egret Castle" or "heron, White Heron Castle") because of its brilliant white exterior and supposed resemblance to a bird taking flight. As with almost all Japanese castles from the Azuchi-Momoyama period onward, the , the most prominent structure, was used as a storehouse in times of peace and as a fortified tower in times of war, and the 's government offices and residences were located in a group of single-story buildings near the ''tenshu'' and the surrounding . Himeji Castle dates to 1333 when Akamatsu Norimura built a fort on top of Himeyama hill. The fort was dismantled and rebuilt as Himeyama Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yamato Province
was a province of Japan, located in Kinai, corresponding to present-day Nara Prefecture in Honshū. Nussbaum, Louis-Frédéric (2005). "Yamato" in . It was also called . Yamato consists of two characters, 大 "great", and 和 " Wa". At first, the name was written with one different character (), but due to its offensive connotation, for about ten years after 737, this was revised to use more desirable characters () (see Names of Japan). The final revision was made in the second year of the Tenpyō-hōji era (). It is classified as a great province in the '' Engishiki''. The Yamato Period in the history of Japan refers to the late Kofun Period (c. 250–538) and Asuka Period (538–710). Japanese archaeologists and historians emphasize the fact that during the early Kofun Period the Yamato Kingship was in close contention with other regional powers, such as Kibi Province near present-day Okayama Prefecture. Around the 6th century, the local chieftainship gained national contro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyroclastic Flow
A pyroclastic flow (also known as a pyroclastic density current or a pyroclastic cloud) is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano at average speeds of but is capable of reaching speeds up to . The gases and tephra can reach temperatures of about . Pyroclastic flows are the deadliest of all volcanic hazards and are produced as a result of certain explosive eruptions; they normally touch the ground and hurtle downhill or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope. Origin of term The word ''pyroclast'' is derived from the Greek (''pýr''), meaning "fire", and (''klastós''), meaning "broken in pieces". A name for pyroclastic flows that glow red in the dark is (French, "burning cloud"); this was notably used to describe the disastrous 1902 eruption of Mount Pelée on Martinique, a Frenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kako River
The Kako River is a river in the Cuyuni-Mazaruni region of Guyana and one of the largest tributaries of the Mazaruni River. 'Kako' is the Akawaio word for jasper which is found in the river. Mining Mining is prevalent throughout Guyana's waterways; there are about 144 mining claims and concessions allocated on the Kako River and its tributaries. Gold mining, done by dredging, pollutes waterways and in 2012, a series of conflicts arose between miners and Amerindians who rely on the water from the Kako River. After a third attempt was made to mine the area, an ex-parte injunction was brought against Toshao Mario Hastings. Amerindian groups defended Hastings, pointing out that the government is denying the people protection of their own land. The people of the surrounding village fear the Kako River to become polluted like the Mazaruni River. In March 2013, the United Nations Committee on International Convention on the Elimination of All Forms of Racial Discrimination expresse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture (geology), texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained matrix (geology), groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent of granite. Its high silica content makes rhyolitic magma extremely viscosity, viscous. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been used extensively for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San'yō Main Line
The is a major railway line owned by JR Group companies in western Japan, connecting Kōbe Station and Moji Station, largely paralleling the coast of the Seto Inland Sea, in other words, the southern coast of western Honshu. The San'yō Shinkansen line largely parallels its route. The name Sanyō derived from the ancient region and highway San'yōdō, the road on the sunny (south) side of the mountains. The Sanyō Main Line is operated by two JR companies: * West Japan Railway Company (JR West) JR Kobe Line, San'yō Line * Kyushu Railway Company (JR Kyushu) San'yō Line The Wadamisaki Line, a short section of line in the length of between and stations in Kobe is a branch of the Sanyō Main Line. A short section connecting Kitakyushu Freight Terminal also forms part of the Sanyō Main Line. Basic data *Operators, distances: . **West Japan Railway Company ( Category-1, Services and tracks) ***From Kobe to Shimonoseki: . ***From Hyōgo to Wadamisaki: . **Kyushu Railway C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
JR West
, also referred to as , is one of the Japan Railways Group (JR Group) companies and operates in western Honshu. It has its headquarters in Kita-ku, Osaka. It is listed in the Tokyo Stock Exchange, is a constituent of the TOPIX Large70 index, and is also one of only three Japan Railways Group constituents of the Nikkei 225 index: the others are East Japan Railway Company, JR East and Central Japan Railway Company, JR Central. It was also listed in the Nagoya Stock Exchange, Nagoya and Fukuoka Stock Exchange, Fukuoka stock exchanges until late 2020. Lines Shinkansen * Hokuriku Shinkansen ( - ) * San'yō Shinkansen * Hakata Minami Line :: Officially not a Shinkansen JR-West's highest-grossing line is the Sanyo Shinkansen high-speed rail line between Osaka and Fukuoka, Fukuoka, Fukuoka. The Sanyo Shinkansen alone accounts for about 40% of JR-West's passenger revenues. The company also operates Hakata Minami Line, a short commuter line with Shinkansen trains in Fukuoka, Fuku ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
