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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 p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Takasago, Hyōgo
260px, Takasago City Hall is a city located in Hyōgo Prefecture, Japan. , the city had an estimated population of 86,888 in 36828 households and a population density of 2500 persons per km². The total area of the city is . Geography Akashi 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 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 * 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 temperature in Takasago is 15.4 °C. The average annual rainfall is 1527 mm with September ... [...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". Historical background The Latin word (older Latin *prīsmo-kaps, literally "the one who takes the first lace/position), 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 formal position of monarch on the basis of principate, not dominion. He also tasked his grandsons as summer rulers of the city when most of the government were on holiday in the country or attending religious rituals, and, for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tokyo Imperial Palace
The is the main residence of the Emperor of Japan. It is a large park-like area located in the Chiyoda district of the 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 Family, an archive, museums and administrative offices. It is built on the site of the old Edo Castle. The total area including the gardens is . During the height of the 1980s Japanese property bubble, the palace grounds were valued by some to be more than the value of all of the real estate in the U.S. state of California. History Edo castle After the capitulation of the 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 26 November 1868, the Emperor arrived at the Edo Castle, made it to his new residence and renamed it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Himeji Castle
is a hilltop Japanese castle complex situated in the city of Himeji which is located 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 period. The castle is frequently known as ''Hakuro-jō'' or ''Shirasagi-jō'' ("White Egret Castle" or " White Heron Castle") because of its brilliant white exterior and supposed resemblance to a bird taking flight. Himeji Castle dates to 1333 when Akamatsu Norimura built a fort on top of Himeyama hill. The fort was dismantled and rebuilt as Himeyama Castle in 1346 and then remodeled into Himeji Castle two centuries later. Himeji Castle was then significantly remodeled in 1581 by Toyotomi Hideyoshi, who added a three-story castle keep. In 1600, Tokugawa Ieyasu awarded the castle to Ikeda Terumasa for his help in the Battle of Sekigahara, and Ikeda completely rebuilt the castle from 1 ... [...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 (c. 758). 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 cont ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow 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 ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...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 most deadly 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 which 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 French ... [...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, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent to granite. Rhyolitic magma is extremely viscous, due to its high silica content. 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 extensively used 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 amendment. Description Rhyolite i ... [...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, 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 Hyōgo Station, Hyōgo and Wadamisaki Station, Wadamisaki stations in Kobe, Hyōgo, 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 (Rail transport in Japan#Categories_of_r ... [...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 JR East and JR Central. It was also listed in the Nagoya and 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. 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. Urban Network The "Urban Network" is JR-West's name for its commuter rail lines in the Osaka-Kobe-Kyoto metropolitan area. These lines t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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