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Beppu, Ōita
270px, Beppu City Hall is a city in Ōita Prefecture on the island of Kyushu, Japan. As of November 30, 2023, the city had a population of 113,045 in 62,702 households, and a population density of 900 persons per km2. The total area of the city is . Beppu is famous for its hot springs. In 2024, Beppu celebrated its centenary as a city. Geography Beppu is situated at the west end of Beppu Bay, around the east central prefecture. Adjacent municipalities include Ōita (the prefectural capital), Usa, Yufu, and Hiji. The east area of the city consists of an alluvial fan as well as alluvial plain, made with rivers flowing into Beppu Bay, namely Asami River, Haruki River and Sakai River. The main urban area of Beppu has been formed within this relatively narrow land which spans approximately 5 km from east to west and 10 km from north to south. The west area of the city includes a number of scenic locations such as Yufugawa Canyon, which has been selected as one of One H ...
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Cities Of Japan
A is a local Public administration, administrative unit in Japan. Cities are ranked on the same level as and , with the difference that they are not a component of . Like other contemporary administrative units, they are defined by the Local Autonomy Law of 1947. City status Article 8 of the Local Autonomy Law sets the following conditions for a municipality to be designated as a city: *Population must generally be 50,000 or greater (原則として人口5万人以上) *At least 60% of households must be established in a central urban area (中心市街地の戸数が全戸数の6割以上) *At least 60% of households must be employed in commerce, industry or other urban occupations (商工業等の都市的業態に従事する世帯人口が全人口の6割以上) *Any other conditions set by prefectural ordinance must be satisfied (他に当該都道府県の条例で定める要件を満たしていること) The designation is approved by the prefectural governor and t ...
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Beppu Bay
is an arm of the western end of the Seto Inland Sea of Japan. Beppu Bay is located on the northeast coast of Kyushu in Ōita Prefecture. The city of Ōita, Ōita, Ōita lies on its southern coast and the city of Beppu, Ōita, Beppu at its western end.''Websters New Geographical Dictionary'', Springfield, Massachusetts: Merriam-Webster Inc., 1984, pp. 137, 568. Notes

Bays of Kyushu Landforms of Ōita Prefecture {{Oita-geo-stub ...
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Osaka
is a Cities designated by government ordinance of Japan, designated city in the Kansai region of Honshu in Japan. It is the capital of and most populous city in Osaka Prefecture, and the List of cities in Japan, third-most populous city in Japan, following the special wards of Tokyo and Yokohama. With a population of 2.7 million in the 2020 census, it is also the largest component of the Keihanshin, Keihanshin Metropolitan Area, which is the List of metropolitan areas in Japan, second-largest metropolitan area in Japan and the 10th-List of urban areas by population, largest urban area in the world with more than 19 million inhabitants. Ōsaka was traditionally considered Japan's economic hub. By the Kofun period (300–538) it had developed into an important regional port, and in the 7th and 8th centuries, it served briefly as the imperial capital. Osaka continued to flourish during the Edo period (1603–1867) and became known as a center of Japanese culture. Following the M ...
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Kamakura Period
The is a period of History of Japan, Japanese history that marks the governance by the Kamakura shogunate, officially established in 1192 in Kamakura, Kanagawa, Kamakura by the first ''shōgun'' Minamoto no Yoritomo after the conclusion of the Genpei War, which saw the struggle between the Taira clan, Taira and Minamoto clan, Minamoto clans. The period is known for the emergence of the samurai, the warrior caste, and for the establishment of feudalism in Japan. There are various theories as to the year in which the Kamakura period and Kamakura shogunate began. In the past, the most popular theory was that the year was 1192, when Minamoto no Yoritomo was appointed . Later, the prevailing theory was that the year was 1185, when Yoritomo established the , which controlled military and police power in various regions, and the , which was in charge of tax collection and land administration. Japanese history textbooks as of 2016 do not specify a specific year for the beginning of the K ...
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Bungo Province
was a province of Japan in the area of eastern Kyūshū, corresponding to most of modern Ōita Prefecture, except what is now the cities of Nakatsu and Usa. Bungo bordered on Hyūga to the south, Higo and Chikugo to the west, and Chikuzen and Buzen to the north. Its abbreviated form was , although it was also called . In terms of the Gokishichidō system, Bungo was one of the provinces of the Saikaidō circuit. Under the '' Engishiki'' classification system, Bungo was ranked as one of the "superior countries" (上国) in terms of importance, and one of the "far countries" (遠国) in terms of distance from the capital. History Early history During the Kofun period, the area of Bungo had three main power centers: the Kunisaki Peninsula, the area around what is now Ōita District and the area around Hita District, each of which was ruled by a ''kuni no miyatsuko''. By the Asuka period, the area had been consolidated into a single province called Toyo Province, also ...
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Humid Subtropical Climate
A humid subtropical climate is a subtropical -temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia) or oceanic climates (in other continents). It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classific ...
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Mount Yufu
is a volcano located on the border of Yufu and Beppu, Ōita, Japan. It is located within Aso Kujū National Park. Overview Mount Yufu is a stratovolcano. Its most recent eruption about 2,200 years ago caused part of the mountain to collapse. Sometimes referred to as " Bungo Fuji," it has two peaks. The west peak (西峰, ''nishi-mine'') is about one meter higher than the east peak (東峰, ''higashi-mine'')''.'' At the base of the mountain is Yufuin, a tourist town famous for its ''onsen''. Some ''onsen'' baths in the town offer a view of Mount Yufu. Route The most popular route is from Yufu Tozanguchi Bus Stop of Kamenoi Bus. It takes two and half hours. There are other routes from Yufu City and Higashi Tozanguchi Bus Stop. From the summit, Beppu Bay, Yufuin, and the Kujū Mountain Range are visible. Both the east peak and west peak are climbable, with the west peak being considered more challenging than the east. Gallery File:Yufudake06.JPG, Summit File:Mt.yufu.jpg ...
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Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the Phanerozoic eon. It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today); a proposed third epoch, the Anthropocene, was rejected in 2024 by IUGS, the governing body of the ICS. The Quaternary is typically defined by the Quaternary glaciation, the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four succ ...
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Aso Kujū National Park
is a national park in Kumamoto and Ōita Prefectures, Japan. The park derives its name from Mount Aso, the largest active volcano in Japan, and the Kujū mountains. Mount Aso is also one of the largest caldera volcanos in the world. History Around 270,000 years ago, a burst of volcanic activity helped shape the area. Aso Shrine at Mount Aso in Kyushu is a Shinto shrine traditionally held to have been a center of worship before the accession of Emperor Jinmu. The ''shikinaisha'' shrine complex at Ichinomiya in what is today Kumamoto Prefecture was said to have been established in 281 BC. The original location of the shrine is uncertain because it was destroyed and rebuilt many times in or near the crater of Aso-san. *On December 4, 1934, this park was first established as Aso National Park. *On September 1, 1953, Mt. Yufu, Mt. Tsurumi, and Mt. Takasaki in Oita Prefecture were designated as extensions. *On May 1, 1956, Mt. Takasaki was separated and incorporated into th ...
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Alluvial Plain
An alluvial plain is a plain (an essentially flat landform) created by the deposition of sediment over a long period by one or more rivers coming from highland regions, from which alluvial soil forms. A ''floodplain'' is part of the process, being the smaller area over which the rivers flood at a particular time. In contrast, the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time. As the highlands erode due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, or ocean. As the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel floodwater capacity, the creek will, over time, seek new, lower paths, forming a meander (a curved path). The leftover higher locations, typically natural levees at the margins of ...
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Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to Semi-arid climate, semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where a flow of sediment or rocks emerge from a confined channel and are suddenly free to spread out in many directions. For example, many alluvial fans form when steep mountain valleys meet a flat plain. The transition from a narrow channel to a wide open area reduces the carrying capacity of flow and results in Deposition (geology), deposition of sediments. The flow can take the form of infrequent debris flows like in a landslide, or can be carried by an intermittent stream or creek. The reduction of flow is key to the formation of alluvial ...
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Hiji, Ōita
270px, Hiji Town Hall 270px, Hiji Castle ruins is a town located in Hayami District, Ōita Prefecture, Japan. , the town had an estimated population of 28,025 in 12811 households, and a population density of 380 persons per km2. The total area of the town is . Geography Hiji is located in central Ōita Prefecture, at the southern tip of the Kunisaki Peninsula, about 25 kilometers north of the prefectural capital at Ōita City. It occupies the northern shore of Beppu Bay. Neighbouring municipalities Ōita Prefecture * Beppu * Kitsuki * Usa Climate Hiji has a humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light to no snowfall. The average annual temperature in Hiji is 16.0 °C. The average annual rainfall is 1623 mm with September as the wettest month. The temperatures are highest on average in August, at around 26.6 °C, and lowest in January, at around 5.6 °C. Demographics Per Japanese census data, t ...
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