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Kyōtango
is a city located in Kyoto Prefecture, Japan. , the city had an estimated population of 52,683 in 22,886 households and a population density of 110 persons per km². The total area of the city is . Geography Kyōtango is located on the coast of the Sea of Japan on the western side of the Tango Peninsula in the northwestern corner of Kyoto Prefecture. The entire area of Kyōtango is in the eastern part of the San'in Kaigan Geopark. Neighbouring municipalities Kyoto Prefecture * Ine * Miyazu * Yosano Hyōgo Prefecture * Toyooka Climate Kyōtango has a Humid climate (Köppen ''Cfa'') characterized by warm, wet summers and cold winters with heavy snowfall. The average annual temperature in Kyōtango is . The average annual rainfall is with December as the wettest month. The temperatures are highest on average in August, at around , and lowest in January, at around . Its record high is , reached on 22 August 2018, and its record low is , reached on 26 February 1981. Demo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tango Province
was a province of Japan in the area of northern Kyoto Prefecture. Tango bordered on Tanba to the south, Tajima to the west, and Wakasa to the east. Its abbreviated form name was . It was also referred to as or . In terms of the Gokishichidō system, Tango was one of the provinces of the San'indō circuit. Under the ''Engishiki'' classification system, Tango was ranked as one of the "middle countries" (中国) in terms of importance, and one of the "near countries" (近国) in terms of distance from the capital. The provincial capital was located in what is now the city of Miyazu. The ''ichinomiya'' of the province is the Kono Shrine also located in Miyazu. The province had an area of . History Early history The Tango region prospered around the Takeno River basin (present-day Kyōtango city) during the Kofun period, during which time many keyhole-shaped burial mounds were constructed. As coins from the Xin dynasty of northern China have been found in the from the Hak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tango Peninsula
was a province of Japan in the area of northern Kyoto Prefecture. Tango bordered on Tanba to the south, Tajima to the west, and Wakasa to the east. Its abbreviated form name was . It was also referred to as or . In terms of the Gokishichidō system, Tango was one of the provinces of the San'indō circuit. Under the ''Engishiki'' classification system, Tango was ranked as one of the "middle countries" (中国) in terms of importance, and one of the "near countries" (近国) in terms of distance from the capital. The provincial capital was located in what is now the city of Miyazu. The ''ichinomiya'' of the province is the Kono Shrine also located in Miyazu. The province had an area of . History Early history The Tango region prospered around the Takeno River basin (present-day Kyōtango city) during the Kofun period, during which time many keyhole-shaped burial mounds were constructed. As coins from the Xin dynasty of northern China have been found in the from the Hak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amino Chōshiyama Kofun
270px, Aerial photograph The is a Kofun period burial mound, located in the Amino neighborhood of the city of Kyōtango, Kyoto in the Kansai region of Japan. The tumulus was designated a National Historic Site of Japan in 1922. Overview The Amino Chōshiyama Kofun is a , which is shaped like a keyhole, having one square end and one circular end, when viewed from above. It is located on a hill at the mouth of the Fukuta River that flows through the Tango Peninsula into the Sea of Japan. It dates from the middle of the Kofun period, or the end of the 4th century to the beginning of the 5th century. The surrounding area has a number of Yayoi period and Kofun period remains. The tumulus is orientated to the north-northeast and has an overall length of 201 meters, making it one of the largest on the Sea of Japan coast. The surface of the mound was covered in white ''fukiishi'', and both cylindrical and figurative ''haniwa'' have been found. Among the ''haniwa'', fragments of a type s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San'in Kaigan Geopark
The is a geopark in Japan. The area was declared a Japanese Geopark in 2008, and a UNESCO Global Geoparks Network, Global Geopark in 2010. The underlying themes of the geopark are "geological features, the natural environment, people's lives, and the formation of the Sea of Japan". This geologically diverse area contains records of the process from when Japan was part of the Asian continent to its present-day formation of the Sea of Japan. People's lives are also diverse in this area because of its geodiversity. Area The San'in Kaigan Geopark is located to the northwest of Osaka and Kyoto and consists of Kyōtango, Kyoto, Kyotango in Kyoto Prefecture, Toyooka, Hyōgo, Toyooka, Kami, Hyōgo (Mikata), Kami, and Shin'onsen, Hyōgo, Shin'onsen in Hyōgo Prefecture, Iwami, Tottori, Iwami, and a major part of Tottori, Tottori, Tottori in Tottori Prefecture. The geopark has an area of 2,458.44 square kilometers. Geosites The geopark includes sites that relate to the surrounding geomorph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ine, Kyoto
is a town located in Yosa District, Kyoto Prefecture, Japan Japan ( ja, 日本, or , and formally , ''Nihonkoku'') is an island country in East Asia. It is situated in the northwest Pacific Ocean, and is bordered on the west by the Sea of Japan, while extending from the Sea of Okhotsk in the north .... , the town had an estimated population of 1984 in 899 households and a population density of 32 persons per km².The total area of the town is . Geography Ine is located in the northern part of Kyoto Prefecture at the northeastern end of the Tango Peninsula. Located on the coast of the Sea of Japan, the town faces Wakasa Bay from the northeast to the southeast. Neighboring municipalities Kyoto Prefecture *Miyazu, Kyoto, Miyazu * Kyōtango, Kyoto, Kyōtango Climate Ine has a Humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cold winters with heavy snowfall. The average annual temperature in Ine is 14.4 °C. The average annual rainfall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toyooka, Hyōgo
is a Cities of Japan, city in the northern part of Hyōgo Prefecture, Japan. , the city had an estimated population of 78,348 in 37769 households and a population density of 110 persons per km².The total area of the city is . Geography Toyooka is located in the northern part of Hyōgo Prefecture and the Kinki region, facing the Sea of Japan in the north. It lies entirely within the San'in Kaigan Geopark. The Maruyama River flows through the central part of the city, and the Toyooka Basin, which is the largest basin in the Tajima region, spreads out in the central part of the city. Toyooka is located in the Snow country (Japan), "snow country" of Japan and is characterized by heavy accumulations of snow in winter. One of Toyooka's famous geological features is a basalt cave called Gembudō. Gembudō was formed 1.6 million years ago from the eruption of an ancient volcano. In 1926, Professor Motonori Matuyama of Kyoto University first proposed the theory of geomagnetic polarity ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yosano, Kyoto
270px, ''Chirimen Kaido'' in Yosano is a town located in Yosa District, Kyoto, Japan. , the town had an estimated population of 20,575 in 8978 households and a population density of 190 persons per km².The total area of the town is . Geography Yosano is located in the northern part of Kyoto Prefecture at the base of the Tango Peninsula. The Nodagawa River runs through most of the town south to north leading to the Miyazu Bay, and the Ama-no-Hashidate. The closest cities are Fukuchiyama to the south and Toyooka to the west, both about 45 minutes by car. The town is around 2 and a half hours north of Kyoto, Osaka, Himeji and Kobe. Neighboring municipalities Kyoto Prefecture *Fukuchiyama * Miyazu * Kyōtango Hyōgo Prefecture * Toyooka Climate Yosano has a Humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light to no snowfall. The average annual temperature in Yosano is 13.4 °C. The average annual rainfall is 1807 mm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miyazu, Kyoto
270px, Miyazu City Hall is a city located in Kyoto Prefecture, Japan. , the city had an estimated population of 16,988 in 8348 households and a population density of 98 persons per km². The total area of the city is . Geography Miyazu is located in the northern part of Kyoto Prefecture at the base of the Tango Peninsula, facing Wakasa Bay of the Sea of Japan to the east. Located in Miyazu City is Amanohashidate or the "bridge to heaven", said to be one of Japan's three most beautiful sights. The naturally formed land bridge is long and covered in pine trees. Neighboring municipalities Kyoto Prefecture *Kyōtango *Maizuru *Fukuchiyama * Yosano *Ine Climate Miyazu has a humid subtropical climate (Köppen ''Cfa''), featuring a marked seasonal variation in temperature and precipitation. Summers are hot and humid, but winters are relatively cold with occasional snowfall. The average annual temperature in Miyazu is . The average annual rainfall is with September as the wettest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muromachi Period
The is a division of Japanese history running from approximately 1336 to 1573. The period marks the governance of the Muromachi or Ashikaga shogunate (''Muromachi bakufu'' or ''Ashikaga bakufu''), which was officially established in 1338 by the first Muromachi ''shōgun'', Ashikaga Takauji, two years after the brief Kenmu Restoration (1333–1336) of imperial rule was brought to a close. The period ended in 1573 when the 15th and last shogun of this line, Ashikaga Yoshiaki, was driven out of the capital in Kyoto by Oda Nobunaga. From a cultural perspective, the period can be divided into the Kitayama and Higashiyama cultures (later 15th – early 16th centuries). The early years from 1336 to 1392 of the Muromachi period are known as the '' Nanboku-chō'' or Northern and Southern Court period. This period is marked by the continued resistance of the supporters of Emperor Go-Daigo, the emperor behind the Kenmu Restoration. The Sengoku period or Warring States period, which begi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tanba Province
was a province of Japan in the area of central Kyoto and east-central Hyōgo Prefectures. Tanba bordered on Harima, Ōmi, Settsu, Tajima, Wakasa, and Yamashiro Provinces. Its abbreviated form name was . In terms of the Gokishichidō system, Tanba was one of the provinces of the San'indō circuit. Under the ''Engishiki'' classification system, Tanba was ranked as one of the "superior countries" (上国) in terms of importance, and one of the "near countries" (近国) in terms of distance from the capital. The provincial capital is believed to have been located in what is now the city of Kameoka, although the exact location remains uncertain. The ''ichinomiya'' of the province is the Izumo-daijingū also located in Kameoka. The province had an area of . History Before the establishment of the Ritsuryō system, the area was under control of the Tanba Kokuzō and included both the Tanba and Tango areas. The province of Tango was created in 713 during the reign of Empress Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kofun
are megalithic tombs or tumuli in Northeast Asia. ''Kofun'' were mainly constructed in the Japanese archipelago between the middle of the 3rd century to the early 7th century CE.岡田裕之「前方後円墳」『日本古代史大辞典』大和書房、2006年。 The term is the origin of the name of the Kofun period, which indicates the middle 3rd century to early–middle 6th century. Many ''kofun'' have distinctive keyhole-shaped mounds (). The Mozu- Furuichi kofungun or tumulus clusters were inscribed on the UNESCO World Heritage List in 2019, while Ishibutai Kofun is one of a number in Asuka-Fujiwara residing on the Tentative List. Overview The ''kofun tumuli'' have assumed various shapes throughout history. The most common type of ''kofun'' is known as a , which is shaped like a keyhole, having one square end and one circular end, when viewed from above. There are also circular-type (), "two conjoined rectangles" typed (), and square-type () kofun. Orientation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kofun Period
The is an era in the history of Japan from about 300 to 538 AD (the date of the introduction of Buddhism), following the Yayoi period. The Kofun and the subsequent Asuka periods are sometimes collectively called the Yamato period. This period is the earliest era of recorded history in Japan, but studies depend heavily on archaeology since the chronology of historical sources tends to be distorted. The word '' kofun'' is Japanese for the type of burial mound dating from this era. It was a period of cultural import. Continuing from the Yayoi period, the Kofun period is characterized by influence from China and the Korean Peninsula; archaeologists consider it a shared culture across the southern Korean Peninsula, Kyūshū and Honshū. On the other hand, the most prosperous keyhole-shaped burial mounds in Japan during this period were approximately 5,000 in Japan from the middle of the 3rd century in the Yayoi period to the 7th century in the Asuka period, and many of them had huge t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
