It is presumed that the name was given because it means that a dream is scented.
The shape of Yamanashi Prefecture is generally circular, with a length of about 90 km from east to west and north to south, and a total area of 4,465 km2. Except for the central Kofu basin, there are very few flat areas, and about 86% of the total area is mountainous. From the north to the east, the Kanto Mountains including Mt. Kobushi are connected, the Doshi Mountains and Misaka Mountains are connected to the south, the Akaishi Mountains to the west, and the steep mountains represented by Mt. Fuji in the south. The river basins in the prefecture are roughly divided into three first-class water systems, the Fuji River basin, the Sagami River basin, and the Tama River basin, which flow down from these mountains, and three second-class water systems, including Lake Motosu. It is located in the southern part of Fossa Magna (Shizuoka-Itoigawa Tectonic Line), and many fault branch lines are distributed around it. The oldest strata are the Shimanto Group, which was deposited from the Mesozoic to the Cenozoic Paleogene, and is distributed in the Southern Alps and the Kanto Mountains, and is subjected to severe folds. The next deposit was the Miocene Miocene Group of the Cenozoic Tertiary, which is mainly composed of green tuffs and is distributed in the Misaka Mountains and the Koma Mountains. Subsequently, from the Miocene to the Pliocene of the Cenozoic Era, the Fuji River Group centered on mudstone, sandstone, and conglomerate was deposited in the Gonan area. All of these are marine strata, and are fragile geology that is prone to collapse and landslides due to structural movements that accompany landing after formation. From the central part to the northern part of the prefecture, plutonic rocks (granite), which are thought to have invaded in the Tertiary period, are widely distributed. From the end of the Cenozoic III to the Quaternary, Mizugamori volcano, Kurofuji volcano, and Yatsugatake volcano are active one after another in the northern part of the Kofu basin, and these volcanic ejecta are deposited over plutonic rocks. The sediments in the Kofu basin are characterized by a predominant gravel layer and a small clay layer, indicating that the relative ground movements of the subsidence of the Kofu basin and the uplift of the surrounding mountains were intense. The climate is generally inland because it is surrounded by mountains, and there is a lot of rainfall in the summer, which is affected by the rainy season and typhoons. However, due to its complex terrain, its characteristics differ from region to region. I heard that the average temperature in Kofu is 15 degrees Celsius and the annual rainfall is 1,165.8 mm. Midai River hydraulic engineering business: The history of flood damage is old, and it is said that “Yamato Takeru no Mikoto was hit by flood damage at the time of the eastern expedition.” Is famous for having done. Shingen Takeda became the landlord of Kai at the age of 21 in 1541, but the following year, the Miteshi River flooded and the Kofu Basin became a riverbank. Having witnessed this, he felt the need for a hydraulic control project, and carried out hydraulic control work such as shogi heads and stone unloading, including the Shingen embankment, in an effort to enhance domestic affairs. These construction methods are said to be the ancestors of river and sabo engineering in Japan and are called the “Koshu Style River Defense Method”. At the top of the alluvial fan (Komaba, Minami-Alps City), Namoto was also built in a gantry pattern, and the flow was directed to the northeast. In Arino, Minami-Alps, a masonry embankment called Shogi-to was built to divide the torrent. About 500 m downstream, the water was split again by a shogi head to weaken the water force, and then joined the tributary Wappazawa. The somewhat weakened water force was merged with the Kamanashi River (Fuji River) and struck toward the high rocks on the opposite bank. Downstream to Takaiwa, a flat land extends from Ryuo Town to Kofu City, so a Shingen-Ko embankment was built to protect this. The earlier Midai River(Originating at Karamatsu Pass (GL = 1,650 m), which is connected to the Alps mountain range, it flows down Ashiyasu (formerly Ashiyasu Village) in Minami Alps from west to east and flows into the Kamanashi River (Fuji River). It is a 18.8 km first-class river. In the lower reaches, the Miteshigawa alluvial fan, which is known as one of Japan’s three major alluvial fans, spreads, and one side of fruit tree farmland spreads out. On the other hand, in the mountains in the upper reaches, it seems that the mountain stream forms a V-shaped valley and has a steep mountain stream with a slope of January 10 or more.), which diverged upstream, was merged with the water that bounced off the Takaiwa, and the water was controlled by the water so that the water could flow through the center of the river. Landslide that occurred in 2000 (Yumura district, Kofu city): It occurs prominently in the geology of the Neogene Miocene, and is characterized by being deeply involved in the tectonic line. The distribution area is concentrated in the middle basin of the Fuji River from Nishiyatsushiro District to Minamikoma District and the Tsurukawa River-Katsura River basin from Kitatsuru District to Otsuki City. The landslide prevention area is an area designated based on the “Landslide Prevention Law(1958 Law No. 30)”, and it seems that the act of inducing and promoting landslides is prohibited in this area as in the case of sabo designated areas. Mt. Fuji is a volcano that has grown through repeated large eruptions in the past. In recent years, it has been in a calm state, and the recent eruption dates back to the 1707 Hoei eruption in the middle of the Edo period, about 300 years ago. The life of a volcano is long, and the rest period of about 300 years is only a moment for the volcano, and it is possible that it will erupt in the near future. From October 2000 to February 2001, there were many “low frequency earthquakes” on Mt. Fuji, which are thought to be caused by the movement of magma beneath Mt. Fuji. This indicates that Mt. Fuji is a living volcano, and it can be considered that the sleeping Mt. Fuji is in a rough state. However, since February 2001, the number of low-frequency earthquakes has decreased, and there seems to be no sign of an eruption so far, but peace of mind is forbidden. It is known that people have lived in the land of Yamanashi prefecture for about 30,000 years. Kai Genji was born in the 12th century, and Shingen Takeda aimed to unify the world during the Warring States period in the 16th century. When the seclusion was lifted in the 19th century, it changed from Kofu to Yamanashi in the first year of the Meiji era, and has been rapidly modernized to the present day. It has been about 30,000 years ago that people’s activities have been recognized on the earth. The primitive society progresses from the stage of hunting, catching fish, and collecting nuts to the stage of rice cultivation, and the unevenness is integrated to form a country. From the end of the 4th century, the Daimaruyama Tomb and the Saikozuka / Maruyamazuka Tomb were built, and it is speculated that a large force existed in the Sone Hill Hills in the Nakamichi district of Kofu City. Yamanashi in the 8th century is called Kai Province and consists of 4 groups of “Yamanashi, Yashiro, Kokuma, Tsuru”. , It is said that it was near Ichinomiya Town. In the 12th century, the system of the ancient nation by the Kuge fluctuated, and it was the samurai who emerged from it. Around 1131, Minamoto no Yoshikiyo and Kiyomitsu’s parents and children entered Kai Province and came to Kai Genji. Among Mr. Kai Genji, Mr. Takeda, Mr. Ogasawara, and Mr. Nanbu prospered until posterity. In the 16th century, Mr. Takeda developed as a warring lord, built the Tsutsuji-gasakikan and the castle in Kofu, and based on this, proceeded with the four neighboring routes, aiming to unify the world. When Mr. Takeda was destroyed in 1582, the rule of Kai Province was transferred to Oda, Toyotomi, and Tokugawa, and the Kofu Domain (Kunichu) and the Yamura Domain (Gunuchiho) were established under the Edo Shogunate, but in 1724 the Shogunate was established. It will be under direct control. The development of Koshu Kaido and Fuji River shipping promoted the distribution of goods and the influx of culture. In the 19th century, due to the contradiction of the shogunate system, a lot of riots occurred in various places, and the Tenpo riot(It originated in the Gunuchiho district (Tsuru) in the eastern part of Kai, and spread to the Kuninaka district, causing a nation-wide turmoil. Also known as the Gunuchiho riot, Kai whole country riot, and Koshu riot. Kai Province was made into an imperial fief in 1724, and was controlled by the Kofu duty number and the third daikan who had jurisdiction over the town of Kofu. In the Kuninaka region, which embraces the Kofu basin, the development of newly reclaimed rice fields progressed in the modern era and became a breadbasket. , Was sent to Edo through Fujikawa Ship Transport. On the other hand, since there is little cultivated land in the Gunuchiho region, which is a mountainous area, there is a strong dependence on inter-farm work such as mountain earning and production of Gunuchiho, and the necessary rice grains are from all over the country, Sagami Province, and Suruga Province. I relied on imports. During the Kansei era, Kofu wholesaler friends weakened, rice dealers in Kajikazawa-inn (currently Kajikazawa, Fujikawa-cho) bought up and the number of rice grains exported as rice was increased, and merchants purchasing from Shinano also advanced, so the rice price There was a soaring price. In the middle of the night of August 17, 1836, a farmer in Shitatani Village broke the rice storehouse in Yamura Village, which started the turmoil. Yamura Village is loved by Tanimura Daikansho, a business trip camp of Ishiwa magistrate’s office, but Sanai Hashimoto, a former clerk, is absent. The villages are cracked down and collected. On the other hand, at the same time as the destruction in Tanimura, Takeshichi (Jizaemon) in Shimowada Village, Tsuru District (Nanahomachi, Otsuki City), and Inume Village (Inume, Uenohara City) in the same county, Torizawa Village (Inume, Uenohara City) When they joined in (Otsuki City), they planned a strong appeal for a reduction in rice prices and became the head of the riot. In addition, Dr. Taijun, the village head of Kuronota Village (Kuronoda, Sasago Town, Otsuki City), drafted the platform. Mr. Takeshichi was 70 years old at the time of Tenpo 7th year. His family of five had a height of Rokuto Ichiishi, but it gradually decreased and he was engaged in a quiet business. He also said that he was a boss who followed uninhabited and unreliable people. Mr. Hyo(Hei)suke was 40 years old in 1836. His surname is Mr. Mizukoshi and he is a family of three. He runs a Edo period lodging for travellers
at Inume-inn. His name is “Paddy shop”. The management of the paddy shop has deteriorated since its predecessor, and Mr. Hyosuke has issued a divorce letter to his wife during the uprising. The trends after the turmoil of both Takeshichi and Hyosuke will be described later. Mr. Takeshichi and Mr. Hyosuke borrowed and lent rice and gold from “unsuitable people” for the relief of the poor on a five-year basis, and were represented by the Kuninaka Village (Kasugai Town, Fuefuki City) and Mr. Okuuemon family. The plan is to have wealthy farmers in the country stop buying rice and release rice grains into the county. Okuuemon Okugawa of Kumanodo Village is a grain dealer who sells rice grains to the county, and it is said that he bought up rice grains during the Tenmei famine and was recognized as the cause of the soaring rice prices in the county. When both of them urged the gathering of the peasants in the county and led the county, they set out for the whole country targeting Okuuemon in Kumano-do Village, Manriki-suji, Yamanashi District, and smashed them all over the road. I returned to the village when I destroyed the house of Emon. Initially, the Gunuchiho were led by Mr. Takeshichi and Mr. Hyosuke, and were engaged in activities in accordance with the manners of revolt. Intensify and disorder. When the Chusei, led by the non-residents, separated from the Gunuchiho, they became mobs, armed with guns and bamboo spears, and deviated from theft and fire, forcing the villages to participate in the rebellion. When the national forces attacked Isawa-inn (Isawa Town, Fuefuki City) on August 22, they broke up into two, one heading from Koshu-dochu to Kofu Town (Kofu City), and the other heading south along the Fuefuki River. On August 23, the following day, the rebellion that proceeded along the Koshu road broke into the castle of Kofu when it broke through the defense battles of Kofu duty number Nagami Isenokami, Kofu deputy officer, Inoue Juzaemon’s hand, and so on. He broke the mansion of the grain brokers and the virtuous people, and also set fire. The rebellion that destroyed the castle of Kofu was further divided into two, and one move proceeded from Enkoji Village to Saijo Village (Showa Town) in Naka District, Koma County, continued to destroy Iida Shinmachi from Nishiaonuma Town, and Kitayama, Koma County via Arakawa. I proceeded to Kamiishida Town (Kofu City), Nishiyahata Village / Ryuo Village (Nishiyahata / Ryuo, Kai City), and when I smashed and ignited, I continued to smash at the Fuebuki River without crossing the Kamanashi River. On the other hand, one move south of Tokoji Village was partially arrested by the pursuit of Kofu taking turns on duty (esp. daimyo’s retainers on duty in Edo) Nagami Isenokami, and this was also divided into two moves in Nakagunsuji Otoguro Village. One went to Otawa Village, Naka District, and the other went to Saijo Village. When the turmoil broke down in Naka District Sujifuse Town and Imafuku Village, they joined in Otawa Village Magome, crossed the Fuefuki River, passed through Yashiro District Nishi District Ueno Town (Ichikawamisato Town), and Ichikawadaimon where Ichikawa cantonment exists. Reach the village. Tetsugoro Yamaguchi, Daikanyama Ichikawa, is in a sickbed, and the command of the suppression was done by Jinzaemon Takashima, but he moved out before many people. It is said that the turmoil was also destroyed in Ichikawadaimon Village, and Kyubei, the president of Kami-yui, was a blank gun but threatened with the gun he brought, forcing him to mobilize to participate in the turmoil. The turmoil further broke down at Kajikazawa inn when going south on the Surshu return, but after that, it returned to the north and went north at Nishigunsuji Aoyagi inn, Saishoji village, Tenjin Nakajo village, Nagasawa village (Fujikawa town). Continued to break down and reached Nishi District muscle Kajikazawa-inn. At Ogisawa-inn, the villagers counterattacked, but the turmoil further crossed the Yamaguchi station from Nirasaki-inn to Nishi-Otakegawa Village (Hakushu Town, Hokuto City) and reached the vicinity of the Koshin border. On August 23, Kofu working number Nagami Isenokami and Kofu bailiff Juzaemon Inoue, who allowed the destruction in Kofu town, requested the Suwa domain of Shinano Province to send troops, and slaughtered all the villages in Kuninaka. The villages in the Kofu Basin, which received the news of the destruction, collect information independently and work for defense. In addition, there were some who actively participated in the suppression of the turmoil, such as the masters of Mt. Ontake Kanazakura Shrine. The Shinano Suwa clan dispatched clan soldiers during the 24th, but when it was confirmed that the county’s return to the village and the turmoil had subsided, he visited Kofu on the 28th and returned to Shinano. The Shogunate has also ordered the Numazu Domain of Suruga Province and the Takato Domain of Shinano to dispatch troops, but both domains have withdrawn shortly after confirming the suppression of the turmoil. Hidetatsu Egawa (Tarozaemon), who has jurisdiction over the territories of Izu, Suruga, Musashi, and Sagami provinces, is also working to collect information about the turmoil. Egawa learned of the turmoil when he returned to Nirayama Daikansho after finishing the village of Suruga in Izu in August 7th, when the turmoil occurred. He is heading to Kai with Yakuro Saito and others. Egawa returned in August when he learned of the suppression of the turmoil from Kofu’s deputy officer, Tozaemon Inoue, on September 3. After the turmoil has subsided, the Shogunate will dispatch a scrutiny officer to investigate at the Ishiwa Daikansho. Mr. Takeshichi and Mr. Hyosuke, who became the leaders of the uprising in the county, left the riot after destroying Okuuemon’s house and returned to the village, but Mr. Takeshichi was guilty and self-confessed and was arrested. Mr. Takeshichi is decided to be crucifixed at Isawa-inn (Isawa Town, Fuefuki City), but he is dead in prison. On the other hand, Hyosuke has escaped from Kai and is wandering from Kanto to Hokuriku, Kinai, Shikoku, and China. A travel diary still exists in Hyosuke, and before 10 years of Tenpo, he returned to Inume Village, took his family to Kisarazu, Awa Province (Kisarazu City, Chiba Prefecture), changed his surname to Nara, and changed his name to Terakoya. Is said to have run. According to interviews with the sectarians’ book and descendants of Hosshoji Temple in Inume, Uenohara City, the Hyosuke family returned from Anbo to Kai before the 5th year of Ansei (1858), and Hyosuke died during the Keio era.)occurred in Yamanashi prefecture. Around this time, Japan began to break the isolation and become a modern nation under the pressure of Western countries. After entering Kofu Castle in March 1868, Koshu became Yamanashi Prefecture on November 20, 1868, after passing through Kai Province and Kofu Prefecture. In the first half of the Meiji era, the silk reeling industry and the wine brewing industry will be fostered by the Fujimura Prefectural Ordinance’s solicitation policy. In the second half, the Chuo Line will open and industry and culture will develop. Farmers have a high rate of crofting, and there are many crofting disputes from the Taisho era to the Showa era. Fujikawa boating declined sharply due to the opening of the Chuo Line, and its history closed in the early Showa period when the Minobu Line opened. In 1945, the end of the war was reached, and after the war, the land reform led to a system centered on self-produced farming, and the subsequent agricultural management was significantly converted to fruit trees. Commerce and industry developed during the period of high economic miracle. Furthermore, after the opening of the entire Chuo Expressway in 1982, logistics has been spurred, and it is said that industrialization is progressing more and more to this day. Yume Kaori Peach : From the Ministry of Agriculture, Forestry and Fisheries variety registration: Application number 19188 Application date 2006/01/05 Date of application publication 2006/11/17 Registration number 16477 Registration date 2008/03/13 Duration of breeder’s rights 30 years. Name and address of cultivar registrant Mr. Tadayoshi Takahashi (Miyoda Baba, Tsukidate-machi, Date City, Fukushima Prefecture), name of the person who cultivated the cultivar Mr. Tadayoshi Takahashi. This variety is cultivated from the natural hybrid seedlings of “Nishino Hakuto Peach”, the size of the fruit is maximum, the shape of the fruit is round, the color covering the pericarp is small, and the ground color of the flesh is greenish white. It is a variety that matures in early October in the breeding ground (Date City, Fukushima Prefecture). The shape of the tree is medium, the size of the tree is large, and the tree vigor is strong. The leaf height is extremely long, the leaf blade width is wide, the leaf blade color is green, and the nectary shape is spherical to kidney-shaped. The flowering type is normal, the petal color is pink, the flower shape is single, the petal shape is oval, wavy, with or without pollen. The size of the fruit is maximum, the shape is circular, the shape of the apex is wide and shallow, the depth of the suture line is medium, the width of the incision is wide, the depth is deep, the ground color of the pericarp is greenish white, covered. The color is red, the color covered is a little, the color type is solid (entire surface), the presence and density of hair on the pericarp is medium, the adhesion of the pericarp is a little strong, the ground color of the flesh is greenish white, and the flesh There is no coloring inside, there is a lot of coloring around the nucleus, the flesh is dense, there are few fibers, there is a lot of juice and sweetness, there is little acidity, there is no astringency / slight, and the aroma is medium. The size of the nucleus is quite large, the shape is oblong, the stickiness with the flesh is a viscous nucleus, the shade of brown is dark, and the nucleus crack is medium. The germination period and flowering period are early, and the number of maturation days is extremely long. Compared with “Yuzora Peach” and “Kanayama”, the distinction is recognized by the fact that the fruits and nuclei are larger. “Manatsu Peach(In 1997, the cultivar was selected from the seedlings of the natural hybrid seeds of Nishino Hakuto Peach at the breeder’s farm (Tsukidate Town, Date District, Fukushima Prefecture). The breeding was completed after confirming that its characteristics were stable in 2015.)”, a variety born from the natural hybrid seedlings of “Nishino Hakuto Peach”, which is his representative variety, was applied for registration in 2004 and registered in 2006. “Natsu no yo” Registered in 2009 and registered in 2013. The brand “Nishino Hakuto” was discovered by peach growers in the Nishino district of Minami-Alps City, Yamanashi Prefecture, and the cultivation technique was established in the 1965’s. A variety that supported the production of delicious peaches in Minami-Alps in the 1950s. The Okute variety “Akizora Peach” was cultivated by crossing with “Akatsuki Peach”, which is an original variety of Kanagawa prefecture. Incorporated Administrative Agency Agricultural and Food Industry Technology Research Organization (Tsukuba City, Ibaraki Prefecture) applied for registration in 1993 and registered in 1995 based on the registration of seedling method varieties.
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