【製品名(商品名)】
キセラ
【種類】
Phasealus vulgaris L.
【卸地】
鹿児島県垂水市新城宮脇（池田青果）
【名前の由来】
Flowering is concentrated in a short period of time, and pod enlargement occurs at the same time. Derivation is while studying.
【主な特徴】
Mrs. Sai Maehara, who lives in a nursing care facility in Ueno-cho, Kanoya City, Kagoshima Prefecture, seems to have reached the age of 112, the oldest in the prefecture, on June 13, 2022. She seems to have celebrated her health and longevity with her relatives and staff holding her birthday party on the same day. Her grandmother said, “Thank you for your birthday,” and thanked everyone. She also she will be the oldest in the prefecture. Maehara was born in 1910 in Shinjo, Tarumizu City. The Taisho eruption of Sakurajima (The biggest volcanic disaster that Japan experienced in the 20th century. Moreover, it seems that it was a peculiar point in the world that Kagoshima city is located within 10 km from the crater. All of the recent volcanic disasters in Japan are local disasters, and it seems that they have not experienced wide-area ash fall damage like the Sakurajima Taisho eruption. Even in the case of secondary disasters such as sediment-related disasters, we have not experienced wide-area simultaneous multiple disasters. However, similar disasters occurred in the Tenmei eruption of Mt. Asama and the Hoei eruption of Mt. Fuji. There is no doubt that the Sakurajima Taisho eruption will be a good model case for the upcoming disaster in the Kanto region. Officials say that they want the lessons to be used as a valuable example of low-frequency large-scale disasters in volcanic disasters.
It seems that huge calderas of Kaku, Tou, Aira, and Ata are lined up linearly from the north in the tension field called Kagoshima Graben. Sakurajima was born on the southern edge of the Aira caldera as a post-caldera volcano about 26,000 years ago, about 3,000 years after the activity about 29,000 years before the Aira caldera erupted the Ito pyroclastic flow. It has a structure in which two stratovolcanoes, Mt. Kitadake and Mt. Minamidake, overlap. be. Recently, it seems that Minamidake is continuing its activities. Large-scale eruption in historical times It seems that Tenpyo-Houji (764), Bunmei (1471), Anei (1779), Taisho (1914), etc. are known as activities in the historical period. The Tenpyo-hoji eruption flowed out lava after the steam magma eruption of Nabeyama. The civilized eruption was the largest Plinian eruption in the historical era, and it seems that the topography of Mt. Kitadake changed completely due to the huge amount of pumice stones. Lava flows out to the east-northeast and southwest of Sakurajima. The Yasunaga eruption was also a fissure eruption, causing lava to flow northeast and south after the Plinian eruption and pyroclastic flow occurred. After that, there was a submarine eruption, and it seems that a new island called the Yasunaga Islands appeared. After the Taisho eruption, Sakurajima remained quiet despite small explosions and pyroclastic flows. And it seems that it flowed to the south and filled the village. Since this Showa eruption does not involve a Plinian eruption, it seems that it is generally not included in a large eruption. After that, an explosion suddenly occurred at the summit of Mt. Minamidake in 1955, and it seems that it continues to erupt until now, even though it has repeatedly disappeared. From 2006, it seems that the center of activity has moved to Showa Crater. It seems that the area around Southern Kyushu was in a geologically active period, such as the 1913 Masaki earthquake, the Hioki earthquake, and the eruption of Mt. Kirishima. Among them, there were precursory phenomena such as a drop in the water level of wells and a felt earthquake on Sakurajima Island, and it seems that some residents have begun to evacuate voluntarily. At 10:05 on January 12, the same year, a violent eruption started on the hillside of Nishi, and at 15:15, on the hillside of Higashi. At 20:14 on the 13th, a pyroclastic flow occurred on the hillside of Nishiyama and the village of Nishisakurajima was burnt. It started to run out of lava around 21:00 and reached the coastline in the evening of the 15th. This lava flow from the west flank filled Karasujima and ended in about two months, but the lava flow from the east flank filled the Seto Strait, reached the Osumi Peninsula around the end of January, and seemed to continue intermittently until the following spring 1915. is. During this time, the village office authorities inquired about the existence of an eruption at the weather station, but it seems that the reply was “No eruption on Sakurajima.” Most of the residents evacuated voluntarily according to the lessons learned from the Yasunaga eruption, but some knowledge classes who believed in the weather station’s words remained, and it seems that they were delayed in escaping. It seems that there were 30 victims of important islanders. On the other hand, at 18:20 on the 12th, a magnitude 7.1 earthquake occurred in Kinkou Bay, and the damage seems to have been concentrated in Kagoshima City and its surrounding areas. It is reported that the city was temporarily unmanned due to the upset caused by the tsunami and the hoaxes of poisonous gas. It is said that the lava flow that flowed out was about 3 billion tons due to the damage caused by the ejecta, and it seems that it covered 1/3 of the area of Sakurajima. A large amount of pumice and volcanic ash erupted, and it seems that they took advantage of the westerlies from the time and covered the Osumi Peninsula mainly. It is said that it reached 1m near Ushine in Tarumizu City. Naturally, it caused a great deal of damage to the agriculture, forestry and fisheries industry, and it seems that it also hindered transportation. The impact on agriculture seems to have varied depending on the amount and particle size of pumice and volcanic ash, and on the varieties of crops. In addition, it seems that the pumice stones floating on the sea hindered the navigation of the ship and hindered the rescue. Naturally in Sakurajima Island, there was a large amount of ash fall in the Takakuma Mountains, so the vegetation was destroyed and the mountains were devastated. It seems to be new. The total number of victims of this sediment disaster seems to exceed that of volcanic disasters. The earthquake in the evening of January 12 was a violent earthquake with a seismic intensity of 6 near Kagoshima City, and it seems that it was felt throughout Kyushu. Human damage was 29 people, but building damage seems to have been concentrated in urban areas, especially in landfills during the Edo period. The collapse of the Shirasu cliff has also occurred, and the evacuees have been involved and nine important people have died. It seems that the railroad was also cut off due to a sediment disaster on the Aira Caldera wall between Shigetomi and Kagoshima. The telephone line and power line were cut off, and the post office and newspaper company were also damaged, so it seems that communication and public relations were hindered. At that time, there was no voluntary disaster prevention organization, but because of the strong territorial society, the youth associations, women’s associations, and local military personnel associations in the surrounding cities, towns and villages around the Gulf set out rescue boats and prepared meals. It seems that he was rescued. It seems that it was fortunate that there were many fishing boats because the islanders at that time were half-farming and half-fishing. It seems that the prefectural office, county office, Kagoshima City Hall, and police, who believed in the words of the weather station, also carried out prompt rescue activities and set up evacuation shelters at the same time as the eruption occurred. The Army and Navy also seemed to play an important role by sending out rescue boats and guarding the unmanned city. The Kagoshima Branch of the Red Cross Society and the Medical Association have also set up first aid stations. The business community, such as the Chamber of Commerce, also spends relief money. Nationwide donations were also collected, including the Tohoku Kyushu Disaster Relief Society. It seems that donations were also received from overseas. It seems that infectious diseases such as dysentery and typhoid fever occurred at the evacuation site, probably because of the evacuation life in an unsanitary condition for a long period of time, causing more deaths than direct disaster victims. Emergency restoration work was carried out immediately on roads and rivers, but the river disaster seems to have continued for a long time as mentioned above. Agricultural land covered with ash fall began to be turned upside down, and it seems that restoration work was carried out according to its thickness. At the Agricultural Experiment Station of the Ministry of Agriculture and Commerce, it seems that they gave careful guidance such as how to neutralize acidified soil and encourage the cultivation of acid-resistant varieties. About half of the islands returned to the island after the eruption had subsided, but it seems that not only the island but also the Osumi Peninsula, where the ash fall was severe, had a series of hardships such as restoration of farmland and reconstruction of houses and schools. Initially, it relied on income such as labor costs for civil engineering work. It seems that a lot of generous assistance was provided by the national treasury subsidy (national tax adjustment fee) and donations. It seems that those who lost their land because they were buried in lava and the residents who could not cultivate due to thick ash fall were forced to relocate. After all, it seems that a total of about 20,000 people have migrated, including 1,001 houses in designated migration areas and 2,071 houses in voluntary migration areas. The latter relies on ties, but the former seems to be an area assigned by the prefecture. It seems that the national government has adopted a method of providing national forests to the prefecture free of charge and the prefecture lending them to migrants. It seems that the land ownership will be transferred 10 years after the completion of the reclamation. It seems that the designated emigration areas are the southern part of the Osumi Peninsula, the foot of Kirishima, Miyazaki Prefecture, and Jeolla-do, Korea. It seems that the migrants have received considerable assistance from the disaster relief fund, such as migration costs, farm equipment costs, seedling costs, furniture costs, hut costs, and food costs. It seems that three ordinary elementary schools have been newly established in remote areas. It seems that there was only one old-fashioned Milne seismograph at the Kagoshima weather station at the time of the Taisho eruption. After the eruption, Professor Fusakichi OMORI (1868-1923: Omori and Akitsune IMAMURA (1870-1948), who represent Japanese seismology in the Meiji and Taisho eras, seem to have had a long-lasting conflict between them. The causes can be divided into theoretical conflicts, differences in basic ideas about disaster prevention, and emotional discrepancies. It is said that the conflict between the two began when Omori instructed Imamura to conduct a preliminary investigation of the Nobi earthquake on October 28, 1891, but the first theoretical conflict occurred. , Meiji Sanriku Earthquake Tsunami (1896) has been handed down as a cause of the tsunami. The controversy in which Imamura insists on the “seafloor crustal movement theory” and Omori insists on the “fluid pendulum theory” lasts for 10 years, and many researchers at that time supported Omori, and Imamura is isolated in academia. After that, the Imamura theory was accepted, but it is thought that the surroundings at this time also deepened the emotional gap between the two.) of the University of Tokyo hurriedly installed a state-of-the-art Omori seismograph and made his own observations, leaving a valuable record. Currently, a detailed observation network by the Japan Meteorological Agency, University, Geospatial Information Authority of Japan, Ministry of Land, Infrastructure, Transport and Tourism, Kagoshima Prefecture, etc. has been set up, and a volcanic activity model of Sakurajima has been established, so it is possible to give some advance information unlike at that time. It seems that the system is in place. Currently, volcanic hazard maps and disaster prevention maps have been released, and it seems that comprehensive disaster prevention drills are held every year on January 12, the day of the eruption. However, it seems that the response to completely new phenomena such as submarine eruptions and collapse of mountains is not sufficient. According to observations, magma has recovered 80% of the time in the Taisho era. He says he must be vigilant against large-scale eruptions. During the Taisho eruption, sediment disasters and floods occurred frequently over a wide area at the same time. Currently, individual measures such as constructing a sabo dam for each river system are being implemented, but it seems necessary to consider wide-area countermeasures in terms of both hardware and software, taking into consideration heavy ash fall and earthquakes. It seems that ash fall and pumice stones caused devastating damage to the agriculture, forestry and fisheries industry, which was the main industry at that time. However, nowadays, the environment surrounding the agriculture, forestry and fisheries industry has changed drastically due to the emergence of large-scale livestock and aquaculture industries that did not exist at that time. It seems necessary to simulate damage to agriculture, forestry and fisheries in response to large-scale and centralized damage. At the time of the Taisho eruption, it seems that many people had no choice but to relocate because they lost not only their household goods but also their land. Even in the present age when science and technology have advanced, there seems to be a risk of losing land. Also, unlike transient earthquake disasters, volcanic disasters are often prolonged. It seems that it is necessary to always think about support for rebuilding lives, including legal development. He also says that it is essential to take measures to deal with the increase in the number of people requiring assistance during a disaster.) At that time, he seems to have a memory of desperately escaping with his family. She is blessed with two sons and two daughters, and according to her relatives, she has two children, eight grandchildren, ten great-grandchildren, and one great-great-grandchild as of the same day. It seems that about 40 people, including the residents of “Ueno Group Home,” who are currently living, gathered at her birthday party. The grandmother she was interviewed by the staff said she also likes to sing, and she seems to have performed this enka “Futarizake (a representative song of singer Miyuki Kawanaka)”. She sang a verse with a tense voice, and she seemed to be wrapped in big applause. “Tarumizu City, Kagoshima Prefecture”, Located in the northwestern part of the Osumi Peninsula, almost in the center facing Kagoshima Bay. A key point on land at sea connecting Kagoshima City, the prefectural capital, and the Osumi Peninsula. Kirishima City to the north and Sakurajima to the west : The east borders Kanoya City with the Takakuma mountain range as the boundary. It covers an area of about 162.12 km2 and has a coastline of 37 km. Taking advantage of such terrain, the aquaculture industry of yellowtail and amberjack is thriving. The climate is mild and fruits such as loquats and citrus fruits : Cultivation of vegetables such as French bean（Pisum sativum）and Green beans is also popular. In addition, hot spring water that springs from the ground from the Takakuma mountain range : It is popular as a healthy drinking water that contains abundant natural minerals in a well-balanced manner. “垂水市”, There are various theories about the origin of the name. Under the cliff of Tarumizu Castle -“Shimizu” drips from between the rocks and there is a pool of water : It is famous because it was the only drinking water in this area. It is said that this place name happened. It is said that the name first appeared in the record during the Heian period. Kazusa no Suke Syunsei（蒲生（Kamou）上総介舜清（Chikakiyo）（真光房）- Son of Fujiwara no Norikiyo）in 1120 : Build a castle from Usa down to Shimo-Osumi. Tarumizu Shimazu family ; 島津忠将 : 薩隅日三州中興之賢太守貴久, Second younger brother 忠良入道日新, Second son. Its eldest son Mochihisa ; In 1598, he moved from Tanegashima Island to Tarumi and became a lord. Kokudaka is 17,000 crop yield, 領地は垂水の他, 大崎, 高山, 大姶良, 鹿屋, 串良, 宮崎の縄瀬などに及ぶ. It ruled Tarumizu for about 250 years until the Meiji Restoration. The castle was too small for vassals to live in. Relocation Started construction of the castle and relocated in 1611 – お長屋跡; 林之城 (現: 垂水小学校). In particular, we focused on promoting education. At that time, it was called the best in the domain in terms of culture. That spirit was inherited after the Meiji Restoration. With the times, many human resources have been produced in various fields. “Shinjo and Usine”, Later, a standing corps was set up in each township to control the military and administration. City flowers / Trees : Rhododendron sataense ;高峠つつじ, A variety of a plant belonging to the heath family called ‘yama-tsutsuji’. “牛根松”, I have to investigate. 宮脇公園 : Located between Japan National Route 220 and the coastline. A park with a beautiful row of ficus superba trees with a total length of 1.5 km. A row of about 100 trees : It is a large tree over 100 years old and has many roots hanging from its branches. It also creates a tropical atmosphere. An evergreen tree of the subtropical Moraceae fig genus that grows on warm coasts. It is treated as an academically valuable plant. Trees are planted as sandproof, windproof, and park trees : It is popular as a place of relaxation for local residents and as a drive spot. The landscape seen from here is beautiful. Kaimon Mountains and Kinko Bay seen from the park ; Sunset over the Satsuma Peninsula, etc.「かごしまよかとこ100選海道の旅」に, 選定. 垂水市教育委員会 2002, 垂水市埋蔵文化財発掘調査報告書6 : 宮ノ前遺跡, 重田遺跡, 新城宮脇, 縄文, 弥生, 古墳時代, 土杭, 縄文土器, 弥生土器, 成川式土器, 縄文時代後期, 晩期, 弥生時代, 古墳時代. Ministry of Agriculture, Forestry and Fisheries Variety registration. Application number 5331 Date of application 1992 / 06 / 15. Registration number 4532 Date of registration 1995 / 06 / 13. This variety is a fixed variety cultivated by mating the strains owned by the applicant, and is a cultivar for pods with finite dwarf, dark green leaves and white flowers, dark green pods, and no streaks. Embryonic axis color is green, elongation and plant type are finite dwarf, plant height is medium, number of main stem nodes is medium, leaf color is dark green, leaflet size is medium, flower color is white. , Width is narrow, degree of bending is straight, beak length is long, shape is lightly bent, no constriction, surface is smooth, cross section is circular, hard and soft is soft, with or without streaks. The ground color is dark green, there is no spot color, the grain size is extremely small, the shape is oblong, there is no type of seed coat spot, the ground color is white, there is no ring color. Medium maturity, medium lodging resistance. Compared to “Compact bean”, the size of the leaflets is large, the degree of pod bending is straightforward, and the length of the pods is long. The surface of the pod is smooth, the length of the pod’s beak is longer than that of “Nerina bean”, the surface of the pod is smooth, the cross section of the pod is circular, etc. It is said that sex is recognized. Plant Breeder’s right has a lifespan of 15 years.The extinction date expires on June 14, 2010. Name of cultivar registrant, SVS Holland (Netherlands, 1601 BM Enkuhayusen), registered cultivar breeder, Jeff Willemsen. We performed forward and reverse mating with “83 / 2423-6” and “83 / 5821-5” as parent lines, and later selected individuals and repeated line selection. In 1987, in the F11 generation, we had the desired characteristics. After confirming that the breeding was completed.
Snow brand seed co., Ltd. is a wholly owned subsidiary of Megmilk Snow Brand Co., Ltd. “ベストクロップキセラインゲン”, After sowing – A mesophyll species that can be harvested in about 62 days. The plant height is around 60 cm, and the leaves are small and have many branches and flowers. The length of the pod is about 15 cm. It is slow to gain weight, and there is little deterioration in quality even with a slight delay-Round pod seed.
It seems that huge calderas of Kaku, Tou, Aira, and Ata are lined up linearly from the north in the tension field called Kagoshima Graben. Sakurajima was born on the southern edge of the Aira caldera as a post-caldera volcano about 26,000 years ago, about 3,000 years after the activity about 29,000 years before the Aira caldera erupted the Ito pyroclastic flow. It has a structure in which two stratovolcanoes, Mt. Kitadake and Mt. Minamidake, overlap. be. Recently, it seems that Minamidake is continuing its activities. Large-scale eruption in historical times It seems that Tenpyo-Houji (764), Bunmei (1471), Anei (1779), Taisho (1914), etc. are known as activities in the historical period. The Tenpyo-hoji eruption flowed out lava after the steam magma eruption of Nabeyama. The civilized eruption was the largest Plinian eruption in the historical era, and it seems that the topography of Mt. Kitadake changed completely due to the huge amount of pumice stones. Lava flows out to the east-northeast and southwest of Sakurajima. The Yasunaga eruption was also a fissure eruption, causing lava to flow northeast and south after the Plinian eruption and pyroclastic flow occurred. After that, there was a submarine eruption, and it seems that a new island called the Yasunaga Islands appeared. After the Taisho eruption, Sakurajima remained quiet despite small explosions and pyroclastic flows. And it seems that it flowed to the south and filled the village. Since this Showa eruption does not involve a Plinian eruption, it seems that it is generally not included in a large eruption. After that, an explosion suddenly occurred at the summit of Mt. Minamidake in 1955, and it seems that it continues to erupt until now, even though it has repeatedly disappeared. From 2006, it seems that the center of activity has moved to Showa Crater. It seems that the area around Southern Kyushu was in a geologically active period, such as the 1913 Masaki earthquake, the Hioki earthquake, and the eruption of Mt. Kirishima. Among them, there were precursory phenomena such as a drop in the water level of wells and a felt earthquake on Sakurajima Island, and it seems that some residents have begun to evacuate voluntarily. At 10:05 on January 12, the same year, a violent eruption started on the hillside of Nishi, and at 15:15, on the hillside of Higashi. At 20:14 on the 13th, a pyroclastic flow occurred on the hillside of Nishiyama and the village of Nishisakurajima was burnt. It started to run out of lava around 21:00 and reached the coastline in the evening of the 15th. This lava flow from the west flank filled Karasujima and ended in about two months, but the lava flow from the east flank filled the Seto Strait, reached the Osumi Peninsula around the end of January, and seemed to continue intermittently until the following spring 1915. is. During this time, the village office authorities inquired about the existence of an eruption at the weather station, but it seems that the reply was “No eruption on Sakurajima.” Most of the residents evacuated voluntarily according to the lessons learned from the Yasunaga eruption, but some knowledge classes who believed in the weather station’s words remained, and it seems that they were delayed in escaping. It seems that there were 30 victims of important islanders. On the other hand, at 18:20 on the 12th, a magnitude 7.1 earthquake occurred in Kinkou Bay, and the damage seems to have been concentrated in Kagoshima City and its surrounding areas. It is reported that the city was temporarily unmanned due to the upset caused by the tsunami and the hoaxes of poisonous gas. It is said that the lava flow that flowed out was about 3 billion tons due to the damage caused by the ejecta, and it seems that it covered 1/3 of the area of Sakurajima. A large amount of pumice and volcanic ash erupted, and it seems that they took advantage of the westerlies from the time and covered the Osumi Peninsula mainly. It is said that it reached 1m near Ushine in Tarumizu City. Naturally, it caused a great deal of damage to the agriculture, forestry and fisheries industry, and it seems that it also hindered transportation. The impact on agriculture seems to have varied depending on the amount and particle size of pumice and volcanic ash, and on the varieties of crops. In addition, it seems that the pumice stones floating on the sea hindered the navigation of the ship and hindered the rescue. Naturally in Sakurajima Island, there was a large amount of ash fall in the Takakuma Mountains, so the vegetation was destroyed and the mountains were devastated. It seems to be new. The total number of victims of this sediment disaster seems to exceed that of volcanic disasters. The earthquake in the evening of January 12 was a violent earthquake with a seismic intensity of 6 near Kagoshima City, and it seems that it was felt throughout Kyushu. Human damage was 29 people, but building damage seems to have been concentrated in urban areas, especially in landfills during the Edo period. The collapse of the Shirasu cliff has also occurred, and the evacuees have been involved and nine important people have died. It seems that the railroad was also cut off due to a sediment disaster on the Aira Caldera wall between Shigetomi and Kagoshima. The telephone line and power line were cut off, and the post office and newspaper company were also damaged, so it seems that communication and public relations were hindered. At that time, there was no voluntary disaster prevention organization, but because of the strong territorial society, the youth associations, women’s associations, and local military personnel associations in the surrounding cities, towns and villages around the Gulf set out rescue boats and prepared meals. It seems that he was rescued. It seems that it was fortunate that there were many fishing boats because the islanders at that time were half-farming and half-fishing. It seems that the prefectural office, county office, Kagoshima City Hall, and police, who believed in the words of the weather station, also carried out prompt rescue activities and set up evacuation shelters at the same time as the eruption occurred. The Army and Navy also seemed to play an important role by sending out rescue boats and guarding the unmanned city. The Kagoshima Branch of the Red Cross Society and the Medical Association have also set up first aid stations. The business community, such as the Chamber of Commerce, also spends relief money. Nationwide donations were also collected, including the Tohoku Kyushu Disaster Relief Society. It seems that donations were also received from overseas. It seems that infectious diseases such as dysentery and typhoid fever occurred at the evacuation site, probably because of the evacuation life in an unsanitary condition for a long period of time, causing more deaths than direct disaster victims. Emergency restoration work was carried out immediately on roads and rivers, but the river disaster seems to have continued for a long time as mentioned above. Agricultural land covered with ash fall began to be turned upside down, and it seems that restoration work was carried out according to its thickness. At the Agricultural Experiment Station of the Ministry of Agriculture and Commerce, it seems that they gave careful guidance such as how to neutralize acidified soil and encourage the cultivation of acid-resistant varieties. About half of the islands returned to the island after the eruption had subsided, but it seems that not only the island but also the Osumi Peninsula, where the ash fall was severe, had a series of hardships such as restoration of farmland and reconstruction of houses and schools. Initially, it relied on income such as labor costs for civil engineering work. It seems that a lot of generous assistance was provided by the national treasury subsidy (national tax adjustment fee) and donations. It seems that those who lost their land because they were buried in lava and the residents who could not cultivate due to thick ash fall were forced to relocate. After all, it seems that a total of about 20,000 people have migrated, including 1,001 houses in designated migration areas and 2,071 houses in voluntary migration areas. The latter relies on ties, but the former seems to be an area assigned by the prefecture. It seems that the national government has adopted a method of providing national forests to the prefecture free of charge and the prefecture lending them to migrants. It seems that the land ownership will be transferred 10 years after the completion of the reclamation. It seems that the designated emigration areas are the southern part of the Osumi Peninsula, the foot of Kirishima, Miyazaki Prefecture, and Jeolla-do, Korea. It seems that the migrants have received considerable assistance from the disaster relief fund, such as migration costs, farm equipment costs, seedling costs, furniture costs, hut costs, and food costs. It seems that three ordinary elementary schools have been newly established in remote areas. It seems that there was only one old-fashioned Milne seismograph at the Kagoshima weather station at the time of the Taisho eruption. After the eruption, Professor Fusakichi OMORI (1868-1923: Omori and Akitsune IMAMURA (1870-1948), who represent Japanese seismology in the Meiji and Taisho eras, seem to have had a long-lasting conflict between them. The causes can be divided into theoretical conflicts, differences in basic ideas about disaster prevention, and emotional discrepancies. It is said that the conflict between the two began when Omori instructed Imamura to conduct a preliminary investigation of the Nobi earthquake on October 28, 1891, but the first theoretical conflict occurred. , Meiji Sanriku Earthquake Tsunami (1896) has been handed down as a cause of the tsunami. The controversy in which Imamura insists on the “seafloor crustal movement theory” and Omori insists on the “fluid pendulum theory” lasts for 10 years, and many researchers at that time supported Omori, and Imamura is isolated in academia. After that, the Imamura theory was accepted, but it is thought that the surroundings at this time also deepened the emotional gap between the two.) of the University of Tokyo hurriedly installed a state-of-the-art Omori seismograph and made his own observations, leaving a valuable record. Currently, a detailed observation network by the Japan Meteorological Agency, University, Geospatial Information Authority of Japan, Ministry of Land, Infrastructure, Transport and Tourism, Kagoshima Prefecture, etc. has been set up, and a volcanic activity model of Sakurajima has been established, so it is possible to give some advance information unlike at that time. It seems that the system is in place. Currently, volcanic hazard maps and disaster prevention maps have been released, and it seems that comprehensive disaster prevention drills are held every year on January 12, the day of the eruption. However, it seems that the response to completely new phenomena such as submarine eruptions and collapse of mountains is not sufficient. According to observations, magma has recovered 80% of the time in the Taisho era. He says he must be vigilant against large-scale eruptions. During the Taisho eruption, sediment disasters and floods occurred frequently over a wide area at the same time. Currently, individual measures such as constructing a sabo dam for each river system are being implemented, but it seems necessary to consider wide-area countermeasures in terms of both hardware and software, taking into consideration heavy ash fall and earthquakes. It seems that ash fall and pumice stones caused devastating damage to the agriculture, forestry and fisheries industry, which was the main industry at that time. However, nowadays, the environment surrounding the agriculture, forestry and fisheries industry has changed drastically due to the emergence of large-scale livestock and aquaculture industries that did not exist at that time. It seems necessary to simulate damage to agriculture, forestry and fisheries in response to large-scale and centralized damage. At the time of the Taisho eruption, it seems that many people had no choice but to relocate because they lost not only their household goods but also their land. Even in the present age when science and technology have advanced, there seems to be a risk of losing land. Also, unlike transient earthquake disasters, volcanic disasters are often prolonged. It seems that it is necessary to always think about support for rebuilding lives, including legal development. He also says that it is essential to take measures to deal with the increase in the number of people requiring assistance during a disaster.) At that time, he seems to have a memory of desperately escaping with his family. She is blessed with two sons and two daughters, and according to her relatives, she has two children, eight grandchildren, ten great-grandchildren, and one great-great-grandchild as of the same day. It seems that about 40 people, including the residents of “Ueno Group Home,” who are currently living, gathered at her birthday party. The grandmother she was interviewed by the staff said she also likes to sing, and she seems to have performed this enka “Futarizake (a representative song of singer Miyuki Kawanaka)”. She sang a verse with a tense voice, and she seemed to be wrapped in big applause. “Tarumizu City, Kagoshima Prefecture”, Located in the northwestern part of the Osumi Peninsula, almost in the center facing Kagoshima Bay. A key point on land at sea connecting Kagoshima City, the prefectural capital, and the Osumi Peninsula. Kirishima City to the north and Sakurajima to the west : The east borders Kanoya City with the Takakuma mountain range as the boundary. It covers an area of about 162.12 km2 and has a coastline of 37 km. Taking advantage of such terrain, the aquaculture industry of yellowtail and amberjack is thriving. The climate is mild and fruits such as loquats and citrus fruits : Cultivation of vegetables such as French bean（Pisum sativum）and Green beans is also popular. In addition, hot spring water that springs from the ground from the Takakuma mountain range : It is popular as a healthy drinking water that contains abundant natural minerals in a well-balanced manner. “垂水市”, There are various theories about the origin of the name. Under the cliff of Tarumizu Castle -“Shimizu” drips from between the rocks and there is a pool of water : It is famous because it was the only drinking water in this area. It is said that this place name happened. It is said that the name first appeared in the record during the Heian period. Kazusa no Suke Syunsei（蒲生（Kamou）上総介舜清（Chikakiyo）（真光房）- Son of Fujiwara no Norikiyo）in 1120 : Build a castle from Usa down to Shimo-Osumi. Tarumizu Shimazu family ; 島津忠将 : 薩隅日三州中興之賢太守貴久, Second younger brother 忠良入道日新, Second son. Its eldest son Mochihisa ; In 1598, he moved from Tanegashima Island to Tarumi and became a lord. Kokudaka is 17,000 crop yield, 領地は垂水の他, 大崎, 高山, 大姶良, 鹿屋, 串良, 宮崎の縄瀬などに及ぶ. It ruled Tarumizu for about 250 years until the Meiji Restoration. The castle was too small for vassals to live in. Relocation Started construction of the castle and relocated in 1611 – お長屋跡; 林之城 (現: 垂水小学校). In particular, we focused on promoting education. At that time, it was called the best in the domain in terms of culture. That spirit was inherited after the Meiji Restoration. With the times, many human resources have been produced in various fields. “Shinjo and Usine”, Later, a standing corps was set up in each township to control the military and administration. City flowers / Trees : Rhododendron sataense ;高峠つつじ, A variety of a plant belonging to the heath family called ‘yama-tsutsuji’. “牛根松”, I have to investigate. 宮脇公園 : Located between Japan National Route 220 and the coastline. A park with a beautiful row of ficus superba trees with a total length of 1.5 km. A row of about 100 trees : It is a large tree over 100 years old and has many roots hanging from its branches. It also creates a tropical atmosphere. An evergreen tree of the subtropical Moraceae fig genus that grows on warm coasts. It is treated as an academically valuable plant. Trees are planted as sandproof, windproof, and park trees : It is popular as a place of relaxation for local residents and as a drive spot. The landscape seen from here is beautiful. Kaimon Mountains and Kinko Bay seen from the park ; Sunset over the Satsuma Peninsula, etc.「かごしまよかとこ100選海道の旅」に, 選定. 垂水市教育委員会 2002, 垂水市埋蔵文化財発掘調査報告書6 : 宮ノ前遺跡, 重田遺跡, 新城宮脇, 縄文, 弥生, 古墳時代, 土杭, 縄文土器, 弥生土器, 成川式土器, 縄文時代後期, 晩期, 弥生時代, 古墳時代. Ministry of Agriculture, Forestry and Fisheries Variety registration. Application number 5331 Date of application 1992 / 06 / 15. Registration number 4532 Date of registration 1995 / 06 / 13. This variety is a fixed variety cultivated by mating the strains owned by the applicant, and is a cultivar for pods with finite dwarf, dark green leaves and white flowers, dark green pods, and no streaks. Embryonic axis color is green, elongation and plant type are finite dwarf, plant height is medium, number of main stem nodes is medium, leaf color is dark green, leaflet size is medium, flower color is white. , Width is narrow, degree of bending is straight, beak length is long, shape is lightly bent, no constriction, surface is smooth, cross section is circular, hard and soft is soft, with or without streaks. The ground color is dark green, there is no spot color, the grain size is extremely small, the shape is oblong, there is no type of seed coat spot, the ground color is white, there is no ring color. Medium maturity, medium lodging resistance. Compared to “Compact bean”, the size of the leaflets is large, the degree of pod bending is straightforward, and the length of the pods is long. The surface of the pod is smooth, the length of the pod’s beak is longer than that of “Nerina bean”, the surface of the pod is smooth, the cross section of the pod is circular, etc. It is said that sex is recognized. Plant Breeder’s right has a lifespan of 15 years.The extinction date expires on June 14, 2010. Name of cultivar registrant, SVS Holland (Netherlands, 1601 BM Enkuhayusen), registered cultivar breeder, Jeff Willemsen. We performed forward and reverse mating with “83 / 2423-6” and “83 / 5821-5” as parent lines, and later selected individuals and repeated line selection. In 1987, in the F11 generation, we had the desired characteristics. After confirming that the breeding was completed.
Snow brand seed co., Ltd. is a wholly owned subsidiary of Megmilk Snow Brand Co., Ltd. “ベストクロップキセラインゲン”, After sowing – A mesophyll species that can be harvested in about 62 days. The plant height is around 60 cm, and the leaves are small and have many branches and flowers. The length of the pod is about 15 cm. It is slow to gain weight, and there is little deterioration in quality even with a slight delay-Round pod seed.
In Kagoshima prefecture, it seems that it is shipped almost every year except in the summer, depending on the combination of production areas and varieties. It seems that relay cultivation for about 10 months is carried out throughout the year from open field (mountain) cultivation, open field cultivation, green house cultivation, humidified greenhouse cultivation, open field (mountain) -open field-Greenhouse-heated house-Greenhouse-open field. Xeringen is a Nakate variety that can be harvested about 62 days after sowing, and has no vines with a plant height of about 60 cm. It is a small leaf with a large number of branches and flowers, and is a bright dark green pod that does not lose its color even when it grows large.
Most of the cultivation in Tarumizu City is open-air cultivation, but since the 1975s, greenhouse cultivation has been carried out, and it seems that cultivation that can be shipped almost all year round is being actively carried out. In addition, while promoting cooperation between livestock farmers and cultivated farmers, we are aiming for recycling-type agriculture by establishing environment-friendly agriculture and promoting recycling of organic resources in the region. It seems that it produces and sells various compost.
I hear that the main business is horticulture and livestock farming that take advantage of the warm climate. Among them, it seems that full-time management is carried out centering on facility vegetables such as “green beans” and open-air vegetables such as “snow garden pea”. In addition, Tarumizu City is a base that aims to establish a place for local citizens to interact, promote voluntary activities, improve their lives and improve their health, and promote and develop, revitalize, and develop rural areas that take advantage of the rich natural environment. It seems that there are two locations, the Life Improvement Center and the Sarugajo Revitalization Facility in Tarumizu City. It seems that it can be used for making miso, blistering pastry (a local confectionery, brown sugar-flavored brown steamed bread-like confectionery), and dressing.
