Conducting HADR in the COVID Pandemic
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Nansei Islands Biological Diversity Evaluation Project Report 1 Chapter 1
Introduction WWF Japan’s involvement with the Nansei Islands can be traced back to a request in 1982 by Prince Phillip, Duke of Edinburgh. The “World Conservation Strategy”, which was drafted at the time through a collaborative effort by the WWF’s network, the International Union for Conservation of Nature (IUCN), and the United Nations Environment Programme (UNEP), posed the notion that the problems affecting environments were problems that had global implications. Furthermore, the findings presented offered information on precious environments extant throughout the globe and where they were distributed, thereby providing an impetus for people to think about issues relevant to humankind’s harmonious existence with the rest of nature. One of the precious natural environments for Japan given in the “World Conservation Strategy” was the Nansei Islands. The Duke of Edinburgh, who was the President of the WWF at the time (now President Emeritus), naturally sought to promote acts of conservation by those who could see them through most effectively, i.e. pertinent conservation parties in the area, a mandate which naturally fell on the shoulders of WWF Japan with regard to nature conservation activities concerning the Nansei Islands. This marked the beginning of the Nansei Islands initiative of WWF Japan, and ever since, WWF Japan has not only consistently performed globally-relevant environmental studies of particular areas within the Nansei Islands during the 1980’s and 1990’s, but has put pressure on the national and local governments to use the findings of those studies in public policy. Unfortunately, like many other places throughout the world, the deterioration of the natural environments in the Nansei Islands has yet to stop. -
Border-Crossers and Resistance to US Military Rule in the Ryukyus, 1945-1953
Volume 6 | Issue 9 | Article ID 2906 | Sep 01, 2008 The Asia-Pacific Journal | Japan Focus Border-Crossers and Resistance to US Military Rule in the Ryukyus, 1945-1953 Matthew R. Augustine Border-Crossers and Resistance to US main island groups. Trade barriers with Japan Military Rule in the Ryukyus, 1945-1953 were relaxed in 1950, but the San Francisco Peace Treaty signed in 1951 reaffirmed that Matthew R. Augustine the Ryukyus would remain under US military rule, divided from Japan. By this time, the Sixty-six years after Japan’s annexation of the increasing cross-border interconnections former Ryukyu Kingdom in 1879, in the waning between residents in the Ryukyus and months of the Asia-Pacific War, the American Okinawan and Amamian residents in Japan had military partitioned the Ryukyu Islands from already given rise to an organized movement Japan. The replacement of Okinawa Prefecture calling for reversion to Japanese sovereignty. by US military rule in the Ryukyus from 1945 had profound implications, for residents of the How did the establishment of the military occupied islands. A major repercussion of the government and new postwar borders actually military government’s separation of theaffect the movement of residents within and Ryukyus was the enforced isolation of the four outside of the Ryukyu Islands? Conversely, to main island groups from occupied Japan. The what extent did the resistance of residents in Ryukyuan-Japanese border severed long- the Ryukyus and their effort to overcome their standing administrative and economic links, division and isolation influence the military while restrictive border controls prohibited free government’s border controls and related travel and interaction between the two sides. -
Marine Accident Investigation Report
MARINE ACCIDENT INVESTIGATION REPORT October 3, 2017 Adopted by the Japan Transport Safety Board Chairman Kazuhiro Nakahashi Member Yuji Sato Member Kenkichi Tamura Member Toshiyuki Ishikawa Member Makiko Okamoto Accident type Grounding Date and time Around 06:00 on February 11, 2017 (local time, UTC+9 hours) Location On the southwest coast of the Suwanosejima Island, Toshima-mura, Kagoshima Around 217° true bearing, 2.0 nautical miles (M) from the primary triangulation station of the Suwanosejima Island (approximately 29°36.7'N, 129°41.4'E) Summary of the Accident An oil tanker, SAGAN, with 18 crews, including the master, became unable to start and drifted due to failures in the main engine while heading northeast off the western coast of the Noma Peninsula, Satsuma-shi, Kagoshima. She grounded on the southwest coast of the Suwanosejima Island, Toshima-mura, Kagoshima. SAGAN was completely destroyed with cracks, etc. on the bottom shell, but there were no casualties. Process and Progress of (1) Setup of the Investigation the Investigation The Japan Transport Safety Board appointed an investigator-in-charge and one other marine accident investigator on February 13, 2017 and another marine accident investigator on March 1st to investigate this accident. (2) Collection of Evidence February 13, 14, April 9, May 18, 31, December 1, 2017: Interview April 5-8, 2017: On-site investigation September 6, 7, 2017: Interview and collection of questionnaire The Japan Transport Safety Board entrusted a private analysis company with the analysis of the fuel oil used at the time of the accident. (3) Comments from Parties Relevant to the Cause Comments on the draft report were invited from parties relevant to the cause of accident. -
The Elements of Concealment in Ryukyuan Diplomacy Between Japan and China in Early Modern Times*
The Elements of Concealment in Ryukyuan Diplomacy between Japan and China in Early Modern Times* WATANABE Miki Introduction Figure 1. An Illustration from the “Illustrated Tale of FurugΩri HachirΩ’s Shipwreck” in Ryπkyπ Nendaiki Figure 1 is an illustration which appeared in a chronicle of the Ryukyu Kingdom entitled Ryπkyπ Nendaiki 琉球 代記, published in Japan in 1832, and was inserted into the vignette, “Illustrated Tale of FurugΩri HachirΩ’s 古郡八郞 Shipwreck.”1) The title in the upper right hand corner reads, “FurugΩri HachirΩ shaves the heads (sakayaki 月代) of the Ryukyu- ans [aboard ship].” The term “sakayaki” refers to the standard male Japa- nese hairstyle in the premodern era, in which the head is shaved from the 88 The Memoirs of the Toyo Bunko, 75, 2017 forehead to the tip of the skull and leaving the remaining hairline in the form of a bowed-out crescent. The figure with the Japanese traditional topknot (chonmage 丁髷) and “sakayaki” is probably FurugΩri HachirΩ him- self, and the newly shaven figure in the bow of the ship, the figure being shaved, and the two figures with long hairpins through round topknots and without “sakayaki” are no doubt the Ryukyuans in question. From the pleasant expression of the Ryukyuans, there seems nothing coercive about the barbering. The account accompanying the illustration may be summed up as follows. Once upon a time, a Japanese by the name of HachirΩ went adrift in the ocean and was cast upon the shores of the Ryukyu Islands. The king of Ryukyu ordered four of his subjects to return HachirΩ to Japan, but alas, that ship also went adrift and was cast upon the shores of Ming China. -
Volcanic Geology and Rocks of Nakanoshima, Takara Islands, Kagoshima Prefecture, Japan
Journal of Geosciences, Osaka City University Vol. 32, Art. 1, p. 1-22 March, 1989 Volcanic Geology and Rocks of Nakanoshima, Takara Islands, Kagoshima Prefecture, Japan Masahiro DAISHI* (with 2 Tables 8 Figs.) Abstract One of the Tokara Islands, Nakanoshima, is situated about 207 km south-southwest of Kago shima City, and has a beautiful cone-shaped stratovolcano, Otake. This island is composed mainly of the N akanoshima volcanic rocks, which originated are in this island. The N akanoshima volcanic rocks consist of the Serizaki andesites in the southeast, the Nanatsuyama andesites in the east, the Sakiwaridake andesites in the south, the Shiizaki andesites in the southwest, the Older Otake vol cano in the north, the Nigoriura andesites in the west, the Negamidake andesites in the east and the Younger Otake volcano in ascending order. The Serizaki andesites are formed by many altered andesitic lava flows and a little pyroclastic rocks of two-pyroxene andesite. The fission track age of lava from Serizaki is 1.75 ± 0.22 Ma. The Nanatsuyama andesites are composed of dense altered andesitic lava flows and pyroclastic rocks of two-pyroxene andesite. The Sakiwaridake andesites consist of partially altered lava flows and pyroclastic rocks of olivine-bearing and olivine-free two-pyroxene andesite. The Shiizaki andesites are composed of partially altered lava flows and pyroclastic rocks of two-pyroxene ande site. The Older Otake volcano consists of lava flows and pyroclastic rocks of olivine-bearing and olivine-free two-pyroxene andesite. The Nigoriura andesites are composed of lava flows and pyro clastic rocks of two-pyroxene hornblende andesite. -
Of Japan( Dissertation 全文 )
A revisional study of the spider family Thomisidae (Arachnida, Title Araneae) of Japan( Dissertation_全文 ) Author(s) Ono, Hirotsugu Citation Kyoto University (京都大学) Issue Date 1988-01-23 URL http://dx.doi.org/10.14989/doctor.r6388 Right Type Thesis or Dissertation Textversion author Kyoto University 学位 請 論 文 (主 論 文) 小 野 族 嗣 1灘 灘灘 灘轟 1 . Thomisidae aus Japan. I. Das Genus Tmarus Simon (Arachnida: Araneae). Acta arachnol., 27 (spec. no.): 61-84 (1977). 2 . Thomisidae aus Japan. II. Das Genus Oxytate L.Koch 1878 (Arachnida: Araneae). Senckenb. biol., 58: 245-251 (1978). 3 . Thomisidae aus dem Nepal-Himalaya. I. Das Genus Xysticus C.L.Koch 1835 (Arachnida: Araneae). Senckenb. biol., 59: 267-288 (1978). 4 . Thomisidae aus dem Nepal-Himalaya. II. Das Genus Lysiteles Simon 1895 (Arachnida: Araneae). Senckenb. biol., 60: 91-108 (1979). 5 . Fossile Spinnen aus miozanen Sedimenten des Randecker Maars in SW- Deutschland (Arachnida: Araneae). Jh. Ges. Naturkde. Wurttemberg, 134: 133-141 (1979). (W.Schawaller t 4E1t) 6 . Thomisidae aus Japan. III. Das Genus Lysiteles Simon 1895 (Arachnida: Araneae). Senckenb. biol., 60: 203-217 (1980). 7 . Thomisidae aus dem Nepal-Himalaya. III. Das Genus Stiphropus Gerstaecker 1873, mit Revision der asiatischen Arten (Arachnida: Araneae). Senckenb. biol., 61: 57-76 (1980). 8 . Erstnachweis einer Krabbenspinne (Thomisidae) in dominikanischem Bernstein (Stuttgarter Bernsteinsammlung: Arachnida, Araneae). Stuttgart. Beitr. Naturk., B, (73): 1-13 (1981). 9 . Revision japanischer Spinnen. I. Synonymieeiniger Arten der Familien Theridiidae, Araneidae, Tetragnathidae and Agelenidae (Arachnida: Araneae). Acta arachnol., 30: 1-7 (1981). 10 . Verwandtschaft von Tetrablemma phulchoki Lehtinen 1981 (Araneae: Tetrablemmidae). Senckenb. -
The Role of Tephras in Developing a High-Precision Chronostratigraphy For
*Manuscript Click here to view linked References 1 The role of tephras in developing a high-precision chronostratigraphy for palaeoenvironmental reconstruction and archaeology in southern Kyushu, Japan, since 30,000 cal. BP: an integration Hiroshi Moriwakia*, Naoko Nakamurab, Toshiro Nagasakoc, David J. Lowed, Tomoe Sangawab a Emeritus Professor, Faculty of Law, Economics and Humanities, Kagoshima University, 1-21-30 Korimoto, Kagoshima, Japan 890-0065 b Research Center for Archaeology, Kagoshima University,1-21-24 Korimoto, Kagoshima, Japan 890-8580 c Faculty of Education, Kagoshima University, 1-21-30 Korimoto, Kagoshima, Japan 890-0065 d Earth Sciences, School of Science, Faculty of Science and Engineering, University of Waikato, Private Bag 3105, Hamilton, New Zealand 3204 * Corresponding author Phone: +81-995-67-0453, Fax: +81-995-67-0453 E-mail address: [email protected] (H. Moriwaki) 2 Keywords Tephrochronology, tephras, palaeoenvironment, archaeology, Late Pleistocene, Holocene, southern Kyushu, tephra lattice, INTIMATE Final MS published in Quaternary International online 4 Aug 2015 'Studies of the Quaternary in Japan' QI volume Please cite this article as: Moriwaki, H., et al., The role of tephras in developing a high-precision chronostratigraphy for palaeoenvironmental reconstruction and archaeology in southern Kyushu, Japan, since 30,000 cal. BP: an integration, Quaternary International (2016) 397, 79-92. 3 Abstract Tephras are important for the chronostratigraphy of palaeoenvironmental and archaeological records in southern Kyushu because numerous tephra beds enable these records to be connected and dated precisely using tephrochronology. A regional tephra-based framework or lattice for the past 30,000 calendar (cal.) years is proposed in the style of recent INTIMATE projects elsewhere. -
Japan and a Geography of Islands
Japan and a geography of islands Royle, S. (2016). Japan and a geography of islands. South Pacific Studies, 37(1), 1-28. http://cpi.kagoshima- u.ac.jp/publications/southpacificstudies/archivespst.html#SPS 37.1 Published in: South Pacific Studies Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2017 KURCPI This work is made available online in accordance with the publisher’s policies. Please refer to any applicable terms of use of the publisher. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:29. Sep. 2021 South Pacific Studies Vol.37, No.1, 2016 Japan and A Geography of Islands Royle Stephen A.1,2 1: Visiting Professor (September 2015-March 2016), Kagoshima University Research Center for the Pacific Islands, 1-21-24 Korimoto, Kagoshima, 890-8580 Japan 2: Emeritus Professor of Island Geography, School of Natural and Built Environment, Queen’s University Belfast, Belfast BT7 1NN, Northern Ireland, UK E-mail: [email protected] Abstract This article takes the author’s 2001 book, A Geography of Islands: Small Island Insularity and extracts from it a series of generalisations in both physical and human geography as applied to islands. -
Izu Islands Thrush Akakokko
Bird Research News Vol.3 No.9 2006. 9.13. Izu Islands Thrush Akakokko (Jpn) Turdus celaenops Morphology and classification Nest: They build a bowl-shaped nest in a tree at a height of 0.5-6m above the Classification: Passeriformes Muscicapidae ground (Kiyosu 1978), solidifying Total length: Approx. 230mm Culmen length: 20-23mm fine tree roots, grass stems, moss and Wingspan: ♂ 112.0-124.0mm ♀ 108.0-117.0mm other materials with soil. The nest Tail length: ♂ 82.0-100.8mm ♀ 74.0-89.0mm has an outer diameter of 13-16.5cm, Tarsus length: ♂ 31.9-35.8mm ♀ 32.5-33.7mm an inner diameter of 8-10cm, a depth Photo 2. Eggs and nest of Izu Weight: ♂ 73.7-81.3g ♀ 65.9-93.1g of 5.5-7cm and a height of 9.5-13cm. Islands Thrushes. [Photo by Tanaka Toshihiko] Total length and bill length are quoted from Takano (1990), and Kiyosu (1978), re- Egg: spectively. Other measurements are taken in the banding study at Miyakejima Island. Clutch size is usually three or four eggs, ranging from two to five Appearance: eggs. The egg has a long diameter of approximately 29mm by 21 Male is black from the head toward the chest, and orange on the mm. The egg has red brown flecks on a blue background. abdomen and flank. The bill and the area around the eye are yel- low. The back, shoulders and wing coverts are dark brown. Female Incubation and nestling periods and fledging rate: is somewhat paler than male. Individuals of the Tokara Islands, Incubation period is unknown. -
List of Volcanoes in Japan
Elevation Elevation Sl. No Name Prefecture Coordinates Last eruption Meter Feet 1 Mount Meakan Hokkaidō 1499 4916 43.38°N 144.02°E 2008 2 Mount Asahi (Daisetsuzan) Hokkaidō 2290 7513 43.661°N 142.858°E 1739 3 Lake Kuttara Hokkaidō 581 1906 42.489°N 141.163°E - 4 Lake Mashū Hokkaidō 855 2805 43.570°N 144.565°E - 5 Nigorigawa Hokkaidō 356 1168 42.12°N 140.45°E Pleistocene 6 Nipesotsu-Maruyama Volcanic Group Hokkaidō 2013 6604 43.453°N 143.036°E 1899 7 Niseko Hokkaidō 1154 3786 42.88°N 140.63°E 4050 BC 8 Oshima Hokkaidō 737 2418 41.50°N 139.37°E 1790 9 Mount Rausu Hokkaidō 1660 5446 44.073°N 145.126°E 1880 10 Mount Rishiri Hokkaidō 1721 5646 45.18°N 141.25°E 5830 BC 11 Shikaribetsu Volcanic Group Hokkaidō 1430 4692 43.312°N 143.096°E Holocene 12 Lake Shikotsu Hokkaidō 1320 4331 42.70°N 141.33°E holocene 13 Mount Shiretoko Hokkaidō 1254 4114 44°14′09″N 145°16′26″E 200000 BC 14 Mount Iō (Shiretoko) Hokkaidō 1563 5128 44.131°N 145.165°E 1936 15 Shiribetsu Hokkaidō 1107 3632 42.767°N 140.916°E Holocene 16 Shōwa-shinzan Hokkaidō 731 2400 42.5°N 140.8°E 1945 17 Mount Yōtei Hokkaidō 1898 6227 42.5°N 140.8°E 1050 BC 18 Abu (volcano) Honshū 571 - 34.50°N 131.60°E - 19 Mount Adatara Honshū 1718 5635 37.62°N 140.28°E 1990 20 Mount Akagi Honshū 1828 5997 36.53°N 139.18°E - 21 Akita-Komaga-Take Honshū 1637 5371 39.75°N 140.80°E 1971 22 Akita-Yake-Yama Honshū 1366 4482 39.97°N 140.77°E 1997 23 Mount Asama Honshū 2544 8340 36.24°N 138.31°E 2009 24 Mount Azuma Honshū 1705 5594 37.73°N 140.25°E 1977 25 Mount Bandai Honshū 1819 5968 37.60°N 140.08°E 1888 -
Coral Reefs of Japan
Osumi Islands and Tokara Archipelago 6-1-2 (Map 6-1-2) Province: Kagoshima Prefecture Location: Osumi Islands: ca. 100 km south off Kagoshima City, including 6-1-2-② Tanegashima (Is.), Yakushima (Is.), Kuchinoerabujima (Is.) and Magejima (Is.); Tokara Archipelago: Island chain of 12 islands stretching for ca. 160 km between Yakushima and Amami Oshima (Is.) Air temperature: 19.2˚C (annual average, at Yakushima) Seawater temperature: 24.3˚C (annual average, north off Yakushima Precipitation: 4,358.8 mm (annual average, at Yakushima) Total area of coral communities: 118.0 ha Total length of reef edge: 19km (around Takarajima, Kodakarajima, and Koshima) Protected areas: Kirishima-Yaku National Park: 44% of Yakushima (20,989 ha); Yakushima Wildness Area: 1,219 ha on Yakushima; World Natural Heritage site: 10,747 ha (designated in 1993) on Yakushima; Kurio Marine Park Zone in Yakushima. 6-1-2-① 6-1-2-① 6-1-2-② *“号”on this map means“site”. 0 2km 06 Coral Reefs of Japan Tokara Archipelago, In addition, reef development on Osumi Islands and Tanegashima is limited to the eastern coast, and con- Tokara Archipelago tinuous development of reefs is not readily observable. On Yakushima, hermatypic coral communities can be (Maps 6-1-2-①, ②) observed in a few places around the island, and coral reefs with well-defined reef flats and reef slopes are lim- ited to the north of the island (Nakai and Wada 1983). Tatsuo Nakai, Satoshi Nojima Nakata (1978) reported the existence of Holocene coral reefs in Anbou in southeastern Yakushima. 1 Corals and coral reefs The Tokara Archipelago consists of 12 small islands (the largest of which, Nakanoshima, is only 34 km2) that are scattered over some 160 km between Tanegashima, 1. -
Tourism Around the Kagoshima Prefecture Islands Makoto HAGINO
KAWAI, K., TERADA, R. and KUWAHARA, S. (eds): The Islands of Kagoshima Kagoshima University Research Center for the Pacific Islands, 15 March 2013 Chapter 13 Tourism Around the Kagoshima Prefecture Islands Makoto HAGINO 1. Introduction 2. Tourism spots from geographic features t would be too difficult for a tourist to visit all the in Kagoshima Prefecture Iislands in Kagoshima Prefecture. For example, 2.1. Kumage area: World Heritage site and more than 320 km separate Kagoshima city, the space center site capital of the prefecture, and Yoronjima Is., which he Kumage area consists of Yakushima Is., is at the southern end of the prefecture. Tourists TTanegashima Is., and the Tokara Islands. It therefore can not visit all of the islands at one should be noted that Yakushima Is. was regis- time, and they go to one of four areas; Kumage, tered as a World Natural Heritage site in 1993. Amami, Koshiki, and Nagashima. Since few tour- The Kagoshima Space Center, which has been lo- ists visit Koshiki and Nagashima, we could focus cated on Tanegashima Is. since 1969, is the only on Kumage and Amami for our analysis. space rocket launching site in Japan. On the Tokara In this paper, we describe the distinctive tour- Archipelago, with its faraway solitary islands, the ism areas in the Kagoshima islands and classify traditional life and culture reflective of the southern them by characteristic factors. It is possible that islands of Japan is sustained. this classification will establish new trends of tour- ism in island areas. Among these eco-tourism sites 2.1.1.