The Development of Small Islands in Japan: an Historical Perspective
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. -
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. -
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 -
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. -
An. Sinensis, An. Zindesayi Japonicus, Tp. Bambusa Yaeyamensis, MZ
18 Mosquito Systematics Vol. 15(l) 1983 -I Mosquitoes of the Tokara Archipelago, Japan .2 2 .3 4 Ichiro Miyagi , Takako Toma , Hiroshi Suzuki and Takao Okazawa ABSTRACT: Nineteen mosquito species belonging to nine genera are recorded from Kuchinoshima, Nakanoshima and Takarajima of Tokara Archipelago, Japan: An. sinensis, An. Zindesayi japonicus, Tp. bambusa yaeyamensis, MZ. genurostris, To. yanbarensis, Cq. ochracea, Or. anopheZoides, Ae. nishikmai, Ae. togoi, Ae. albopictus, Ae. fZavopictus downsi, Ae. riversi, Ae. vexans nipponii, Ar. subalbatus, Cx. ryukyensis, Cx. halifaxii, Cx. pipiens quinquefaseiatus, Cx. tritaeniorhynehus and Cx. bitaeniorhynehus. All of them are new records from the islands. Among them 13 species are widely distributed in the Ryukyu Islands and the Palaearctic Japan. Five species, Tp. bambusa yaeyamensis, Ml. genurostris, Ae. nishikawai, Ae. flavopietus downsi and CX. ryukyensis, are an Oriental element and the northernmost records. An. Zindesayi japonicus has not been found in the Ryukyu Archipelago and this is the sourhernmost record of the species. The distribution and habits of the species are also discussed. INTRODUCTION The Tokara Archipelago (Fig. 1), lying in the east China sea between the latitudes of 29-30' N and the longitudes of 129-130' W, is mainly composed of nine small islands: Kuchinoshima (13.30 km*), Nakanoshima (27.54 km*), Gajyajima (4.50 km*), Suwanosejima (22.5 km2), Tairajima (1.99 km2), Akusekijima (7.04 km2), Takarajima (7.0 km2), Kodakarajima (1.17 km2) and Yokoatejima (3.76 km2). The Archipelago represents an extremely interesting area from a zoogeo- graphical standpoint. As is well known, the mosquito fauna of the northern Satsuma Islands (including Tanegashima and Yakushima) are in the same zoological zone as the mainland of Japan which belongs to the Palaearctic Region. -
List of Volcanoes in Japan - Wikipedia, the Free Encyclopedia Page 1 of 8
List of volcanoes in Japan - Wikipedia, the free encyclopedia Page 1 of 8 List of volcanoes in Japan From Wikipedia, the free encyclopedia See also: List of volcanoes This is a list of active and extinct volcanoes in Japan. Contents ■ 1 Hokkaidō ■ 2 Honshū ■ 3 Izu Islands ■ 4 Kyūshū ■ 5 Ryukyu Islands ■ 6 Other ■ 7 References ■ 7.1 Notes ■ 7.2 Sources http://en.wikipedia.org/wiki/List_of_volcanoes_in_Japan 4/7/2011 List of volcanoes in Japan - Wikipedia, the free encyclopedia Page 2 of 8 Hokkaidō Elevation Elevation Last eruption Name Coordinates (m) (ft) Mount Meakan 1499 4916 43.38°N 144.02°E 2006 Mount Asahi (Daisetsuzan) 2290 7513 43.661°N 142.858°E 1739 Mount E 618 2028 41.802°N 141.170°E 1874 Hokkaidō Komagatake 1131 3711 42.061°N 140.681°E 2000 Kutcharo 1000 3278 43.55°N 144.43°E - Lake Kuttara 581 1906 42.489°N 141.163°E - Lake Mashū 855 2805 43.570°N 144.565°E - Nigorigawa 356 1168 42.12°N 140.45°E Pleistocene Nipesotsu-Maruyama Volcanic 2013 6604 43.453°N 143.036°E 1899 Group Niseko 1154 3786 42.88°N 140.63°E 4050 BC Oshima 737 2418 41.50°N 139.37°E 1790 Mount Rausu 1660 5446 44.073°N 145.126°E 1880 Mount Rishiri 1721 5646 45.18°N 141.25°E 5830 BC Shikaribetsu Volcanic Group 1430 4692 43.312°N 143.096°E Holocene Lake Shikotsu 1320 4331 42.70°N 141.33°E 1981 44°14′09″N Mount Shiretoko 1254 4114 145°16′26″E Mount Iō (Shiretoko) 1563 5128 44.131°N 145.165°E 1936 Shiribetsu 1107 3632 42.767°N 140.916°E Holocene Showashinzan 731 2400 42.5°N 140.8°E 1945 Mount Tokachi 2077 6814 43.416°N 142.690°E 1989 42°41′24″N Mount Tarumae 1041 -
Culture and Society in the Islands of Kagoshima Sueo KUWAHARA
KAWAI, K., TERADA, R. and KUWAHARA, S. (eds): The Islands of Kagoshima Kagoshima University Research Center for the Pacific Islands, 15 March 2013 Chapter 1 Culture and Society in the Islands of Kagoshima Sueo KUWAHARA 1. The islands of Kagoshima Islands because these islands remained under US apan extends roughly 4,000 km from northeast military control at this time. Instead, due to the de- Jto southwest along the northeastern coast of layed reversion of these islands to Japan, Special the Eurasian mainland, and comprises five main Development Acts were enacted for these islands islands, Hokkaido, Honshu, Shikoku, Kyushu, in order to reduce the gap in income level between and Okinawa, along with many “rito” - remote (or the mainland and these islands (KUWAHARA 2012). small) islands.1 According to the report The Pres- Kagoshima Prefecture, which is located in the ent State of Maritime Security, published by the southern end of Kyushu, stretches for 600 km from Japan Coast Guard in 1987, “rito” is defined as its northernmost to southernmost end. Within the having a coast of more than 100 m in circumfer- distance, there are 605 islands including 28 inhab- ence. According to this definition, the Japanese ited ones. The population of Kagoshima Prefecture archipelago consists of 6,852 islands, of which is about 1.8 million, while that of all the islands in 421 are inhabited and more than 90 % uninhabited Kagoshima is about 180,000, which is about 10 % (Nihon Rito Center 1996: 1-2). of the prefectural population. Thus, Kagoshima is Despite ranking -
Faculty of Engineering
ISSN 2186-1714 KAGOSHIMA UNIVERSITY NEWSLETTER Spring 2018 Special Issue 学部紹介 特集 Faculty of Engineering KAGOSHIMA UNIVERSITY Contents KAGOSHIMA UNIVERSITY Special Issue NEWSLETTER No.15 Faculty of Engineering, P.1 Graduate School of Engineering Published by International Community Kagoshima University Global Initiative Centre 国際交流 1-21-30, Korimoto, Kagoshima National Institute of Technology Japan, 890-8580 P.9 email: Karnataka (NITK), India [email protected] Dhruva Narayana Katpady Board Editor Sameshima Sōichirō Editor in Chief International Programme Steve Cother The GOES Programme Contributing Editors Nakatani Sumie P.10 Bo Causer, Specially Appointed Assistant Professor, Morita Toyoko Global Development Office, Graduate School of Science Fukutomi Shō and Engineering Design & Printing Shibundo Co. Ltd. KUToday is a biannual publication to Discover KU present information about Kagoshima University to a wider What artifacts can tell us international audience. Each edition P.12 will feature one faculty for about our ancestors prospective overseas students as well as other topics such as educational Shinzato Takayuki, Research Associate, Research Centre programmes, research and alumni for Archaeology information. Some articles are translations from the Japanese-language publication, Kadai Journal, upon which KU Today 鹿大 is loosely based. Any comments or suggestions about KUToday will be Campus Walk Around warmly received. 見て P.14 あ Division of Instrumental Analysis PDF files on KUToday can be る Sawada Tsuyoshi, Associate Professor, Research Support Centre downloaded from https://www.kagoshima-u.ac.jp/en/ 紀 about/newsletter.html A Note on Names Following convention East Asian names appearing in KU Today are written family name followed by P.16 Faces and Snapshots given name. -
Volcanic Island Chain South of Kyushu, Japan Kisei KINOSHITA and Masaya SAKAMOTO
KAWAI, K., TERADA, R. and KUWAHARA, S. (eds): The Islands of Kagoshima Kagoshima University Research Center for the Pacific Islands, 15 March 2013 Chapter 21 Volcanic Island Chain South of Kyushu, Japan Kisei KINOSHITA and Masaya SAKAMOTO 1. Introduction etrating sedimentary layers. he Nansei (Ryukyu) Islands south of Kyushu Tincludes many insular volcanoes, as shown in 2. Satsuma-Iojima and Takeshima Islands Fig. 1, forming a volcanic island chain extending ap- ow let us start our “Volcano tour,” moving proximately 380 km from Satsuma-Iojima Is. (north) Nnorth to south. Two small islands, Satsuma- to Io-Torishima Is. (south). The northernmost vol- Iojima Is. and Takeshima Is. (shown in Fig. 3) are lo- cano stands at the rim of Kikai caldera, which was cated 50 km south of the mouth of Kagoshima Bay. the source of the most catastrophic eruption in Japan About 7,300 years ago, the Kikai-Akahoya eruption during the last 10,000 years. Each of the others has occurred here, leaving the submerged Kikai caldera. specific properties and histories almost unknown Pyroclastic flows, composed of hot lava fragments because of their geographical isolation. A brief in- and gases, travelled over the sea to Yakushima Is., troductory overview is given here, describing the Tanegashima Is. and other nearby islands, and cov- geoscientific character of the small volcanic islands. ered with lithic fragments such as pumice, lapilli and Let us examine the tectonic setting of these is- ash. They further reached the Osumi and Satsuma land volcanoes. They belong to the West Japan Vol- peninsulas of mainland Kyushu, wiping out the canic Zone, together with Kaimondake, Sakurajima early Jomon culture.