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Niigata Port Tourist Information
Niigata Port Tourist Information http://www.mlit.go.jp/kankocho/cruise/ Niigata Sushi Zanmai Kiwami The Kiwami ("zenith") platter is a special 10-piece serving of the finest sushi, offered by participating establishments in Niigata. The platter includes local seasonal offerings unavailable anywhere else, together with uni (sea urchin roe), toro (medium-fat tuna), and ikura (salmon roe). The content varies according to the season and sea conditions, but you can always be sure you will be eating the best fish of the day. Location/View Access Season Year-round Welcome to Niigata City Travel Guide Related links https://www.nvcb.or.jp/travelguide/en/contents/food/index_f ood.html Contact Us[City of Niigata International Tourism Division ] TEL:+81-25-226-2614 l E-MAIL: [email protected] l Website: http://www.nvcb.or.jp/travelguide/en/ Tarekatsu Donburi A famous Niigata gourmet dish. It consists of a large bowl of rice(donburi) topped with a cutlet fried in breadcrumbs, cut into thin strips, and mixed with an exotic sweet and sour sauce. Location/View Access Season Year-round Welcome to Niigata City Travel Guide Related links https://www.nvcb.or.jp/travelguide/en/contents/food/index_f ood.html Contact Us[City of Niigata International Tourism Division ] TEL:+81-25-226-2614 l E-MAIL: [email protected] l Website: http://www.nvcb.or.jp/en/ Hegi-soba noodles "Hegi soba" is soba that is serviced on a wooden plate called "Hegi". It is made from seaweed called "funori" and you can enjoy a unique chewiness as well as the ease with whici it goes down your throat. -
TOBU BUS Routes in Kashiwa Area As of Feb. 2012
TOBU BUS Routes in Kashiwa Area As of Feb. 2012 ◎JR Kashiwa Station IPMU ( about 30 minutes ) 280 Yen (one way) 系統番号 Number 起点 From / To 経由地 Other Stops 起点 To/From 西 01 柏 駅 西 口 東大前 IPMU ― 国立がん研究センター 柏 ― Nishi- Kashiwa-Eki Nishi-Guchi Todai Mae Kokuritsu-Gan-Kenkyu-Center Kashiwa 01 (Kashiwa Station West Exit) (Tokyo university) (National Cancer center) IPMU 柏 駅 西 口 税関研修所 国立がん研究センター 柏 44 ― Kashiwa-Eki Nishi-Guchi ― Zeikan Kenshu-jo Kokuritsu-Gan-Kenkyu-Center Kashiwa 44 (Kashiwa Station West Exit) (Customs Training Institute) (National Cancer center) IPMU ◎TSUKUBA EXPRESS Kashiwanoha Campus station IPMU ( about 10 minutes ) 160 Yen (one way) 西 柏の葉キャンパス駅西口 国立がん研究センター 流山おおたかの森駅東口 03 柏 IPMU ― ― Nishi- Kashiwanoha Campus-Eki Nishi-Guchi Kokuritsu-Gan-Kenkyu-Center Nagareyama-otakanomori-Eki Higashi-Guchi Kashiwa 03 (Kashiwanoha Campus Station West Exit) (National Cancer center) (Nagareyama-otakanomori Station East Exit) 西 柏の葉キャンパス駅西口 国立がん研究センター 江戸川台駅東口 04 柏 IPMU Nishi- Kashiwanoha Campus-Eki Nishi-Guchi Kokuritsu-Gan-Kenkyu-Center Edogawadai -Eki Higashi-Guchi Kashiwa 04 (Kashiwanoha Campus Station West Exit) (National Cancer center) (Edogawadai Station East Exit) 西 柏の葉キャンパス駅西口 東大前 IPMU 江戸川台駅東口 10 柏 ― ― Kashiwanoha Campus-Eki Nishi-Guchi Todai Mae Edogawadai -Eki Higashi-Guchi Nishi- Kashiwa 10 (Kashiwanoha Campus Station West Exit) (Tokyo university) (Edogawadai Station East Exit) IPMU General Research Bldg. (Kashiwa Research Complex) Please look closely to the bus number. 西柏 and 柏 are two different busses. 西 (Ex. 02 will take you to the -
Kinematic Reconstruction of the Caribbean Region Since the Early Jurassic
Earth-Science Reviews 138 (2014) 102–136 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Kinematic reconstruction of the Caribbean region since the Early Jurassic Lydian M. Boschman a,⁎, Douwe J.J. van Hinsbergen a, Trond H. Torsvik b,c,d, Wim Spakman a,b, James L. Pindell e,f a Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands b Center for Earth Evolution and Dynamics (CEED), University of Oslo, Sem Sælands vei 24, NO-0316 Oslo, Norway c Center for Geodynamics, Geological Survey of Norway (NGU), Leiv Eirikssons vei 39, 7491 Trondheim, Norway d School of Geosciences, University of the Witwatersrand, WITS 2050 Johannesburg, South Africa e Tectonic Analysis Ltd., Chestnut House, Duncton, West Sussex, GU28 OLH, England, UK f School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff CF10 3YE, UK article info abstract Article history: The Caribbean oceanic crust was formed west of the North and South American continents, probably from Late Received 4 December 2013 Jurassic through Early Cretaceous time. Its subsequent evolution has resulted from a complex tectonic history Accepted 9 August 2014 governed by the interplay of the North American, South American and (Paleo-)Pacific plates. During its entire Available online 23 August 2014 tectonic evolution, the Caribbean plate was largely surrounded by subduction and transform boundaries, and the oceanic crust has been overlain by the Caribbean Large Igneous Province (CLIP) since ~90 Ma. The consequent Keywords: absence of passive margins and measurable marine magnetic anomalies hampers a quantitative integration into GPlates Apparent Polar Wander Path the global circuit of plate motions. -
A Dangling Slab, Amplified Arc Volcanism, Mantle Flow and Seismic Anisotropy in the Kamchatka Plate Corner
AGU Geodynamics Series Volume 30, PLATE BOUNDARY ZONES Edited by Seth Stein and Jeffrey T. Freymueller, p. 295-324 1 A Dangling Slab, Amplified Arc Volcanism, Mantle Flow and Seismic Anisotropy in the Kamchatka Plate Corner Jeffrey Park,1 Yadim Levin,1 Mark Brandon,1 Jonathan Lees,2 Valerie Peyton,3 Evgenii Gordeev ) 4 Alexei Ozerov ,4 Book chapter in press with "Plate Boundary Zones," edited by Seth Stein and Jeffrey Freymuller Abstract The Kamchatka peninsula in Russian East Asia lies at the junction of a transcurrent plate boundary, aligned with the western Aleutian Islands, and a steeply-dipping subduction zone with near-normal convergence. Seismicity patterns and P-wave tomography argue that subducting Pacific lithosphere terminates at the Aleutian junction, and that the downdip extension (>150km depth) of the slab edge is missing. Seismic observables of elastic anisotropy (SKS splitting and Love-Rayleigh scattering) are consistent \Vith asthenospheric strain that rotates from trench-parallel beneath the descending slab to trench-normal beyond its edge. Present-day arc volcanism is concentrated near the slab edge, in the Klyuchevskoy and Sheveluch eruptive centers. Loss of the downdip slab edge, whether from thermo-convective or ductile instability, and subsequent "slab-window" mantle return flow is indicated by widespread Quaternary volcanism in the Sredinny Range inland of Klyuchevskoy and Sheveluch, as well as the inferred Quaternary uplift of the central Kamchatka depression. The slab beneath Klyuchevskoy has shallower dip (35°) than the subduction zone farther south (55°) suggesting a transient lofting of the slab edge, either from asthenospheric flow or the loss of downdip load. -
SAITO HAJIME/ Embracing Hiroshima
EMBRACING HIROSHIMA Saito Hajime Abstract: The main purpose of this paper is to examine an episode in John Hersey’s book Hiroshima (1946) and the occupational policy of General Headquarters (GHQ), the organization which administered the defeated land of Japan during the Occupied Era (1945-1952). It is John Dower and his readers that should be interested in the episode because in his seminal work, Embracing Defeat (1999), Dower touches on Hiroshima in terms of the GHQ’s censorship of Japanese writings about the atomic bombs dropped on the cities of Hiroshima and Nagasaki. What matters most in terms of the episode is that in 1951 the GHQ allowed copies of Hiroshima to be imported from the United States to be sold in Japan. In the same year some of Japan’s university professors were invited to teach it in their English classes. A controversy over the use of this work as a textbook arose among Japanese university teachers of English, and Rintaro Fukuhara and Takashi Nozaki exemplified these opinions. Their contrasting views on the text suggest the ways in which intellectuals or academics can or cannot cope under the pressure of a hegemonic cultural power.1 The purpose of this paper is to show an episode that John Dower, the author of Embracing Defeat: Japan in the Wake of World War II (1999), should be interested in. It examines John Hersey’s famous non-fiction book Hiroshima (1946), as well as the occupational policy of the General Headquarters (GHQ’s) SAITO HAJIME, Associate Professor, Faculty of Humanities and Social Sciences, University of Tsukuba (Japan). -
Fault Model of the 12Th Century Southwestern Hokkaido Earthquake
Ioki et al. Earth, Planets and Space (2019) 71:54 https://doi.org/10.1186/s40623-019-1034-6 FULL PAPER Open Access Fault model of the 12th century southwestern Hokkaido earthquake estimated from tsunami deposit distributions Kei Ioki1* , Yuichiro Tanioka2, Gentaro Kawakami3, Yoshihiro Kase3, Kenji Nishina3, Wataru Hirose3, Kei’ichi Hayashi3 and Ryo Takahashi3 Abstract Tsunami deposits were collected along the coast of southwestern Hokkaido and Okushiri Island, northern Japan. The distribution of these deposits suggested that large earthquakes and tsunamis have repeatedly occurred of south- western Hokkaido. Along the southern coast of Okushiri Island, fve tsunami sand/gravel layers have been deposited during the last 3000 years. The latest was deposited by the 1741 Oshima–Oshima landslide tsunami and the second by the 12th century tsunami. The later tsunami was probably generated by a large earthquake because submarine seismo-turbidites with similar age exist in the region and a large inland landslide had occurred in Okushiri Island in approximately the 12th century. The ages of paleo-tsunami events prior to the 12th century are 1.5–1.6, 2.4–2.6, 2.8–3.1 ka. In this study, a fault model of the 12th century earthquake was estimated by comparing tsunami deposit distributions and calculated tsunami inundation areas at fve sites in Okushiri Island and Hiyama region. Fault model F17, a submarine active fault in the Japan Sea near Oshima–Oshima, is a probable source for this tsunami. Numerical simulation of the tsunami was performed based on fault model F17; we modifed the fault parameters (length and slip amount) from the original model to explain tsunami deposit distributions. -
Geography & Climate
Web Japan http://web-japan.org/ GEOGRAPHY AND CLIMATE A country of diverse topography and climate characterized by peninsulas and inlets and Geography offshore islands (like the Goto archipelago and the islands of Tsushima and Iki, which are part of that prefecture). There are also A Pacific Island Country accidented areas of the coast with many Japan is an island country forming an arc in inlets and steep cliffs caused by the the Pacific Ocean to the east of the Asian submersion of part of the former coastline due continent. The land comprises four large to changes in the Earth’s crust. islands named (in decreasing order of size) A warm ocean current known as the Honshu, Hokkaido, Kyushu, and Shikoku, Kuroshio (or Japan Current) flows together with many smaller islands. The northeastward along the southern part of the Pacific Ocean lies to the east while the Sea of Japanese archipelago, and a branch of it, Japan and the East China Sea separate known as the Tsushima Current, flows into Japan from the Asian continent. the Sea of Japan along the west side of the In terms of latitude, Japan coincides country. From the north, a cold current known approximately with the Mediterranean Sea as the Oyashio (or Chishima Current) flows and with the city of Los Angeles in North south along Japan’s east coast, and a branch America. Paris and London have latitudes of it, called the Liman Current, enters the Sea somewhat to the north of the northern tip of of Japan from the north. The mixing of these Hokkaido. -
The Stoloniferous Octocoral, Hanabira Yukibana, Gen. Nov., Sp
Contributions to Zoology 88 (2019) 54-77 CTOZ brill.com/ctoz The stoloniferous octocoral, Hanabira yukibana, gen. nov., sp. nov., of the southern Ryukyus has morphological and symbiont variation Yee Wah Lau Molecular Invertebrate Systematics and Ecology Laboratory, Graduate School of Engineering and Science, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa 903-0123, Japan [email protected] Frank R. Stokvis Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA, Leiden, The Netherlands Yukimitsu Imahara Wakayama Laboratory, Biological Institute on Kuroshio, 300-11 Kire, Wakayama-shi, Wakayama 640-0351, Japan James D. Reimer Molecular Invertebrate Systematics and Ecology Laboratory, Graduate School of Engineering and Science, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa 903-0123, Japan Tropical Biosphere Research Center, University of the Ryukyus, 1 Senbaru, Nishihara, Okinawa 903-0123, Japan Abstract Stoloniferan octocorals (Cnidaria: Anthozoa: Octocorallia: Alcyonacea) are a relatively unexplored fauna in the Ryukyus (southern Japan), known to be a tropical marine region of high biodiversity and endemism of species. Specimens of stoloniferous octocorals were collected during fieldwork along the coasts of two islands (Okinawa and Iriomote) in the Okinawa Prefecture. Despite their phenotypic polyp variation, this study shows their morphological and molecular uniqueness, leading to the description of a new genus with a single species: Hanabira yukibana, gen. nov., sp. nov. They are placed within the Clavulariidae and form a sister clade basally to the genus Knopia Alderslade & McFadden, 2007 and species of Clavularia Blainville, 1830. The polyps of this new species show morphological variation in both shape and sclerite density, but there is conformity in the typical overall petal shaped tentacles, which have fused pinnules (pseudopinnules). -
Effects of Constructing a New Airport on Ishigaki Island
Island Sustainability II 181 Effects of constructing a new airport on Ishigaki Island Y. Maeno1, H. Gotoh1, M. Takezawa1 & T. Satoh2 1Nihon University, Japan 2Nihon Harbor Consultants Ltd., Japan Abstract Okinawa Prefecture marked the 40th anniversary of its reversion to Japanese sovereignty from US control in 2012. Such isolated islands are almost under the environment separated by the mainland and the sea, so that they have the economic differences from the mainland and some policies for being active isolated islands are taken. It is necessary to promote economical measures in order to increase the prosperity of isolated islands through initiatives involving tourism, fisheries, manufacturing, etc. In this study, Ishigaki Island was considered as an example of such an isolated island. Ishigaki Island is located to the west of the main islands of Okinawa and the second-largest island of the Yaeyama Island group. Ishigaki Island falls under the jurisdiction of Okinawa Prefecture, Japan’s southernmost prefecture, which is situated approximately half-way between Kyushu and Taiwan. Both islands belong to the Ryukyu Archipelago, which consists of more than 100 islands extending over an area of 1,000 km from Kyushu (the southwesternmost of Japan’s four main islands) to Taiwan in the south. Located between China and mainland Japan, Ishigaki Island has been culturally influenced by both countries. Much of the island and the surrounding ocean are protected as part of Iriomote-Ishigaki National Park. Ishigaki Airport, built in 1943, is the largest airport in the Yaeyama Island group. The runway and air security facilities were improved in accordance with passenger demand for larger aircraft, and the airport became a tentative jet airport in May 1979. -
Local Dishes Loved by the Nation
Sapporo 1 Hakodate 2 Japan 5 3 Niigata 6 4 Kanazawa 15 7 Sendai Kyoto 17 16 Kobe 10 9 18 20 31 11 8 ocal dishes Hiroshima 32 21 33 28 26 19 13 Fukuoka 34 25 12 35 23 22 14 40 37 27 24 29 Tokyo loved by 41 38 36 Nagoya 42 44 39 30 Shizuoka Yokohama 43 45 Osaka Nagasaki 46 Kochi the nation Kumamoto ■ Hokkaido ■ Tohoku Kagoshima L ■ Kanto ■ Chubu ■ Kansai 47 ■ Chugoku ■ Shikoku Naha ■ Kyushu ■ Okinawa 1 Hokkaido 17 Ishikawa Prefecture 33 Okayama Prefecture 2 Aomori Prefecture 18 Fukui Prefecture 34 Hiroshima Prefecture 3 Iwate Prefecture 19 Yamanashi Prefecture 35 Yamaguchi Prefecture 4 Miyagi Prefecture 20 Nagano Prefecture 36 Tokushima Prefecture 5 Akita Prefecture 21 Gifu Prefecture 37 Kagawa Prefecture 6 Yamagata Prefecture 22 Shizuoka Prefecture 38 Ehime Prefecture 7 Fukushima Prefecture 23 Aichi Prefecture 39 Kochi Prefecture 8 Ibaraki Prefecture 24 Mie Prefecture 40 Fukuoka Prefecture 9 Tochigi Prefecture 25 Shiga Prefecture 41 Saga Prefecture 10 Gunma Prefecture 26 Kyoto Prefecture 42 Nagasaki Prefecture 11 Saitama Prefecture 27 Osaka Prefecture 43 Kumamoto Prefecture 12 Chiba Prefecture 28 Hyogo Prefecture 44 Oita Prefecture 13 Tokyo 29 Nara Prefecture 45 Miyazaki Prefecture 14 Kanagawa Prefecture 30 Wakayama Prefecture 46 Kagoshima Prefecture 15 Niigata Prefecture 31 Tottori Prefecture 47 Okinawa Prefecture 16 Toyama Prefecture 32 Shimane Prefecture Local dishes loved by the nation Hokkaido Map No.1 Northern delights Iwate Map No.3 Cool noodles Hokkaido Rice bowl with Tohoku Uni-ikura-don sea urchin and Morioka Reimen Chilled noodles -
Japan Earthquake and Tsunami Update Friday, April 1, 2011 Overview
Japan Earthquake and Tsunami Update Friday, April 1, 2011 Note: New content has been inserted in red, italicized, bold font. Overview A powerful 9.0-magnitude earthquake hit Japan on March 11 at 1446 local time (0546 GMT), unleashing massive tsunami waves that crashed into Japan’s northeastern coast of Honshu, the largest and main island of Japan, resulting in widespread damage and destruction. According to the Government of Japan (GoJ), as of Friday (April 1), 11,734 people are confirmed dead and 16,375 people are reported to be missing. (Kyodo, Reuters, April 1) There are no new figures for the number of injured, but the UN reported last week that 2,766 people 1 were injured. Casualty numbers are likely to increase as emergency teams continue to reach and assess affected areas. The earthquake sparked widespread tsunami warnings across the Pacific. According to the US Geological Survey (USGS), the shallow quake struck at a depth of six miles (10 km) (20 km deep according to Japan’s Meteorological Agency), around 80 miles (125 km) off the eastern coast of Japan, and 240 miles (380 km) northeast of Tokyo. Key Concerns: • There are more than 166,000 evacuees. • UN says priority needs remain: fuel, prefabricated housing, clothing and medicine. Request for international assistance Japan has asked for international help to deal with the disaster and has so far received offers of assistance from 134 countries and 33 international organizations. It has accepted relief items from 24 countries to date. According to OCHA, the GoJ says the need for further international assistance is limited and any support should be in accordance with the GoJ’s criteria. -
Kashiwa-No-Ha Smart City
Kashiwa-no-ha Smart City Mitsui Fudosan Co., Ltd. 1. Location Location 25 km from central Tokyo 27 minutes by Tsukuba Express from Akihabara Tokyo Access Airport Access Tokyo: 30 min Haneda: 58 min Akihabara: 27 min by Train Narita: 62 min by Train Roppongi: 50 min Haneda (54km): 60 min by Car Narita (48km): 60 min Note: Excluding transfer and waiting times Area under Development Kashiwa-no-ha Campus To Tsukuba Kashiwa Interchange of Joban Expressway Kashiwa-no-ha Park A land readjustment project area Tsukuba Express covering roughly 273 hectares and with a planned population of 26,000 Developed from scratch Leveraging advanced knowledge Kashiwa-no-ha Campus Station and technologies A social experiment in which residents are participating To Akihabara The Transitional Process of Community Building 2000 2001 2003 2005 2006 Opening of Center for Opening of Urban Opening of Opening of Closing of the Environment Health Opening of the Design Center LaLaport University of Tokyo Mitsui Kashiwa and Field Sciences, Tsukuba Kashiwa-no-ha Kashiwanoha Kashiwa Campus Golf Club Chiba University Express Line (UDCK) (Approx. 160 shops) Commencement of the Land Readjustment Project 2008 2009 2011 2012 2014 Kashiwa-no-ha Recognized as Completion of Park City Opening of Gate Square, International Completion of Park City “Comprehensive Kashiwanoha Campus The Core of the Ekimae Campus Town Kashiwanoha Campus Special Zone” and Second Avenue (Station-front) Initiative First Avenue “Environmental (880 Housing Units) Town Center (977 Housing Units) Future City” 1st Stage - The Completion of the Initial Period 2nd Stage Kashiwa-no-ha Campus Station Area in 2014 Kashiwa Interchange of Joban Expressway University of Tokyo Toyofuta Industrial Park Kashiwanoha Park Konbukuro Pond Park Government research center Kashiwa-no-ha High School Chiba STAGE Ⅱ University Nibangai (880 units) Tsukuba Express Line LaLaport KASHIWANOHA Gate Square STAGE Ⅰ Route No.