Highlights of Hokkaido
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Cherry Blossom Viewing – Hokkaido Style Jan
12 Information Rebun● Wakkanai ● www.hokkaido-pedia.jpwww.hokkaido-pedia.jp Rishiri ● HOKKAIDO 2012 China Southern Airlines Hospitals http://www.cs-air.jp/ ●Mombetsu Sapporo City General Hospital Takasu ● Sakhalin Airlines http://www.city.sapporo.jp/city/english/index.html ●Abashiri Asahikawa ● Tokoro ● http://www.satairlines.ru/index.php ●Shiretoko Hokkaido University Hospital Otaru Eva Air http://www.huhp.hokudai.ac.jp/english/med01.html 2 ● http://www.evaair.com/html/b2c/english/ February Niseko ● ●Sapporo Sapporo Medical University Hospital Chitose ● Jin Air http://web.sapmed.ac.jp/byoin/ Obihiro ● http://www.jinair.com/Language/ENG/ Library Eastar Air Hakodate ● http://www.eastarjet.com/book/index.htm?lang=en Sapporo Chuo Library http://www.city.sapporo.jp/toshokan/english/english.html International Airport Foreign Currency Exchange Information New Chitose Airport http://www.new-chitose-airport.jp/en/ North Pacific Bank Police http://www.hokuyobank.co.jp/ Trains 110 Hokkaido Bank JR Hokkaido http://www.hokkaidobank.co.jp/service/foreigncash/ Emergency http://www2.jrhokkaido.co.jp/global/index.html index.html 119 JR Information Desk Post Office JR Sapporo Station West Exit (8:30 – 19:00) Tourist Information New Chitose Airport Station (8:30 – 19:00) Sapporo Central Post Office http://www.japanpost.jp/ Sapporo Buses http://www.welcome.city.sapporo.jp/english/access/ International Telephone information.html Hokkaido Chuo Bus http://www.chuo-bus.co.jp/sightseeing.en/ http://hokkaido.jp.currentlocaltimes.com/dialingcode.html Hokkaido http://en.visit-hokkaido.jp/ -
Northern Islands of Hokkaido by Bike
northern islands of hokkaido by bike trip highlights Starts from Abashiri Memanbetsu on the east coast of Hokkaido Finishes in Wakkanai, Japan’s northern-most city Cycle-friendly rural roads and cycling paths Cycling in Rishiri Island, undiscovered cycling paradise Hiking in Rebun Island, home to many rare alpine plants Staying at traditional Japanese inns with hot springs on site Experience Hokkaido’s fresh seafood oriental cuisines Optional cycle tour in the ancient city of Kyoto Trip Duration 7 days Trip Code: NOH Grade Moderate level Activities 5 day cycle Accommodation 6 nights motel/hotel accommodation Kia Ora from Adventure South why travel with Adventure South? Thank you for your interest in our Northern Islands of Hokkaido By “Small Groups, Great Guides, Superb Holidays.” Bike adventure. It’s a superb adventure and we hope you can join us. This comment encapsulates an Adventure South active holiday in Adventure South has been operating active holidays throughout New Japan. The phrase was not born from a long and tortuous strategic Zealand since 1992 and Japan since 2008. Thanks to our experience planning process, it came from a client review! We could not have we’re confident to say that we offer the very best travel itineraries said it any better. Our client feedback also confirms that what helps available in New Zealand and Japan today. make our holidays different are the quality of our professional guides. An Adventure South holiday aims to take you beyond the more They share their humour, compassion and wilderness experience to popular and busy trails to provide you with a truly unique Japanese ensure that you have a great vacation and the right degree of personal wilderness experience. -
Baikal–Hokkaido Archaeology Project Contributions to Research Dissemination and Communication
Baikal–Hokkaido Archaeology Project Contributions to Research Dissemination and Communication This document lists all publications, presentations and other dissemination contributions by BHAP members from 2011– 2014. Publications are categorized by year, type and listed by author (alphabetical order), with BHAP members underlined. Detailed accounts of BHAP workshops, business meetings and conferences are listed separately and found on pages 23-32. 2014 REFEREED CONTRIBUTIONS Books edited works (4 in total) Cummings V, Jordan P and M. Zvelebil. (eds.) 2014. The Oxford Handbook of the Archaeology and Anthropology of Hunter- Gatherers. Oxford: Oxford University Press. Jordan P, Gillam JC, Uchiyama J. (eds.). 2014. Neolithization of Cultural Landscapes in East Asia. Journal of World Prehistory, Special Issue, Volume 27, No 3–4 (7 papers). Okada M. and Kato H. (eds.) 2014. Indigenous Heritage and Tourism: Theories and Practices on Utilizing the Ainu Heritage. Center for Ainu and Indigenous Studies, Hokkaido University, Sapporo. Wagner M, Jin G, Tarasov PE. (eds.) 2014. The Bridging Eurasia Research Initiative: Modes of mobility and sustainability in the palaeoenvironmental and archaeological archives from Eurasia. Quaternary International, Special Issue, Volume 348, 266 pages. Book chapters (8 in total) Kubo D, Tanabe CH, Kondo O, Ogihara N, Yogi A, Murayama S, Ishida H. Cerebellar size estimation from endocranial measurements: an evaluation based on MRI data. In: Akazawa T, Ogihara N, Tamabe CH, Terashima H. (eds.) Dynamics of Learning in Neanderthals and Modern Humans, Volume 2, Cognitive and Physical Perspectives, Replacement of Neanderthals by Modern Humans Series, Tokyo: Springer Japan, 209-215, 2014. Jordan P and V. Cummings. 2014. Introduction. In: Cummings, V, Jordan P and M. -
Rishiri-Rebun-Sarobetsu National Park
Ministry of the Environment Ministry of the Environment 2 3 For Rebun Island Cape Noshappu (Kafuka) Soya Bay Todojima Island For Rishiri Island (Oshidomari) Cape Sukoton Cape Kaneta Wakkanai Wakkanai Port Wakkanai Airport Funadomari Minamiwakkanai Cape Gorota Port Masuporo River Lake Kushu Onuma Cape Sukai Wakkanai City Bakkai 40 Koetoi River Rebun-cho Bakkai Port Mt. Rebun Kohonenuma Swamp Yuchi Kabutonuma Rebun Falls Jizoiwa Rock Kabutonuma Swamp For Wakkanai Kafuka Port Soya Line Momoiwa Rock Wakkanai Nekoiwa Rock Rebun Island port Cape For Rishiri Island (Oshidomari) Junsainuma Swamp Mt. Rebun Noshappu Wakkanai Kafuka For Rishiri Island Port Tokumitsu (Kutsugata) Soya Line Toyotomi-cho Oshidomari Port For Rebun Island (Kafuka) Sarobetsu Plain Rebun Rishiri Channel Cape Fuji For Wakkanai Naganuma Channel Kutsugata Mt. Rishiri Toyotomi Port Rebun ChannelRishiri Airport Sarobetsu Visitor Center Rishiri Island Oshidomari Port Nihonkai Ororon Line Sarobetsu River Cape Nozuka Penkenuma Mt. Pon Himenuma Swamp Swamp The Sea of Japan For Rebun Island (Kafuka) Kanrosensui Spring Sarobetsu Plain Kannoniwa Rock Pankenuma Rishirifuji-cho Swamp Shimonuma Tanetomi Marsh Kutsugata Port Horonobe-cho Cape Kutsugata Park Mikaeridai Park Observatory Horonobe Horonobe Visitor Center 40 Mt. Rishiri Rishiri Channel Teshio River Kamihoronobe Rishiri-cho Ishizaki Jinmeniwa Rock Minamihoronobe Negumanoiwa Rock Lighthouse Kitanoitsukushima- 232 bentengu Shrine Oniwaki Port Yasuushi Daisetsuzan Reiho Spring National Park Numaura Marsh Otadomarinuma Swamp Minamihama Marsh Numaura Observatory Senhoshi Coast Cape Senhoshi Park Teshio-cho 4 5 6 7 9 10 11 15 16 17 20 21 24 25 26 27. -
Southern Asian Dolly Varden Charr, Salvelinus Curilus on the Higashi
利尻研究 Rishiri Studies (40): 13–20, March 2021 Southern Asian Dolly Varden Charr, Salvelinus curilus on the Higashi-Nodottomari River in Rishiri Island ―Along with a review of the distribution of the charr in northern Hokkaido― 1) 2) Genki Sahashi * and Kentaro Morita 1)Salmon Research Department, Fisheries Resources Institute, Japan Fisheries Research and Education Agency, 2-2 Nakanoshima, Toyohira-ku, Sapporo, 062-0922 Japan 2)Uryu Experimental Forest, Field Science Center for Northern Biosphere, Hokkaido University, Moshiri, Horokanai, Hokkaido 074-0741 Japan Abstract. Southern Asian Dolly Varden charr, Salvelinus curilus (syn. S. malma krascheninnikovi), is a salmonid fish and distributed in northeastern Asia. Rishiri Island represents the northern edge of the distri- bution range for the charr in Japan, and several studies have reported their presence. However, no basic ecological information, such as body size distribution and population densities, have been reported for the charr population of Rishiri Island. In this paper, we report the body size distribution and population density of the Southern Asian Dolly Varden charr in the Higashi-Nodottomari River on Rishiri Island and review previous reports regarding the charr on Rishiri Island. In the Higashi-Nodottomari River, 76 immature in- dividuals, 12 mature males, and 5 mature females were collected. The fork length distribution showed a multi-modal distribution, and the smallest size group (ranging from 40–70 mm) is considered to represent age 0+ years (Kitano & Nakano, 1991; Kitano, 1995; Sahashi & Morita, 2018). The estimated population density was 0.37 ind./m2. Based on the literature survey, collection records reporting the charr were con- firmed in five rivers on Rishiri Island. -
Vegetation Change and Human Impacts on Rebun Island (Northwest Pacific) Over the Last 6000 Years
Quaternary Science Reviews 193 (2018) 129e144 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Vegetation change and human impacts on Rebun Island (Northwest Pacific) over the last 6000 years * Christian Leipe a, , Stefanie Müller b, Konrad Hille a, Hirofumi Kato c, Franziska Kobe a, Mareike Schmidt a, Konrad Seyffert a, Robert Spengler III d, Mayke Wagner b, ** Andrzej W. Weber e, Pavel E. Tarasov a, a Institute of Geological Sciences, Paleontology Section, Freie Universitat€ Berlin, Malteserstr. 74-100, Building D, 12249 Berlin, Germany b Eurasia Department and Beijing Branch Office, German Archaeological Institute, Im Dol 2-6, 14195 Berlin, Germany c Center for Ainu and Indigenous Studies, Hokkaido University, Kita 8, Nishi 6, Kita-ku Sapporo, Hokkaido, Japan d Max Planck Institute for the Science of Human History (Max-Planck-Institut für Menschheitsgeschichte), Jena, Germany e Department of Anthropology, University of Alberta, Tory Bldg. 13e15, Edmonton, Alberta, Canada article info abstract Article history: This study presents a high-resolution, chronologically well-constrained pollen record from Lake Kushu Received 3 May 2018 (452505800N, 1410200500E) and a record of archaeobotanical remains from the nearby Hamanaka 2 Received in revised form archaeological site. The pollen record suggests continuous long-term cooling, which parallels the decline 10 June 2018 in Northern Hemisphere summer insolation. This cooling trend is overlaid by several rather quick Accepted 10 June 2018 transitions towards cooler conditions (ca. 5540/5350, 1550, and 390 cal BP) and one distinct decadal- scale cold event around 4130 cal BP. These shifts, on one hand, correspond with major hemispherical or global-scale climate transitions/events, including the ‘Holocene Climate Transition’, the onset of the Keywords: ‘ ’ ‘ ’ ‘ ’ Holocene Dark Ages Cold Period main phase, the Little Ice Age , and the 4.2 kiloyear event , respectively. -
Obsidian Resource Use from the Jomon to Okhotsk Period on Rebun Island: an Analysis of Archaeological Obsidian
JASREP-00441; No of Pages 11 Journal of Archaeological Science: Reports xxx (2016) xxx–xxx Contents lists available at ScienceDirect Journal of Archaeological Science: Reports journal homepage: www.elsevier.com/locate/jasrep Obsidian resource use from the Jomon to Okhotsk period on Rebun Island: An analysis of archaeological obsidian Sean C. Lynch a,⁎,HirofumiKatob, Andrzej W. Weber a,c a Department of Anthropology, University of Alberta, 13-14 HM, Tory Building, Edmonton T6G 2H4, Canada b Center for Ainu and Indigenous Studies Hokkaido University, Sapporo, Kita 8, Nishi 6, Kita-ku, 060-0808, Japan c UMR 7269 – Laboratoire Méditerranéen de Préhistoire Europe Afrique, Aix-Marseille Université, 5 rue du Château de l'Horloge - B.P. 647, 13094 Aix-en-Provence, Cedex 2, France article info abstract Article history: Hokkaido obsidian sources have been widely exploited by hunter-gatherer groups in Northeast Asia since the Received 15 October 2015 Upper Paleolithic (~30,000 cal. BP). Rebun Island is located 50 km from the northwest tip of Hokkaido in the Received in revised form 4 March 2016 Sea of Japan. Given that obsidian does not occur naturally on Rebun Island, all obsidian materials found there Accepted 1 May 2016 are the result prehistoric transportation of these resources. Examination of 133 obsidian artifacts collected Available online xxxx from excavations on Rebun Island employing portable X-ray fluorescence (pXRF) provides data for assessment of obsidian resource use during the Middle Jomon, Epi-Jomon, and Okhotsk periods on Rebun Island. Previously Keywords: fi Obsidian published data are also consulted for the Late and Final Jomon, and Epi-Jomon period on Rebun Island. -
The Wildlife in Japan
T he 日本 Wildlife in の J apan 自然 The Wildlife in Japan Published in March 2015 Chuo-godochosha No. 5, 1-2-2 Kasumigaseki, Chiyoda-ku, Tokyo 100-8975, Japan http://www.env.go.jp/ © Ministry of the Environment 2015 This brochure is printed on recycled paper. Edited and published by : Wildlife Division, Nature Conservation Bureau Editorial work : Japan Wildlife Research Center Design : artpost inc. Photos provided by : Hitoshi Imai, Harumi Iida, Kazuo Unno, Yoshiteru Eguchi, Katsumi Kawasaki, Kenji Kitaura, Masahide Kubota, Kano Koide, Yasumasa Kobayashi, Atsushi Sakurai, Yasushi Sugawara, Takao Sugeta, Hiroshi Takahashi, Tomonari Nakajima, Kenji Numata, Fumihiko Ban, Shinichi Hirasawa, Yukio Horiguchi, Misaki Mizukami, Kazuo Minato, Katsuhiko Mori, Noriaki Yamamoto, Shiro Yabe, Hisashi Yokota, Pika Fan Club and Society of Scientific Photography(SSP) 1 1 Flora of Japan The flora of Japan can be roughly classified into the following four categories based on the differences in temperature and precipitation: alpine zone, subalpine zone, summer-green broad-leaved forest zone and evergreen broad-leaved forest zone. The alpine zone is dominated by stone pines, the subalpine zone is dominated by spruces, and evergreen needle-leaved trees, the summer-green broad-leaved forest zone is dominated by deciduous broad-leaved trees such as Japanese beeches and Japanese oaks, and the evergreen broad-leaved forest zone is dominated by evergreen broad-leaved trees such as Yabutsubaki (Camellia japonica) and Shii (Castanopsis spp.) The Japanese archipelago is long, stretching from north to south, and has mountain ranges exceeding 3,000 m ; therefore, its vegetation changes both horizontally (with latitude) and vertically (with altitude). -
Journey to Japan's Islands
JOURNEY TO Japan’s Over 6,800 enchanting islands waiting to be discovered Get on board and set sail for some of page 04 page 08 page 12 page 16 RISHIRI ^ REBUN SADO Island IZU Islands OKI Islands Japan’s most idyllic islands There are over 410 inhabited islands in Japan, each JOURNEY TO 04 REBUN ISLAND Japan’s RISHIRI ISLAND with its own distinctive traditions, culture, history, and events. Visiting these islands has been likened to stepping into a time capsule, as the essence of a bygone era continues to thrive. Approaching by sea, you’ll see islands overlapping on the horizon, a scene noted as 08 SADO ISLAND one of the most beautiful in this Land of the Rising Sun. 16 OKI ISLANDS When you land, prepare yourself to be mesmerized by the unique townscapes each island has to offer. 12 IZU ISLANDS 24 GOTO ISLANDS 20 SETOUCHI As you walk around, notice how time slows down. ISLANDS Nostalgia comes to the fore, filling your heart with 28 OSUMI ISLANDS the warmth and happiness of a Japan from yesteryear. It’s time to take an adventure well off the beaten path and visit some of Japan’s wonderful islands. 32 YAEYAMA ISLANDS Nozomi Kobayashi | AUTHOR AND PHOTOGRAPHER Nozomi Kobayashi is a travel writer from Japan. She has authored a number of books based on her own travel experiences, visiting 65 countries worldwide and over 100 of Japan’s islands. Currently, she is active in a wide range of fields, including giving talks and speeches about her traveling. As a boat trip ambassador for the Japan Passenger Boat Association, she promotes the charm and enjoyment that can be had from boat trips to Japan’s islands. -
Marine Reservoir Effects Deduced from 14C Dates On
Radiocarbon, Vol 58, Nr 4, 2016, p 755–770 DOI:10.1017/RDC.2016.93 © 2016 by the Arizona Board of Regents on behalf of the University of Arizona. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. MARINE RESERVOIR EFFECTS DEDUCED FROM 14C DATES ON POTTERY RESIDUES, BONES, AND MOLLUSKAN SHELLS FROM THE HAMANAKA 2 ARCHAEOLOGICAL SITE, REBUN ISLAND, HOKKAIDO, JAPAN Yoshiki Miyata1,2* • Akiko Horiuchi3 • Megumi Kondo4 • Shin Onbe2,5 • Kunio Yoshida6 • Seiya Nagao1 • PaleoLaboAMSDatingGroup7 • Toyohiro Nishimoto2 1The Low Level Radioactivity Laboratory, Institute of Nature and Environmental Technology, Kanazawa University, O 24, Wake-machi, Nomi, Ishikawa 923-1224, Japan. 2National Museum of Japanese History, 117 Jonai-cho, Sakura, Chiba 285-8502, Japan. 3College of Liberal Arts, International Christian University, 3-10-2 Osawa, Mitaka, Tokyo 181-8585, Japan. 4Graduate School of Humanities and Sciences, Ochanomizu University, 2-1-1 Ohtsuka, Bunkyo, Tokyo 112-8610, Japan. 5The Research Institute for Humanity and Nature, 457-4 Motoyama, Kamigamo, Kita-ku, Kyoto 603-8047, Japan. Present address: Kumakougen Town, Board of Education, 188 Kuma, Kamiukena-gun, Ehime 791-1201, Japan. 6The University Museum, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo 113-0033, Japan. 7AMS Dating Facility, Paleo Labo Co., Ltd., 1900-65 Shimo-tazawa, Kurohone-cho, Kiryu, Gunma 376-0144, Japan. ABSTRACT. This article investigates the marine reservoir effects from apparent age differences among molluskan shells, birds, and sea mammals from the Hamanaka 2 archaeological site, Rebun Island, Japan, which was occupied during the latter half of the Late Jomon period (1300−1200 cal BC). -
Arc Chaeology Fieldwork K on Rebun N Island, Ja Apan 2011
Archaeology Fieldwork on Rebun Island, Japan 2011 For all participants, please read all of the following documentation carefully. If you have ANY questions or concerns, please contact us at [email protected] General Information Figure 1. Rebun Island from Rishiri Mountain Beginning in 2011, the University of Alberta (Canada) has launched a joint ventuure with Hokkaido University (Japan) and several other international partners called the Baikal‐Hokkaido Archaeology Project. Fieldwork for this project foccuses upon the archaeological sites on Rebun Island, Japan. Before joining with Hokkaido University, the Baikal Archaeology project completed fieldwork, including several field schools, at several cemeteries and habitation sites along the coasts of Lake Baikal in Siberia, Russia. With this new collaboration, our 2011 fieldwork will include extensive excavations of the Late Jomon cemetery Funadomari and testing of Hamanaka, a multi‐component shell midden site with graves ranging in age from the Jomon to the historical Ainu periods. Both sites are located along the north coastt of Rebun Island. While there will be no formal field school offered in 2011, we would like to extend an invitation to interested volunteers to assist in our excavations on Rebun Island. Participants will have the opportunity to learn the skills asssociated with the archaeological excavation of cemeteries including topographic survey, drawing, photography, ground penetrating radar, as well as the identification, removal and curation of hhuman osteological material. In addition, students will experience the beautiful Japanese culture while living in the small fishing town of Funadomari. Though we are not offering course credit this year, we hope to organize formal field schools in future years. -
11. Rishirizan)
(11. Rishirizan) 11. Rishirizan Latitude: 45°10'43" N, Longitude: 141°14'31" E, Elevation: 1,721 m (Rishirizan) (Elevation Point) Overview of Rishirizan ,taken from Otadomari Swamp to south-by-southwest on October 19, 2011 by the Japan Meteorological Agency Summary Rishirizan is located 30 km west of Wakkanai, in the north of Hokkaido. It makes up the majority of the 18 km x 16 km Rishiri Island, and its ejecta extend 80m below sea level. Rishirizan became active approximately 200,000 years ago, and formed the main volcanic edifice in the years leading up to approximately 40,000 years ago, with ejecta type and ejection rates varying over that span (initial and peak period activity). It then exhibited activity from multiple craters, producing only a small amount of ejecta (approximately 10 % of the total ejecta volume). There was no more principle activity, which caused volcanic tephra fall in the north of Hokkaido, since approximately 8,000 years ago. The SiO2 content is between 49.1 and 72.8 wt %. Photo Maar and Pyroclastic Cone at the south foot of the volcano, taken from east side on August 24, 2007 by the Japan Meteorological Agency 1 (11. Rishirizan) Red Relief Image Map Rishirizan Figure 11-1 Topography of Rishirizan. 1:50,000 scale topographic map (Rishiri Island) and digital map 50 m grid (elevation) published by the Geospatial Information Authority of Japan were used. 2 (11. Rishirizan) Chronology of Eruptions ・Volcanic Activity in the Past 10,000 Years The last eruption of Rishirizan formed maars, made up of basalt magma, and a group of small scoria cones, as well as producing a lava flow that reached the south foot of the volcano.