Memorial to Hisashi Kuno 1910-1969
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Travel the Mountains, Lakes, and Streams of Lake Towada, Oirase and Hakkoda
Towada-Hachimantai National Park Sample Course From young green buds in the spring to the rich rustic leaves Day2 of autumn, the views around the Jogakura Ohashi Bridge and the Sukayu Onsen area are spectacular B.m1 Early morning walk in each and every season. 9:00am Accommodation in Hakkoda JR bus 40min ↓ In this beech forest, there’s Travel the Mountains, 10:00am a trail that connects together six Hike the Tsutayacho marshes. Enjoy the views of the Lakes, and Streams of no Mori Course forest, as well as the flora and fauna that is distinct to Option A Lake Towada, Oirase and Towada-Hachimantai Option B National Park. Hakkoda - the All-in-one ↓JR bus 60min ↓JR bus 10min 1:30pm 12:30pm min B01 Towada Lake Canoe Tour 120 Course Lunch 2nights 3days, ↓JR bus 40min ↓JR bus 10min 5:20pm 1:40pm Oirase Keiryu Hotel Walk around Oirase Gorge Highlights ↓JR bus 30min 4:45pm Experience the exceptional scenic beauty of the lake and relax on the shore of the lake by gently flowing Accommodation in Towada Kohan streams. Make sure you don’t miss out on the JR bus Located halfway along the Oirase Gorge, there is a rest stop th pass that offers unlimited travel around Lake Towada, meals. A bus route is close to the trail, so once you have chec Oirase, and Hakkoda. timetable you can wander further upstream. at offers light ked the bus This is the only hotel along the Oirase Gorge. Guests National From Shin Aomori Station can enjoy views of the gorge from an open-air hot Parks of Japan spring, as well as a variety of activities. -
Structural Heterogeneity in and Around the Fold-And-Thrust Belt of The
Iwasaki et al. Earth, Planets and Space (2019) 71:103 https://doi.org/10.1186/s40623-019-1081-z FRONTIER LETTER Open Access Structural heterogeneity in and around the fold-and-thrust belt of the Hidaka Collision zone, Hokkaido, Japan and its relationship to the aftershock activity of the 2018 Hokkaido Eastern Iburi Earthquake Takaya Iwasaki1* , Noriko Tsumura2, Tanio Ito3, Kazunori Arita4, Matsubara Makoto5, Hiroshi Sato1, Eiji Kurashimo1, Naoshi Hirata1, Susumu Abe6, Katsuya Noda7, Akira Fujiwara8, Shinsuke Kikuchi9 and Kazuko Suzuki10 Abstract The Hokkaido Eastern Iburi Earthquake (M 6.7) occurred on Sep. 6, 2018 in the southern part of Central Hokkaido, Japan. Since Paleogene, this region has experienced= the dextral oblique transpression between the Eurasia and North American (Okhotsk) Plates and the subsequent collision between the Northeast Japan Arc and the Kuril Arc due to the oblique subduction of the Pacifc Plate. This earthquake occurred beneath the foreland fold-and-thrust belt of the Hidaka Collision zone developed by the collision process, and is characterized by its deep focal depth (~ 37 km) and complicated rupture process. The reanalyses of controlled source seismic data collected in the 1998–2000 Hokkaido Transect Project revealed the detailed structure beneath the fold-and-thrust belt, and its relationship with the aftershock activity of this earthquake. Our refection processing using the CRS/MDRS stacking method imaged for the frst time the lower crust and uppermost mantle structures of the Northeast Japan Arc underthrust beneath a thick (~ 5–10 km) sedimentary package of the fold-and-thrust belt. Based on the analysis of the refraction/wide- angle refection data, the total thickness of this Northeast Japan Arc crust is only 16–22 km. -
2021 Fall Tohoku & Hokkaido Tour #1
photo © hokkaidoguide.com 2021 FALL GUARANTEED! TOHOKU & HOKKAIDO TOUR #1 RISK FREE! Let’s Support Tohoku! “Ganbatte Tohoku!” Explore the less traveled Tohoku region then enjoy a visit to Hokkaido. Enjoy the onsen (hot springs) Cancel for Any Reason by 07/08/21! of Tsunagi, Oyu Onsen, Hakodate and Toya…a once in a lifetime experience! No Penalties & No Cancellation Fees! 10 Nights / 12 Days • 24 Meals (10 Breakfasts, 8 Lunches, 6 Dinners) Escorted from Honolulu • English-Speaking Local Guide October 06 – 17, 2021 • Tour Manager: Jennifer Lum-Ota COMPLETE PACKAGE! VISIT: $ * Omiya • Sendai • Matsushima • Kesennuma • Hiraizumi • Tsunagi • Tazawa • Morioka 4988 Oirase • Towada • Oyu Onsen • Aomori • Hakodate • Toya • Jozankei • Sapporo INCLUDES ROUNDTRIP AIRFARE FROM HONOLULU, 10 NIGHTS HOTEL, 24 MEALS, TIPS FOR LOCAL TOUR GUIDES AND BUS DRIVERS, ALL TAXES & FEES TOUR HIGHLIGHTS: Shinkansen Bullet Train Ride • Zuihoden • Matsushima Scenic Cruise EARLY BOOKING Zuiganji Temple • Sendai Shopping Area • Ishinomaki Genki Ichiba DISCOUNT PER PERSON Ishinomaki Community and Information Center • Kesennuma Seafood Market “Umino Ichi” $ Chusonji Temple • Lake Tazawa • Tatsuko Statue • Oirase Gorge • Lake Towada Cruise SAVE 100 † Hirosaki Castle • Nebuta House Warasse • JR Super Express Train Ride BOOK BY JANUARY 29, 2021 Hokkaido Road Station Danshaku Lounge • Hakodate Night View Tour Hakodate Morning Market • Hakodate Bay Area Shopping • Goryokaku Tower and Park $ Silo Observatory • Lake Hill Farm • Date History and Culture Center • Hoheikyo Dam -
Towada-Hachimantai National Park Guide Book
Towada-Hachimantai National Park Guide Book 十和田八幡平国立公園 Feel the landscapes of Northern Tohoku that change from season to season in the vast nature 四季それぞれに美しい北東北を自然の中で体感 In Japan, each of the four seasons has its own colour that allows visitors to truly feel its atmosphere. Especially in Tohoku, where winter is crucially rigorous, people wait for the arrival of spring, sing the joys of summer, and appreciate the rich harvests of autumn. There are many things in Tohoku that bring joy to people throughout the year. Towada-Hachimantai National Park is located in the mountainous area of Northern Japan, and lies upon the three prefectures of Northern Tohoku. It is composed of “Towada-Hakkoda Area” , on the northern side that consists of Lake Towada, Oirase Gorge and Hakkoda Mountains and “Hachimantai Area” , on the southern side that consists of Mt. Hachimantai, Mt. Akita-Komagatake and Mt. Iwate. Both areas are very rich in natural resources, such as forests, lakes and marshes, and a wide variety of fauna and flora. There are also many onsen spots where you can immerse your body and soul. 01 Shin-Hakodate-Hokuto Hakodate Airport Oma To Tomakomai Aomori Contents ● Tohoku Shinkansen about 3hr 10 min. Tokyo Station Shin-Aomori Station Towada-Hakkoda Area Shin-Aomori Station Airplane about 1hr 20 min. Haneda Airport Misawa Airport Airplane about 1hr 15 min. Haneda Airport Aomori Airport Tohoku Shinkansen about 1hr 30 min. Sendai Station Shin-Aomori Station Hokkaido / Tohoku Shinkansen about 1hr Shin-Hakodate-Hokuto Station Shin-Aomori Station Highway Bus about 4hr 50 min. Sendai Station Aomori Station Joy of Spring Iwate 04 春の歓喜 Tohoku Shinkansen about 2hr 20 min. -
Discover the Natural, Ancient & Modern Wonders Aboard the MS Caledonian Sky May & June 2019
SPECIAL OFFER – saVE £500 PER PERSON JAPAN DISCOVER THE NATURAL, ANCIENT & MODERN WONDERS ABOARD THE MS CALEDONIAN SKY MAY & JUNE 2019 ms caledonian sky Deluxe Balcony Suite On Deck The Restaurant The MS Caledonian Sky is one of our three flag ships and sister vessel to the MS Island Sky and MS Hebridean Sky. All three vessels were built in the same ship yard in Italy at similar times and share the same excellent attributes that make them three of the finest small ships in the world. With a maximum passenger capacity of only 114, a vessel of her size is capable of carrying many more but instead the MS Caledonian Sky has the benefit of unusually large suites, luxuriously appointed public areas and spacious outside decks. Your Suite Your Dining On board there are 57 exceptionally With only one sitting and a maximum of just over 100 passengers, the spacious and well designed suites. cuisine on board the MS Caledonian Sky is of a consistent superior The passenger accommodation is quality that befits such a vessel. In keeping with the informal atmosphere arranged over four decks and all suites on board, when dining you are able to choose your seating arrangements have outside views. All feature a sitting and choice of restaurants at your leisure; whether that be joining a table area and some have private balconies. of four to six other passengers in the elegant à la carte Restaurant or Each affords considerable comfort with outside buffet-style on the Lido Deck in the evening sunshine. In the main en-suite bathroom featuring a country Restaurant, breakfast is served buffet-style, with certain items cooked to style wash basin, heated towel rail, order on request. -
Response and Earthquake Induced Damage of Underground Structures in Rock Mass
Response and Earthquake Induced Damage of Underground Structures in Rock Mass Ömer Aydan* Yoshimi Ohta* Melih Geni** Naohiko Tokashiki*** K. Ohkubo**** *Tokai University, Department of Marine Civil Eng., Shizuoka, Japan Email: [email protected] **Zonguldak Karaelmas University, Mining Engineering Dept., Zonguldak, Turkey ***Ryukyu University, Civil Engineering Dept., Okinawa, Japan ****Nakanihon Expressway Company, Tokyo, Japan ABSTRACT Underground structures are generally known as earthquake-resistant structures as compared to surface structures. Nevertheless, the recent earthquakes showed that underground structures are also vulnerable to earthquakes. There may be several reasons for such damage such as high ground motions and permanent ground movements. This study attempts to describe various forms of damage to underground structures such as tunnels, caverns, natural caves and abandoned mines during major earthquakes. Results of various model tests on shaking table are also presented to show the effect of ground shaking on the response and collapse of underground structures in continuum and discontinuum. Furthermore, some empirical equations are proposed to assess the damage to underground structures, which may be useful for quick assessments of possible damage. Keywords: Underground opening; Earthquake damage; Fault; Shaking; Concrete lining 1. INTRODUCTION It is well known that the underground structures such as tunnels and powerhouses are generally resistant against earthquake-induced motions (Dowding and Rozen, 1978; Sharma & Judd, 1991). However, they may be damaged when permanent ground movements occur in/along the underground structures. There are several examples of damage to tunnels due to permanent ground movements during, for example, 1930 Tanna, 1978 Izu-Oshima-Kinkai, 1995 Kobe, 1999 Düzce-Bolu, 1999 Chi-chi, 2004 Chuetsu, 2005 Kashmir and 2008 Wenchuan earthquakes. -
Izu Peninsula Geopark Promotion Council
Contents A. Identification of the Area ........................................................................................................................................................... 1 A.1 Name of the Proposed Geopark ........................................................................................................................................... 1 A.2 Location of the Proposed Geopark ....................................................................................................................................... 1 A.3 Surface Area, Physical and Human Geographical Characteristics ....................................................................................... 1 A.3.1 Physical Geographical Characteristics .......................................................................................................................... 1 A.3.2 Human Geographical Charactersitics ........................................................................................................................... 3 A.4 Organization in charge and Management Structure ............................................................................................................. 5 A.4.1 Izu Peninsula Geopark Promotion Council ................................................................................................................... 5 A.4.2 Structure of the Management Organization .................................................................................................................. 6 A.4.3 Supporting Units/ Members -
Repeated Occurrence of Surface-Sediment Remobilization
Ikehara et al. Earth, Planets and Space (2020) 72:114 https://doi.org/10.1186/s40623-020-01241-y FULL PAPER Open Access Repeated occurrence of surface-sediment remobilization along the landward slope of the Japan Trench by great earthquakes Ken Ikehara1* , Kazuko Usami1,2 and Toshiya Kanamatsu3 Abstract Deep-sea turbidites have been utilized to understand the history of past large earthquakes. Surface-sediment remo- bilization is considered to be a mechanism for the initiation of earthquake-induced turbidity currents, based on the studies on the event deposits formed by recent great earthquakes, such as the 2011 Tohoku-oki earthquake, although submarine slope failure has been considered to be a major contributor. However, it is still unclear that the surface-sed- iment remobilization has actually occurred in past great earthquakes. We examined a sediment core recovered from the mid-slope terrace (MST) along the Japan Trench to fnd evidence of past earthquake-induced surface-sediment remobilization. Coupled radiocarbon dates for turbidite and hemipelagic muds in the core show small age diferences (less than a few 100 years) and suggest that initiation of turbidity currents caused by the earthquake-induced surface- sediment remobilization has occurred repeatedly during the last 2300 years. On the other hand, two turbidites among the examined 11 turbidites show relatively large age diferences (~ 5000 years) that indicate the occurrence of large sea-foor disturbances such as submarine slope failures. The sedimentological (i.e., of diatomaceous nature and high sedimentation rates) and tectonic (i.e., continuous subsidence and isolated small basins) settings of the MST sedimentary basins provide favorable conditions for the repeated initiation of turbidity currents and for deposition and preservation of fne-grained turbidites. -
FURTHER READING for the Article 'Orogenic Belts' by A. M. C. Şengör
FURTHER READING for the article ‘Orogenic Belts’ by A. M. C. Şengör in the second edition of the Encyclopaedia of Solid Earth Geophysics published by Springer Cham., Berlin and Heidelberg. Aaron, J. M., editor, 1991, An Issue dedicated to Aspects of the Geology of Japan, Site of the 29th International Geological Congress: Episodes, v. 14, no. 3, pp. 187- 302. Akbayram, K., , Şengör, A. M. C. and Özcan, E, 2017, The evolution of the Intra- Pontide suture: Implications of the discovery of late Cretaceous–early Tertiary mélanges, in Sorkhabi, R., editor, Tectonic Evolution, Collision, and Seismicity of Southwest Asia— In Honor of Manuel Berberian’s Forty-Five Years of Research Contributions: Geological Society of America Special Paper 525, pp. 573-612. Altunkaynak, Ş., 2007, Collision-driven slab breakoff magmatism in northWestern Anatolia, Turkey: The Journal of Geology, v. 115, pp. 63-82. Anonymous, 1984, Origin and History of Marginal and Inland Seas: Proceedings of the 27th International Geological Congress, Moscow, 4-14 August 1984,v. 23, VNU Science Press, Utrecht, vii+223 pp. Arai, R., IWasaki, T., Sato, H., Abe, S. and Hirata, N., 2009, Collision and subduction structure of the Izu–Bonin arc, central Japan, revealed by refraction/wide-angle reflection analysis: Tectonophysics, v. 475, pp. 438-453. Aramaki, S. and Kushiro, I., editors, 1983, Arc Volcanism: Elsevier, Amsterdam, VII+652 pp. Arkle, J. C., Armstrong, P. A., Haeussler, P. J., Prior, M. G., Harman, S., Sendziak, K. L. and Brush, J. A., 2013, Focused exhumation in the syntaxis of the Western Chugach Mountains and Prince William Sound, Alaska: Geological Society of America Bulletin, v. -
27. Sedimentary Facies Evolution of the Nankai Forearc and Its Implications for the Growth of the Shimanto Accretionary Prism1
Hill, I.A., Taira, A., Firth, J.V., et al., 1993 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 131 27. SEDIMENTARY FACIES EVOLUTION OF THE NANKAI FOREARC AND ITS IMPLICATIONS FOR THE GROWTH OF THE SHIMANTO ACCRETIONARY PRISM1 Asahiko Taira2 and Juichiro Ashi2 ABSTRACT A combination of Deep Sea Drilling Project-Ocean Drilling Program drilling results and site survey data in the Shikoku Basin, Nankai Trough, and Nankai landward slope region provides a unique opportunity to investigate the sedimentary facies evolution in the clastic-dominated accretionary forearc. Here, we consider the facies evolution model based on the drilling results, IZANAGI sidescan images, and seismic reflection profiles. The sedimentary facies model of the Nankai forearc proposed in this paper is composed of two parts: the ocean floor-trench- lower slope sedimentary facies evolution and the upper slope to forearc basin sedimentary facies evolution. The former begins with basal pelagic and hemipelagic mudstones overlain by a coarsening upward sequence of trench turbidites which are, in turn, covered by slope apron slumps and lower slope hemipelagic mudstone. This assemblage is progressively faulted and folded into a consolidated accretionary prism that is then fractured and faulted in the upper slope region. Massive failure of the seafloor in the upper slope region produces olistostrome deposits that contain lithified blocks derived from older accretionary prism dispersed in a mud matrix. The contact between the older accretionary prism and the upper slope olistostrome is a submarine unconformity that is the first stratigraphic evidence for the exhumation of an older prism to the seafloor. The olistostrome beds are then overlain by forearc basin-plain mudstone and turbidites which are progressively covered by coarsening-upward delta-shelf sequences. -
Hokkaido, Tohoku & Central Japan: Kyoto Aoi
All Japan Tours 337 N.Vineyard Ave Suite 215, Ontario, CA 91764 Toll Free: 1-855-325-2726 (US/CANADA) Tel: 1-909-988-8885 Fax: 1-909-349-1736 E-mail: [email protected] Hokkaido, Tohoku & Central Japan: Kyoto Aoi Festival & Cherry Blossoms 2017 - 5/4 Exploring Japan's two main islands: Hokkaido & Honshu, as well as the Kyoto Aoi Festival Tour Code: GTG1065452 Tour Information Land cost: from USD $5198 Tour cost includes: • 10 nights Western style and 4 nights Japanese style Single supplement: USD $1120 accommodation • Meet and greet upon arrival at Chitose Airport Tour duration: 15 days 14 nights • Airport transfers on arrival and departure Destination: • Private coach transfers between destinations in Hokkaido (Sapporo / Otaru / Shiraoi / Noboribetsu / Japan Lake Toya / Hakodate), Tohoku (Seikan Tunnel / • Comprehensive escorted with AJT professional Towada / Morioka / Hiraizumi / Matsushima), Central English speaking tour guide Japan (Nikko / Tokyo / Mt Fuji / Hakone / Hikone / Koka / Kyoto / Uji / Nara / Osaka) • Gratuities Meals • Breakfast everyday • 10 lunches and 6 dinners Admission fees and activities • All entry fees to sites, activities listed in the itinerary Dates & Price 2017 Start Date End Date Twin / Triple Start City End City Style Status Thu. May 4, 2017 Thu. May 18, 2017 USD $5198.00 Sapporo Osaka Deluxe View Tour 2018 Start Date End Date Twin / Triple Start City End City Style Status Fri. May 4, 2018 Fri. May 18, 2018 USD $5198.00 Sapporo Osaka Deluxe View Tour Page 1/16 Itinerary Tour Code: GTG1065452 Day 1 Chitose Airport Welcome to Sapporo! An AJT representative will meet you at the arrival gate and direct you to the hotel. -
Historical Changes in the Ecosystem Condition of a Small Mountain Lake
RESEARCH ARTICLE Historical Changes in the Ecosystem Condition of a Small Mountain Lake over the Past 60 Years as Revealed by Plankton Remains and Daphnia Ephippial Carapaces Stored in Lake Sediments Hajime Ohtsuki1*, Tamotsu Awano1, Narumi K. Tsugeki1¤a, Seiji Ishida1¤b, Hirotaka Oda2, Wataru Makino1, Jotaro Urabe1 1 Graduate School of Life Sciences, Tohoku University, Sendai, Miyagi, Japan, 2 Chronological Research, Nagoya University, Nagoya, Aichi, Japan ¤a Current Address: Senior Research Fellow Center, Ehime University, Matsuyama, Ehime, Japan ¤b Current Address: Department of Environmental Science, Toho University, Funabashi, Chiba, Japan * [email protected] OPEN ACCESS Citation: Ohtsuki H, Awano T, Tsugeki NK, Ishida S, Oda H, Makino W, et al. (2015) Historical Changes in Abstract the Ecosystem Condition of a Small Mountain Lake over the Past 60 Years as Revealed by Plankton To examine if changes in species composition of a plankton community in the past due to an- Remains and Daphnia Ephippial Carapaces Stored in thropogenic activities can be clarified in lakes without any monitoring data, we analyzed ge- Lake Sediments. PLoS ONE 10(3): e0119767. doi:10.1371/journal.pone.0119767 netically ephippial carapaces of Daphnia with plankton remains stored in the bottom sediments of Lake Hataya Ohunma in Japan. In the lake, abundance of most plankton re- Academic Editor: Jiang-Shiou Hwang, National – 2 Taiwan Ocean University, TAIWAN mains in the sediments was limited and TP flux was at low levels (2 4mg/m /y) before 1970. However TP flux increased two-fold during the period from 1980s to 1990s. In parallel with Received: September 5, 2014 this increase, abundance of most plankton remains increased although abundance of benthic Accepted: January 16, 2015 testate amoebae’s remains decreased, indicating that the lake trophic condition had changed Published: March 10, 2015 from oligo- to mesotrophic for the past 60 years.