Island Island
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Ai2014-5 Aircraft Serious Incident Investigation Report
AI2014-5 AIRCRAFT SERIOUS INCIDENT INVESTIGATION REPORT HOKKAIDO AIR SYSTEM CO., LTD. J A 0 3 H C November 27, 2014 The objective of the investigation conducted by the Japan Transport Safety Board in accordance with the Act for Establishment of the Japan Transport Safety Board (and with Annex 13 to the Convention on International Civil Aviation) is to prevent future accidents and incidents. It is not the purpose of the investigation to apportion blame or liability. Norihiro Goto Chairman, Japan Transport Safety Board Note: This report is a translation of the Japanese original investigation report. The text in Japanese shall prevail in the interpretation of the report. AIRCRAFT SERIOUS INCIDENT INVESTIGATION REPORT HOKKAIDO AIR SYSTEM CO., LTD. SAAB 340B, JA03HC EMERGENCY OPERATION TO AVOID COLLISION WITH THE TERRAIN ABOVE OKUSHIRI AIRPORT AROUND 11:38 JST, JUNE 4, 2011 November 7, 2014 Adopted by the Japan Transport Safety Board Chairman Norihiro Goto Member Shinsuke Endoh Member Toshiyuki Ishikawa Member Sadao Tamura Member Yuki Shuto Member Keiji Tanaka SYNOPSIS Summary of the Incident On June 4 (Saturday), 2011, a SAAB 340B, registered JA03HC, operated by Hokkaido Air System Co., Ltd., took off from Hakodate Airport as a scheduled Flight 2891. During the approach to Runway 31 of Okushiri Airport, the aircraft executed a go-around and once started climbing, but it soon reversed to descend. Consequently, at around 11:38 Japan Standard Time, its flight crew became aware of the situation and executed an emergency operation to avoid crash to the ground. The aircraft flew back to Hakodate Airport, following some holdings over Okushiri Airport. -
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. -
Hokkaido Map Scenic Spots in the Kamikawa Area
Cape Soya Wakkanai Rebun Island Wakkanai Airport Scenic spots in the Kafuka Oshidomari Kamikawa area Mt. Rishiri Hokkaido Map ▲ Rishiri Nakagawa/Aerial photo of Teshio River Saku Otoineppu/The place that Hokkaido was named Rishiri Island Toyotomi Onsen (Mizukiri Contest (Stone-skipping Contest)) in July Airport Toyotomi Nakagawa Otoineppu Etorofu Island 40 Bifuka/Farm inn tonttu Horokanai/Santozan Mountain Range Shibetsu/Suffolk Land Kenbuchi/Nano in July Wassamu/A street lined with white birch in winter Bifuka Yagishiri Chiebun Sunflower fields● ●Nayoro Onsen Teuri Okhotsk Island Island Haboro Nayoro Mombetsu Lake Shumarinai Shimokawa Monbetsu ●Icebreaker Airport "Garinko-go" ●Takinoue Park Shiretoko Peninsula Kamiyubetsu World Sheep Museum● Shibetsu Tulip Park ● Takinoue Lake Saroma Nayoro/Sunflower fields Shimokawa/Forest in winter Asahikawa/Kamuikotan Library of picture books● Mt. Rausu Kenbuchi ▲ Engaru Lake Notoro Wassamu Horokanai Mt. Teshio Abashiri Utoro Onsen Rausu ▲ Maruseppu Lake Abashiri Rumoi Takasu Pippu ●Maruseppu Abashiri-Kohan Onsen Kunashiri Island Onsen Shiretoko-Shari Mashike Aibetsu Memanbetsu ●Tohma Limestone cave Airport Kitami Snow Crystal Museum● Tohma Kamikawa ● Shikotan Island Asahiyama Zoo 39 ▲ Asahikawa Asahikawa Mt. Shari ▲ 237 Airport Sounkyo Onsen Mt. Shokanbetsu 39 Onneyu Onsen Higashikagura Kawayu Onsen ▲ Asahidake Onsen Lake Kussharo Higashikawa Mt. Asahidake Tenninkyo Onsen Habomai Islands Takikawa Ashibetsu Biei Takasu/Palette Hills in May Pippu/The top of Pippu Ski Area in Jan. Aibetsu/Kinokonosato park golf course in May Shirogane Onsen ▲ Lake Mashu Shintotsukawa Kamifurano Mt. Tomuraushi Lake Akan Mashu Nakashibetsu Airport 12 Akan Mashu Cape Shakotan Nakafurano ▲ Akanko Onsen Mt. Tokachi Nukabira Onsen ▲ Onsen Mt. Oakan Bibai Furano Nemuro Cape Kamui Nemuro Peninsula Ishikari Bay 44 Otaru Iwamizawa 38 Ashoro Minamifurano Yoichi Sapporo ▲ Hoshino Resorts Shiranuka Yubari Mt. -
400869 Why Did Tsunami Fires? : in the 1993 Hokkaido Nansei-Oki and The
NH41C-1012 Why did tsunami fire? : in the 1993 Hokkaido Nansei-Oki and the 2011 Tohoku-Oki earthquakes Yuji Enomoto* & Tsuneaki Yamabe (Shinshu Univ.)Shigeki Sugiura & Hitoshi Kondo (Geneses Res. Inst. Inc.) *Corresponding author, e-mail: [email protected] 130° 140° 150° 1993 M7.8 45° Aonae district a Hokkaido b c e f Nansei-Oki eq. Hokkaido M7.8 (Depth:35km) 5 4 Okushiri 3 5 4 3 2 island Hokkaido 40° 2 Tohoku Okushiri Tsunami 2011 M9 Tohoku-Oki eq. NHK Video 1 camera d g ̴10min 1 Okushiri 35° Island after ̴a few the e.q. min. Honshu at later 50km 22:17JST 30° Aonae 100m Fig.1 a right & g; the Okushiri-cho kirokusho on 1993 Hokkaido Nansei-Oki jisin:Tsunami simulation by Disaster Control Research Center, Tohoku University, :1b & e photo by Geographical Survey Inst.: c,d & f, NHK TV Special Program “Okushiri-toh karano Houkoku, aired at 20:00-20:50 on 16 July 1993. Mysterious tsunami fires When the tsunami struck Aonae Mesh Labo-experiments, where a weight was a) Electrode To: have occurred at the Aonae district, a people who witnessed mA meter at electrode Falling bias 0 volt, dropped on the seawater bubbled with methane, this situation testify as follows: weight: or district of Okushiri Island, 1.5kg Electrostatic showed that splashed mists were positively Hokkaido ,Japan in the 1993 “Mists was rising, and sea Voltmeter charged (Fig.3 b & c). Hokkaido Nansei-Oki water was foaming” A b) c) I (uA) 200 earthquake (Fig.1a). About 10 similar scene could be observed 1 2 3 0 minutes after the M7.8 in the video footage shot during Acrylic pipe50mm 100 , mA Deionized water Time, sec. -
Hokkaido Self Drive 6天5晚 北海道自驾游 6D5n Hokkaido Self Drive Ground Arrangement | (T/C: Ga-Jha) Self Drive | Updated: 28Nov2018
海道自驾游 北HOKKAIDO SELF DRIVE 6天5晚 北海道自驾游 6D5N HOKKAIDO SELF DRIVE GROUND ARRANGEMENT | (T/C: GA-JHA) SELF DRIVE | UPDATED: 28NOV2018 Red Brick Warehouse 金森红砖仓库 Odori Park 大通公园 DAY 1: ARRIVAL CHITOSE AIRPORT – NOBORIBETSU - TOYA (D) | 抵达千岁机场 - 登别-洞爷 (晚餐) Upon arrive at Chitose airport (CTS), pick up your vehicle at the car rental shop after you may wish to visit: • Lake Shikotsu (photo stop) | 支笏湖 Drive to Noboribetsu (Estimate 1hr) • Jigokudani (photo stop) | 登别地狱谷 Dinner at hotel DAY 2: TOYA – HAKODATE (B) | 洞爷 - 函馆 (早) After breakfast, you may wish to visit: Drive to Hakodate (Estimate 2.5hrs) • Lake Onuma & Lake Konuma (photo stop) | 大沼公园 • Red Brick Warehouse | 金森红砖仓库 • Motomachi area | 元町 • Mt. Hakodate Ropeway for Night View | 函馆山夜景 - Lake Shikotsu 支笏湖 乘坐吊车 (Exclude ticket: about JPY1280/pax) DAY 3: HAKODATE – OTARU (B) | 函馆 - 小樽 (早) After breakfast, you may wish to visit: • Hakodate Morning Market | 函馆早市 Drive to Niseko (Estimate 2.5hrs) • Onsen Experience | 体验日本温泉 (Exclude ticket: about JPY1050/pax) Drive to Otaru (Estimate 1.5hrs) • Otaru Canal | 小樽运河 • Kitaichi Glass | 北一硝子馆 • Music Box Museum | 水晶音乐城 DAY 4: OTARU - SAPPORO (B) | 小樽 - 札幌 (早) After breakfast, you may wish to visit: • Nikka Yoichi Whisky Factory | 日华威士忌余市蒸留厂 Asahikawa Zoo 旭山动物园 Drive to Sapporo (Estimate 1.5hrs) • Odori Park | 大通公园 尽情玩乐,时间掌握在自己手中。 • TV Tower | 札幌电视塔 玩 More FLEXI time. • Former Government Building (photo stop) | 旧道厅 • Clock Tower (photo stop) | 时计台 在北海道,享受自驾游的乐趣。 • Hokkaido Shrine (photo stop) | 北海道神宮 乐 Enjoy Self-drive FUN in Hokkaido. • Shiroi -
The Role of Diffraction Effects in Extreme Run-Up Inundation at Okushiri Island Due to 1993 Tsunami
Nat. Hazards Earth Syst. Sci., 15, 747–755, 2015 www.nat-hazards-earth-syst-sci.net/15/747/2015/ doi:10.5194/nhess-15-747-2015 © Author(s) 2015. CC Attribution 3.0 License. The role of diffraction effects in extreme run-up inundation at Okushiri Island due to 1993 tsunami K. O. Kim1, D. C. Kim2, B. H. Choi3, K. T. Jung1, J. H. Yuk4, and E. Pelinovsky5,6 1Marine Radionuclide Research Center, Korea Institute of Ocean Science and Technology, Ansan, 426-744, Korea 2Technology R&D Institute, Hyein E&C Co. Ltd., Seoul, 157-861, Korea 3Department of Civil and Environmental Engineering, Sungkyunkwan University, Chunchun-dong 300, Jangan-gu, Suwon, 440-746, Korea 4Disaster Management HPC Technology Research Center, Korea Institute of Science and Technology Information, Daejeon, 305-806, Korea 5Nizhny Novgorod State Technical University n.a. R.E. Alekseev, Nizhny Novgorod, 603950, Russia 6Institute of Applied Physics, Nizhny Novgorod, 603950, Russia Correspondence to: B. H. Choi ([email protected]) Received: 15 October 2014 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 13 November 2014 Revised: 27 February 2015 – Accepted: 4 March 2015 – Published: 8 April 2015 Abstract. The tsunami generated on 12 July 1993 by 1 Introduction the Hokkaido–Nansei–Oki earthquake (Mw D 7.8) brought about a maximum wave run-up of 31.7 m, the highest The tsunami generated on 12 July 1993 by the Hokkaido– recorded in Japan during the 20th century, near the Monai Nansei–Oki earthquake (Mw D 7:8) produced the worst lo- Valley on the west coast of Okushiri Island (Hokkaido cal tsunami-related death toll in Japan in 50 years, bring- Tsunami Survey Group, 1993). -
Ÿþm I C R O S O F T W O R
AA2012-6 AIRCRAFT ACCIDENT INVESTIGATION REPORT NAKANIHON AIR SERVICE CO., LTD. J A 3 9 0 2 July 27, 2012 The objective of the investigation conducted by the Japan Transport Safety Board in accordance with the Act for Establishment of the Japan Transport Safety Board and with Annex 13 to the Convention on International Civil Aviation is to determine the causes of an accident and damage incidental to such an accident, thereby preventing future accidents and reducing damage. It is not the purpose of the investigation to apportion blame or liability. Norihiro Goto Chairman, Japan Transport Safety Board Note: This report is a translation of the Japanese original investigation report. The text in Japanese shall prevail in the interpretation of the report. AIRCRAFT ACCIDENT INVESTIGATION REPORT NAKANIHON AIR SERVICE CO., LTD. CESSNA TU206G, JA3902 IN THE MOUNTAINS EAST OF MT. IWABE-DAKE, FUKUSHIMA-TOWN, MATSUMAE-GUN, HOKKAIDO PREFECTURE AROUND 10:40 JST, JULY 28, 2010 June 22, 2012 Adopted by the Japan Transport Safety Board Chairman Norihiro Goto Member Shinsuke Endoh Member Toshiyuki Ishikawa Member Sadao Tamura Member Yuki Shuto Member Toshiaki Shinagawa SYNOPSIS Summary of the Accident On July 28 (Wednesday), 2010, a Cessna TU206G, registered JA3902, operated by Nakanihon Air Service Co., Ltd., took off from Niigata Airport at 08:49 local time1 for a ferry flight to Sapporo Airfield, but it did not arrive there even after the estimated arrival time of 12:49 and went missing. Search and rescue (SAR) activities found the crashed aircraft in the mountains east of Mt. Iwabe-dake in Fukushima-town, Matsumae-gun, Hokkaido Prefecture, on July 30 (Friday), 2010. -
An Adventure Around Lake Akan Together with the Ainu the Ainu Are
An adventure around Lake Akan together with the Ainu The Ainu are an indigenous people of Japan. Discover the unique culture of the Ainu living in the shores of Lake Akan. In the hustle and bustle of daily life, The Ainu People There are some things you may have forgotten. Prior to the modern history of Japan, Hokkaido was mainly inhabited by an indigenous people distinct from the "Wajin" people of the Taking the time to listen to the forest, mainland. These indigenous people called themselves the Ainu. In the Ainu language, the word "Ainu" means "human". And taking the time to appreciate The Ainu lived a lifestyle that made full use of the blessings of nature All the living beings in this earth. through hunting and fi shing. They had no written language, and they passed down their history and cultural heritage orally, but they have developed a unique spiritual culture and a rich tradition that includes epics, songs, and dances. The Ainu way of life gently reminds us Of the importance of these simple things. The Ainu Spirit So come and meet the Ainu people The Ainu believe that everything in nature is inhabited by a divine And experience their rich culture. spirit called "kamuy". This includes animals, plants, fi re, and water, and even objects essential to their daily lives, such as the tools they It will surely enrich your own life. use. It also includes phenomena humans cannot control such as the weather. They revere these things as manifestations of kamuy who have come to the human world. -
Liquefaction Damage of Sandy and Volcanic Grounds in the 1993 Hokkaido Nansei-Oki Earthquake
Missouri University of Science and Technology Scholars' Mine International Conferences on Recent Advances 1995 - Third International Conference on Recent in Geotechnical Earthquake Engineering and Advances in Geotechnical Earthquake Soil Dynamics Engineering & Soil Dynamics 06 Apr 1995, 10:30 am - 12:30 pm Liquefaction Damage of Sandy and Volcanic Grounds in the 1993 Hokkaido Nansei-Oki Earthquake S. Miura Muroran Institute of Technology, Japan K. Yagi Chizaki Kogyo Co. Ltd., Japan S. Kawamura Hokkaido College, Senshu University, Japan Follow this and additional works at: https://scholarsmine.mst.edu/icrageesd Part of the Geotechnical Engineering Commons Recommended Citation Miura, S.; Yagi, K.; and Kawamura, S., "Liquefaction Damage of Sandy and Volcanic Grounds in the 1993 Hokkaido Nansei-Oki Earthquake" (1995). International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics. 3. https://scholarsmine.mst.edu/icrageesd/03icrageesd/session03/3 This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This Article - Conference proceedings is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. (\ Proceedings: Third International Conference on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics, '-'1 April2-7, 1995, Volume I, St.louis, Missouri Liquefaction Damage of Sandy and Volcanic Grounds in the 1993 Hokkaido Nansei-Oki Earthquake Paper No. -
Unusual Rupture Process of the Japan Sea Earthquake
Eos, Vol. 74, No. 34, August 24, 1993 ure 4, which shows the result of multiple Unusual Rupture currence of large, shallow, underthrusting shock inversion of P-waves recorded by the earthquakes on the west coast of Honshu IRIS network. Process of the Japan and Hokkaido is somewhat odd. Nonethe less, there is now almost a continuous link Vertical displacements of Okushiri were age of the rupture areas of such earthquakes measured by Shimamoto et al. (Shimamoto Sea Earthquake off the western coasts of Honshu and Hok et al., personal communication, 1993). Ac PAGES 377, 379-380 kaido, and this activity extends north to cording to Shimamoto et al., the earthquake Sakalin. subsided and tilted the island. The amount On July 12, 1993, a large earthquake and The August 2, 1940, earthquake ruptured of subsidence ranges from about 20 cm associated tsunami caused terrible damage the northernmost segment along this margin; (±10 cm) at the northern end to about 90 to the Japan Sea side of Japan, Korea, and the June 16, 1964, Niigata earthquake rup cm (±10 cm) at the southern end of the is Russia. The southwestern shore of Hokkaido tured the southernmost segment; and the land. This Okushiri subsidence seems to and Okushiri Island were particularly hard May 26, 1983, Japan Sea earthquake then support the idea that the earthquake's main hit. All aspects of this earthquake will un filled in a segment off northern Honshu [see rupture occurred on the westerly dipping doubtedly be studied in great detail. This Fukao and Furumoto, 1975; Satake, 1986]. -
Volcanic Origin of the 1741 Oshima-Oshima Tsunami in the Japan Sea
Earth Planets Space, 59, 381–390, 2007 Volcanic origin of the 1741 Oshima-Oshima tsunami in the Japan Sea Kenji Satake Active Fault Research Center, National Institute of Advance Industrial Science and Technology, 1-1-1 Higashi, Tsukuba 305-8567, Japan (Received September 25, 2006; Revised January 9, 2007; Accepted January 19, 2007; Online published June 8, 2007) The generation mechanism of the 1741 Oshima-Oshima tsunami, which is considered to be the most destructive tsunami that has ever originated in the Japan Sea, has been the subject of much debate. The tsunami caused about 2,000 casualties along the Hokkaido and northern Honsu coasts and inflicted damage as far as the Korean Peninsula. The tsunami source is located between recent tsunamigenic earthquakes, but there is no historical record of an earthquake in 1741. In contrast, the records indicate volcanic activity of Oshima-Oshima, including a large-scale sector collapse, although the volume change associated with the subaerial landslide is too small to explain the observed tsunami heights. Recent marine surveys indicate that the landslide extended to the ocean bottom with a volume change of about 2.5 km3, nearly an order of magnitude larger than the subaerial slide. On the basis of mapped bathymetry, the generation of the tsunami is calculated using a simple kinematic landslide model. The tsunami propagation is computed in two different grids—a 6 grid around the source and a 1 grid for the entire Japan Sea. A parameter search of the model shows that the observed tsunami heights are best explained by a horizontal slide velocity of 40 m/s and a rise time of 2 min. -
Chapter 2 Aircraft Accident and Serious Incident Investigations
Chapter 2 Aircraft accident and serious incident investigations Chapter 2 Aircraft accident and serious incident investigations 1 Aircraft accidents and serious incidents to be investigated <Aircraft accidents to be investigated> ◎Paragraph 1, Article 2 of the Act for Establishment of the Japan Transport Safety Board(Definition of aircraft accident) The term "Aircraft Accident" as used in this Act shall mean the accident listed in each of the items in paragraph 1 of Article 76 of the Civil Aeronautics Act. ◎Paragraph 1, Article 76 of the Civil Aeronautics Act (Obligation to report) 1 Crash, collision or fire of aircraft; 2 Injury or death of any person, or destruction of any object caused by aircraft; 3 Death (except those specified in Ordinances of the Ministry of Land, Infrastructure, Transport and Tourism) or disappearance of any person on board the aircraft; 4 Contact with other aircraft; and 5 Other accidents relating to aircraft specified in Ordinances of the Ministry of Land, Infrastructure, Transport and Tourism. ◎Article 165-3 of the Ordinance for Enforcement of the Civil Aeronautics Act (Accidents related to aircraft prescribed in the Ordinances of the Ministry of Land, Infrastructure, Transport and Tourism under item 5 of the paragraph1 of the Article 76 of the Act) The cases (excluding cases where the repair of a subject aircraft does not correspond to the major repair work) where navigating aircraft is damaged (except the sole damage of engine, cowling, engine accessory, propeller, wing tip, antenna, tire, brake or fairing). <Aircraft serious incidents to be investigated> ◎Item 2, Paragraph 2, Article 2 of the Act for Establishment of the Japan Transport Safety Board (Definition of aircraft serious incident) A situation where a pilot in command of an aircraft during flight recognized a risk of collision or contact with any other aircraft, or any other situations prescribed by the Ordinances of Ministry of Land, Infrastructure, Transport and Tourism under Article 76-2 of the Civil Aeronautics Act.