• Search Research Projects
  • Search Researchers
  • How to Use
  1. Back to project page

2003 Fiscal Year Final Research Report Summary

Periodicity of large-scale landslide revealed by the landslide-lake sediments and ancient documents

Research Project

Project/Area Number 13640458
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field Geology
Research InstitutionGifu University

Principal Investigator

KAWAKAMI Shin-ichi  Gifu University, Faculty of Education, Department of Geology, Associate Professor, 教育学部, 助教授 (80183036)

Co-Investigator(Kenkyū-buntansha) KOIDO Yoshimitsu  Gifu University, Faculty of Education, Department of Geology, Professor, 教育学部, 教授 (60101424)
徐 勝  核燃料サイクル開発機構, 東濃地科学センター, 研究員
KOJIMA Satoru  Gifu University, Faculty of Engineering, Department of Civil Engineering, Professor, 工学部, 教授 (20170243)
XU Sheng  Tono Geoscience Center, Japan Nuclear Cycle Development Institute, Researcher
Project Period (FY) 2001 – 2003
Keywordslandslide / large-scale slope faulure / landslide-lake / periodicity / ancient document / accretionary complex / Mino terrane
Research Abstract

Prediction of large-scale landslides with more than one million cubic meters of landslide debris is important in central Japan with steep-slope topography, because they cause heavy damages on infrastrucutes. Three largest landslides (Nan'notani, Neoshiratani and Tokuyamashiratani landslides) are know to occur during last one hundred years in the Mino terrane. Two of them occurred at the sites with specific geologic structures : the resistant limestones against weathering and erosion are thrust over the weak melanges. These geologic structures formed at the time of accretion, and are useful to predict the future slides in the Mino terrane. Similar geologic structures are present in the Funafuseyama, Ibukiyama, Ryozensan and Fujiwaradake areas. Very large-scale landslides in the western slope of Ibukiyama dammed-up the Anegawa River flowing on the foot of the mountain, and formed landslide lakes. We measured the 14C ages of the lake sediments and revealed the ages of the lakes to be 34,000 and 5,200 years before present. The Sekigahara pass south of Ibukiyama has been the most important traffic route connecting eastern and western Japan, and many ancient documents described landslide events at Ibukiyama. We analyzed these documents and found that the landslide events occured at about 890, 1500, 1700 and 1909 (Anegawa earthquake) AD. These events made no landslide lakes, and the events 34,000 and 5,200 years before present making the landslide lakes were quite large in scale

  • Research Products

    (6 results)

All Other

All Publications (6 results)

  • [Publications] 山口卓哉: "美濃帯のジュラ紀メランジュの室内透水試験-八百津地城および伊自良地域の例-"応用地質. 44巻. 303-312 (2003)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 小嶋 智: "中部地方の地質特性と斜面災害"充てん. 41号. 8-13 (2002)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] 小嶋 智: "付加体分布域の大規模斜面崩壊の特徴と予測:中部地方美濃帯の例"十津川災害111周年記念集会-斜面災害発生場所予測に向けて-. 41-47 (2001)

    • Description
      「研究成果報告書概要(和文)」より
  • [Publications] Yamaguchi, T.: "Hydraulic conductivity measurements of Jurassic melange in the Yaotsu and Ijira areas, Mino terrane, central Japan"Jour.Japan Soc.Eng.Geol.. vol.44. 303-312 (2003)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Kojima, S.: "Geologic characteristics and slope disasters in central Japan"Juten. no.41. 8-13 (2002)

    • Description
      「研究成果報告書概要(欧文)」より
  • [Publications] Kojima, S.: "Characteristics and prediction of large-scale landslide in accretionary complex terrane : examples from the Mino terrane, central Japan"111th Memorial Conference of Totsugawa Disaster--For the Special Prediction of Landslides--. 41-47 (2001)

    • Description
      「研究成果報告書概要(欧文)」より

URL: 

Published: 2005-04-19  

Information User Guide FAQ News Terms of Use Attribution of KAKENHI

Powered by NII kakenhi