Skip to main content

Geologic and Hydrologic Investigations on Slope Failures Triggered by Extreme Rainfall on Izu Oshima Island, Japan

  • Chapter
  • First Online:
Understanding and Reducing Landslide Disaster Risk (WLF 2020)

Part of the book series: ICL Contribution to Landslide Disaster Risk Reduction ((CLDRR))

Included in the following conference series:

  • 697 Accesses

Abstract

A volcanic slope on Izu Oshima Island in Japan experienced a significant rainfall-induced landslide disaster in October, 2013. Because this slope had been stable for centuries, a special investigation was carried out on the cause. Because of its volcanic origin, the failed slope consisted of layers of ash, sand and lava. While the investigation concerned many disciplines, this paper addresses the post-disaster geotechnical studies. The emphasis was put on the reason why some parts of the slope “did not” fail because the post-disaster construction of infrastructures in the affected area relied on the future stability of the affected mountain slope. In line with this, another focus was on the geohydrological characteristics in the underlying lava layer. We concluded that the lava layer is pervious and allows drainage of infiltrated rain water and that, only during extremely heavy rain, slope failures are triggered in subsurface “valleys” that are carved in lava bedrock. For seven years after the disaster, the remaining parts of the slope have been stable.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 139.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 179.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 179.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Bell FG, Maud RR (2000) Landslides associated with the colluvial soils overlying the Natal Group in the greater Durban region of Natal, South Africa. Environ Geol 39(9):1029–1038

    Google Scholar 

  • Disaster Prevention Board of Tokyo Metropolitan Government (1990) Characteristics on volcanic activities in Izu Archipelago, p 40. (in Japanese)

    Google Scholar 

  • Japan Meteorological Agency (1958) Kanogawa typhoon, Technical Report, 37, p 140. (in Japanese)

    Google Scholar 

  • Koyama M, Hayakawa Y (1996) Syn- and post-caldera eruptive history of Izu Oshima Volcano based on tephra and loess stratigraphy. J Geogr Tokyo Geogr Soc 105(2):133–162. (in Japanese)

    Google Scholar 

  • Nakamura K (1964) Volcano-stratigraphic study of Oshima Volcano, Izu. Bull Earthq Res Inst Univ Tokyo 42(4):649–728. (in Japanese)

    Google Scholar 

  • Terashima T, Matsushi Y, Hattanji T (2014) Hydrological aspects of shallow landslide occurrence in Izu-Oshima Island, triggered by a heavy rainfall of typhoon 26th on October 15–16, 2013. Ann Disaster Prev Res Inst Kyoto Univ 57A:17–24. (in Japanese)

    Google Scholar 

  • Tokyo Metropolitan Government (2014) Report of committee on disaster mitigation plan after slope disaster in 2013. (in Japanese)

    Google Scholar 

  • Wang G, Jiang Y, Chang C, Doi I, Kamai T, (2019) Volcaniclastic debris avalanche on Motomachi area of Izu-Oshima, Japan, triggered by severe storm: phenomenon and mechanisms. Eng Geol 251:24–36

    Google Scholar 

Download references

Acknowledgements

This study was conducted as an emergency investigation after the disaster with a financial support from the Ministry of Education, Culture, Sports, Science and Technology. It was supported by the Oshima Municipal Government, Ministry of Environment and Geopark of Oshima (Mr. A. Kajiya). The borehole data provided by the Tokyo Metropolitan Government was essential. Collaboration was successfully made by Japanese Geotechnical Society, Japan Society of Civil Engineers, Japan Society of Engineering Geology and Japan Landslide Society. Boring investigations were carried out by the Chisui Kaihatsu Company. Sincere appreciation is dedicaetd to any members of our research group, including Dr. Gonghui Wang, Dr. Taro Uchimura and Dr. Hiroshi Yamaguchi whose names could not be included in the authors’ list of this paper due to number limitation.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Ikuo Towhata .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2021 Springer Nature Switzerland AG

About this chapter

Check for updates. Verify currency and authenticity via CrossMark

Cite this chapter

Towhata, I., Akima, T., Goto, S., Goto, S., Tanaka, J., Aoyama, S. (2021). Geologic and Hydrologic Investigations on Slope Failures Triggered by Extreme Rainfall on Izu Oshima Island, Japan. In: Arbanas, Ž., Bobrowsky, P.T., Konagai, K., Sassa, K., Takara, K. (eds) Understanding and Reducing Landslide Disaster Risk. WLF 2020. ICL Contribution to Landslide Disaster Risk Reduction. Springer, Cham. https://doi.org/10.1007/978-3-030-60713-5_12

Download citation

Publish with us

Policies and ethics