Investigation of slopes on the Takanoobane lava dome using the resistivity imaging method

Y. Kochi, T. Kariya, D. Matsumoto, T. Hirose, Hemanta Hazarika

Research output: Contribution to journalArticle

Abstract

In the Kumamoto earthquake in 2016, landslides occurred in many place on moderately inclined slope in the Takanoobane lava dome. In this research, we focus on the orange-colored pumice layer (Kpfa), which is predisposed to the landslide, and show the distribution using the resistivity imaging method on a slope where no landslide has occurred. According to the survey results, the slope without the landslide was observed when the slope was hard to slip mechanically due to the Kpfa layer was distributed in a shallow place or paleogeography of the foundation layer surface (Takanoobane lava) .

Original languageEnglish
Pages (from-to)261-266
Number of pages6
Journallowland technology international
Volume19
Issue number4
Publication statusPublished - Mar 1 2018

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Landslides
Domes
Imaging techniques
Abrasives
Earthquakes

All Science Journal Classification (ASJC) codes

  • Engineering(all)

Cite this

Investigation of slopes on the Takanoobane lava dome using the resistivity imaging method. / Kochi, Y.; Kariya, T.; Matsumoto, D.; Hirose, T.; Hazarika, Hemanta.

In: lowland technology international, Vol. 19, No. 4, 01.03.2018, p. 261-266.

Research output: Contribution to journalArticle

Kochi, Y. ; Kariya, T. ; Matsumoto, D. ; Hirose, T. ; Hazarika, Hemanta. / Investigation of slopes on the Takanoobane lava dome using the resistivity imaging method. In: lowland technology international. 2018 ; Vol. 19, No. 4. pp. 261-266.
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