Landform and Vulnerability for Disaster in Land Use Changing

Chapter

Abstract

The fluvial and coastal landforms have important roles causing natural disaster and had influence on disaster-stricken area of liquefaction under the expansion of land use changing in the Tone River lowland. In this chapter, the disaster vulnerability, specific liquefaction, is designated upon several mesh maps of risk levels, landform, land use, and vulnerability transformation of liquefaction on land use changing in the case of the lower Tone River floodplain. The liquefaction vulnerability is brought by physical dimensions as the scale of earthquake, the distance from hypocentral region, landform and sedimentation, underground water table, etc., and the other hand, the human dimensions as recent rapid land use change and regional planning without knowledge of geomorphology are accelerating higher vulnerable level, low resilience, and longer period for resuscitation from disaster. The land use changing with urban sprawl on site has been inducing to be new and transforming vulnerability level. Geomorphology demonstrates landform process and explaining the former natural disaster occurrence history and vulnerability level of disaster; therefore, understanding disaster vulnerability on site in the fluvial and coastal plain would support future regional planning toward to secure from disaster mitigation and appropriate land use pattern planning should be discussed in future. The essential of risk reduction needs appropriate sustainable education, and the geomorphology should be core subject due to secure for lives.

Keywords

Vulnerability Fluvial landform Coastal landform Land use change Liquefaction Risk Landform Mesh map 

Notes

Acknowledgement

I should offer my thanks for Mr. Sho Naruse who supported for my research of liquefaction assessment along the lower Tone River in 2011 and 2012. The late Dr. Masahiko Oya who was a superior fluvial geomorphologist and the author studied with him the lower Tone River and prepared geomorphologic land classification map of Lake Kasumigaura and surrounding. These joint researches are important groundwork of this chapter and the author should express my thanks for Dr. Masahiko Oya.

References

  1. Asano I, Tokashiki M, Mori M, Nishihara M (2011) Damage to irrigation and drainage canals along the Tone River downstream by the 2011 off the Pacific coast of Tohoku earthquake. Nokouken Rep 213:145–173Google Scholar
  2. Haraguchi T, Iwamatsu A (eds) (2011) Great eastern Japan earthquake tsunami detail map, Aomori, Iwate and Miyagi edition (p 168) and Fukusima, Ibaragi and Chiba edition (p 98). Kokon-Shoin Publisher, Tokyo, Japan (Japanese)Google Scholar
  3. Haruyama S (1987) Land use of the Tone River basin. Agriculture waster use of the Tone River basin, Agriculture Engineering Association, Tokyo, Japan, pp 25–35 (Japanese)Google Scholar
  4. Haruyama S (1994) Development and environmental conservation in the lake and surroundings -Songklar lake, Laguna lake and Kasumigaura lake. J Int Relat Res 20:25–36 (Japanese) Google Scholar
  5. Haruyama S (2001) Land use planning for disaster mitigation. J Rural Plann 20(2):87–90 (Japanese)Google Scholar
  6. Haruyama S, Hayashi K (2013) Tsunami 2004 disaster impacted by recent land use change in Phuket, Thailand. Haruyama S (ed) Coastal geomorphology and vulnerability of disaster towards disaster risk reduction, TERRAPUB Publisher, Tokyo, Japan, pp 69–86Google Scholar
  7. Haruyama S, Mizuno S (2007) Disaster features and resilience of each local community under 2004 Fukui flooding. J Nat Disaster 26(3):307–322 (Japanese)Google Scholar
  8. Haruyama S, Naruse S (2013) Liquefaction and landform structure in 2011 mega earthquake at Katori city, Chiba Prefecture, Japan. SLUAS science report 2013 towards sustainable land use in Asia (IV), JSPS Science Fund Basic Research (S) No.2122200, pp 100–399Google Scholar
  9. Haruyama S, Oya M (1993) Physical geographical analysis of the Tone River management -lesson from the Akaborigawa channel excavation. J Acad Stud Geogr Hist Soc Sci 41:1–19, The School of Education of Waseda University (Japanese)Google Scholar
  10. Haruyama S, Taresawa Y (2014) Local community activities for disaster reduction in regard to the 2011 tsunami. Geographia Polonica 87(3):299–306CrossRefGoogle Scholar
  11. Haruyama S, Yoshida A (2014) Flood risk under recent land use change in the lower Syonai river basin. SLUAS science report 2014 towards sustainable land use in Asia (V), JSPS Science Fund Basic Research (S) No.21222003, pp 177–188Google Scholar
  12. Hirai Y (1989) Land form feature and geomorphologic development of lagoon in Japan. Geogr Rev 62:145–159 (Japanese)Google Scholar
  13. Honma M (2013) Utilization plan for geological data in real estate transactions and recovery status from liquefaction damages in Urayas city. GSJ Chisitsu News 12(12):357–360 (in Japanese)Google Scholar
  14. Kataoka E (1998) Sawara city history. Sawara city office, p 163Google Scholar
  15. Koarai M (2013) Liquefaction damage of the east Japan great earthquake and evaluation of liquefaction risk using geospatial information. GSJ Chisitsu News 12(12):166–361 (in Japanese)Google Scholar
  16. Koarai M, Nakano T (2013) Liquefaction damage in the Kanto region caused by 2011 of the Pacific coast of Tohoku earthquake in Japan, and the land condition of damaged areas detected by time-series geospatial information. In: The proceedings of 26th International Cartographic Conference, pp 21–32Google Scholar
  17. Koarai M, Nakano T, Okatani T (2015) Relationship between tsunami hazard related to the 2011 off the Pacific coast of Tohoku earthquake and geographical Condition such as topography and land use on the Sendai plain and Ishinomaki plain. J Geogr 124(2):211–226 (in Japanese)CrossRefGoogle Scholar
  18. Komatsubara T (2006) Relationship between micro-topography and damage by the 1894 Meiji Shonai earthquake. J Hist Earthq 21:249 (in Japanese)Google Scholar
  19. Kotoda K, Wakamatsu K, Midorikawa R (1993) Seismic microzoning on soil liquefaction potential based on geomorphological land classification. J Geotech 28(2):127–143 (in Japanese)Google Scholar
  20. Oya M (1969) Geomorphology and flooding of the plain in the middle and lower reaches of the Tone River in Kanto plain. J Geogr 78(5):43–56 (in Japanese) Google Scholar
  21. Oya  M (1993) Fluvial geography. Kokonshoin Publisher. 221–239 (in Japanese)Google Scholar
  22. Oya M, Haruyama S (1987a) Flooding and urbanization in the lowlands of Tokyo and Vicinity. Nat Disaster Sci 9(2):1–12Google Scholar
  23. Oya M, Haruyama S (1987b) Landform of the Tone River basin and the southern part of Kasumigauwa lake. J Ootone. 9(2):2–4 (in Japanese)Google Scholar
  24. Oya M, Kato Y, Haruyama S, Hirai Y, Kobayashi K, Inoue Y, Oshizawa N (1986) Geomorphologic land classification map of Kasumigaura lake. No.1 and No.2. Kasumigaura River Engineering Office, Ministry of Construction, Kanto region construction office (in Japanese)Google Scholar
  25. Oya M, Kinoshita T, Wakamatsu K, Hadori T, Ishii Y (1989a) Shizensaigai wo Shiru and Fusegu (How to know and how to prevent of natural disaster). Kokon-shoin Publisher, Tokyo, Japan, p 236 (in Japanese)Google Scholar
  26. Oya M, Haruyama S, Hirai Y (1989b) Geomorphologic land classification map of lake Kasumigaura, Kitaura and their Vicinity, East of Tokyo. GEOGRAFIA FISICA E DINAMICA QUATERNARIA. Bollettino del Comitato Glaciologico Italiano. Ser.3 12(1):47–50Google Scholar
  27. Saito Y, Inouchi Y (1993) Kasumigaura. Urban Kubota 32:56–64 (Japanese)Google Scholar
  28. Saito Y, Inouchi Y, Yokota S (1990) Geologic history of Kasumigaura- transition history of coastal lake environment effected by sea level changes. J Geol 36:103–118 (in Japanese)Google Scholar
  29. Suzuki Y, Watanabe M, Azuma T, Okada A (1996) Active tectonics of the Rokko-Awaji, and earthquake fault of the southern Hyogo prefectural earthquake of 1955: tectonic geomorphological and paleo-seismological studie and problems. Geogr Rev Japan 69A(7):469–482 (in Japanese)Google Scholar
  30. Takahashi M (1996) Geo-environment analysis of the Hannshinn-Awaji great earthquake disaster. Geogr Rev Japan 69A(7):504–517 (in Japanese)Google Scholar
  31. Taresawa Y, Haruyama S (2013) Coastal landform in the southern part of Miyagi prefecture and 2011 tsunami disaster, coastal geomorphology and vulnerability of disaster towards disaster risk reduction. TERRAPUB Publisher, Tokyo, Japan, pp 87–96Google Scholar
  32. Toyota M, Ikeda H (2003) The formation of lacustrine lowlands around lake Kaumigaura. Geologic environment information bank of Chiba. http://wwwp.pref.chiba.lg.jp/pbgeogis/servlet/infobank.index (in Japanese)
  33. Wakamatsu K (1993) The study of liquefaction vulnerable assessment related with geological condition and geomorphologic condition using historical liquefaction in Japan. Ph. D Dissertation of Waseda University, p 228 (in Japanese)Google Scholar
  34. Wakamatsu K (2012) Recurrent liquefaction induced by the 2011 great east Japan earthquake. Japan Earthq Eng J 12(5):69–88 (in Japanese)Google Scholar

Copyright information

© Springer International Publishing Switzerland 2016

Authors and Affiliations

  1. 1.Graduate School of BioresourceMie UniversityTsuJapan

Personalised recommendations