Landslides Caused by Climate Change and Groundwater Movement in Permafrost Mountain

  • Shan W
  • Guo Y
  • Hu Z
  • et al.
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Abstract

Abstract Long-haul travel does not constitute an obstacle for tourists to travel and is fast gaining the attention of tourists in new and unique experiences. This study was conducted to identify the long-haul travel motivation by international tourists to Penang. A total of 400 respondents participated in this survey, conducted around the tourist attractions in Penang, using cluster random sampling. However, only 370 questionnaires were only used for this research. Data were analysed using SPSS software 22 version. The findings, ‘knowledge and novelty seeking’ were the main push factors that drove long-haul travel by international tourists to Penang. Meanwhile, the main pull factor that attracts long- haul travel by international tourists to Penang was its ‘culture and history’. Additionally, there were partly direct and significant relationships between socio-demographic, trip characteristics and travel motivation (push factors and pull factors). Overall, this study identified the long-haul travel motivations by international tourists to Penang based on socio-demographic, trip characteristics and travel motivation and has indirectly helped in understanding the long-haul travel market particularly for Penang and Southeast Asia. This research also suggested for an effective marketing and promotion strategy in pro- viding useful information that is the key to attract international tourists to travel long distances. Keywords:

Figures

  • Figure 1. High-latitude permafrost distribution in Northeast China (data from Zurich University, Switzerland), and the location of study area.
  • Figure 2. Annual average maximum temperatures, average temperatures, average minimum temperatures and aver‐ age precipitation in Sunwu County (1954–2013).
  • Figure 3. Permafrost distribution map in K176 + 500–K180 + 000 section of Bei’an-Heihe Highway.
  • Figure 4. Full view of K175 + 500–K180 + 200 section of Bei’an-Heihe Highway (blue line is the boundary of the land‐ slides, the orange area is corn field).
  • Figure 5. Satellite photos of K176 + 500–K179 + 900 section of Bei’an-Heihe Highway (Google earth). (A) Landslide in K178 + 530 section (in 2000); (B) satellite photos of K178 + 530 (2004.6); and (C) satellite photos of K178 + 530 (2010.9).
  • Figure 6. Geological map of K177 + 400–K179 + 200 section of Bei’an-Heihe Highway.
  • Figure 7. Landslide scene photos: (a) Panoramic view of landslide (in November 2014); (b) the trailing edge of land‐ slide (in June 2010); and (c) the leading edge of landslide (in October 2013).
  • Figure 8. Drilling borehole layout on Landslide K178 + 530 and the geomorphological map of the landslide area (using SURFER software to draw the geomorphological map based on GPS terrain data in June 2010).

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CITATION STYLE

APA

Shan, W., Guo, Y., Hu, Z., Wang, C., & Zhang, C. (2016). Landslides Caused by Climate Change and Groundwater Movement in Permafrost Mountain. In River Basin Management. InTech. https://doi.org/10.5772/63068

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