2003
DOI: 10.1016/s0013-7952(02)00199-0
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Seasonal movement of the Slumgullion landslide determined from Global Positioning System surveys and field instrumentation, July 1998–March 2002

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Cited by 207 publications
(158 citation statements)
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“…It increases the soil volume and compaction and decreases the pores which will be more vulnerable to vehicles. This finding is similar to that of Feiznia et al (2001) and Coe et al (2003). The liquid index and plastic index and soil moisture have proved the reasons of soil movement and changes from plastic to liquid phase.…”
Section: Resultssupporting
confidence: 92%
“…It increases the soil volume and compaction and decreases the pores which will be more vulnerable to vehicles. This finding is similar to that of Feiznia et al (2001) and Coe et al (2003). The liquid index and plastic index and soil moisture have proved the reasons of soil movement and changes from plastic to liquid phase.…”
Section: Resultssupporting
confidence: 92%
“…The active part of this landslide is about 3.9 km long, and its widths range from 100 m to 500 m [45]. The surface elevation of the landslide ranges from 2750 m to 3650 m [46,47]. The great altitude difference causes the continuous sliding for hundreds of years.…”
Section: Study Area and Experimental Resultsmentioning
confidence: 99%
“…Guerriero et al, 2015). Slow movement is normally concentrated along lateral-slip surfaces (Fleming and Johnson, 1989;Gomberg et al, 1995;Coe et al, 2003;Guerriero et al, 2016) which consist of fault-like segments (e.g. Segall and Pollard, 1980) locally associated with cracks arranged in en echelon sets (Fleming and Johnson, 1989).…”
Section: Introductionmentioning
confidence: 99%
“…Iverson, 2005;Grelle et al, 2014). Thus, most earth flows move faster during periods of high precipitation or snowmelt than during drier periods, and the correlation between precipitation and velocity is normally complex (Coe et al, 2003;Schulz et al, 2009). Earth flow surges can occur when prolonged rainfalls are associated with the loss of efficient drainage pathways (Handwerger et al, 2013) and new sediment becomes available in the source zone through retrogression of the upper boundary (e.g., Guerriero et al, 2014).…”
Section: Introductionmentioning
confidence: 99%