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terrain factorscontributingto slope instability
the main factorscontributingto slope instability
Evaluation of FactorsInfluencingSlope Instability
the crucial factorscausingslope instability in the
the various factorscontributeto slope instability
the relevant factorsinfluencingslope instability
These factors combinedto causeslope instability
assess factorscontributingto slope instability
the most significant factorstriggeringslope instability
physical factorsleadto slope instability
These methods ... the factorsinfluencethe slope instability
the human factorsresultin slope instability
the specific causal factorscontributingto slope instability
many factors including(passive) can be caused bySlope instability
outside trigger factorscausinginstability of the slope
areas with unstable slopes and local factorscan causeslope instability
Shocks - A sudden shock , such as an earthquakemay triggerslope instability
conditioning factors , a series of elements of the terraincontributeto slope instability
the causes of landslides and the role of the principal factorscontributeto slope instability
A numerical rating system ... five factorscontributeto slope instability
His testimony , that wave action from the lake and other environmental factorscauseslope instability
A number of factors , including human actions and natural phenomenacan contributeto slope instability
a series of factors characterising the geomorphic hazards ( either passive or activemay causeslope instability
Three key factors ... Geology - weak soil composition and strengthcontributeto slope instability
Often excavation for road construction and widening projects ... certain geological and geotechnical factorscauseslope instability
Shocks and vibrations - A sudden shock , such as an earthquakemay triggerslope instability
the increase of groundwater pressure(passive) caused byslope instability
Slides like this ... steep slopes , thick colluvial soils , and undercutting of the slope by road construction or streamscreateslope instability
mainly ... the unfavorable change of hydrodynamic condition in the slope due to reservoir filling and/or operation(passive) to be caused ... by以小時為基本時間單位較為合適。Reservoir slope instability
land usecausingslope instability , etc
changescauseslope instability
Unsaturated Soils ... rain infiltration in unsaturated soilscan triggerslope instability
the rapid deposition of sediment from the fluvial systems e(passive) caused byd. Slope instability
to map the areas more potentially proneto triggerslope instability p
The water table ... the sitecontributedto the slope instability
salt movements in a complex deep - water environment Bryant Canyon area northwest Gulf of Mexico(passive) caused bySlope - instability processes
increasing groundwater pressure(passive) caused byslope instability
soil shear strength and increased weight of soilcausingslope instability [ 3
indiscriminate hill cutting activities and heavy rainfall(passive) caused bySlope instability
processes and mechanismsinfluencingthe slope instability
to landslides and slumpingleadingto landslides and slumping
landslides and snow avalanchesmay causelandslides and snow avalanches
elevated groundwater pressure(passive) caused byelevated groundwater pressure
to mudslides and landslides , subsidence and other geologic hazards , fires and floodsleadingto mudslides and landslides , subsidence and other geologic hazards , fires and floods
to landslides , a victorious geological hazardleadingto landslides , a victorious geological hazard
to landslides , a in the 1964 alaska earthquakeleadingto landslides , a in the 1964 alaska earthquake
in large landslides and debris flowsresultingin large landslides and debris flows
to landslides , a major geological hazard which collapse and cause floodsleadingto landslides , a major geological hazard which collapse and cause floods
to a massive movement of land masses known as landslidesleadingto a massive movement of land masses known as landslides
rising groundwater pressure(passive) caused byrising groundwater pressure
landslides that spill into rivers ... increasing the likelihood of floods down valleycan provokelandslides that spill into rivers ... increasing the likelihood of floods down valley
to A risk of landslides and landslides that can generate both infrastructure losses and human losseswould leadto A risk of landslides and landslides that can generate both infrastructure losses and human losses
in landslides in the hilly regions of north - east India including Mizoramresultingin landslides in the hilly regions of north - east India including Mizoram
in likely disruption to infrastructure and people.[103resultingin likely disruption to infrastructure and people.[103
G20 Summit | Rightways « Landslide tragedy(passive) caused byG20 Summit | Rightways « Landslide tragedy
2019 Landslide tragedy(passive) caused by2019 Landslide tragedy
to landslides and eventually sediment transport in the deep valleys and gorges in this part of the Himalayaleadingto landslides and eventually sediment transport in the deep valleys and gorges in this part of the Himalaya
coseismic landslides , which cost 1.5 million US$ / year in Javaeventually triggeringcoseismic landslides , which cost 1.5 million US$ / year in Java
to one major landslide blocking the lake in 2006 and other landslides affecting the main road and the water dam infrastructure alsoledto one major landslide blocking the lake in 2006 and other landslides affecting the main road and the water dam infrastructure also
Tech War Landslide tragedy(passive) caused byTech War Landslide tragedy
water to come into contact with residual hot rocks leading to small hydrovolcanian events close inshore of Rittercausingwater to come into contact with residual hot rocks leading to small hydrovolcanian events close inshore of Ritter
Refereed ] Geological disasters(passive) caused byRefereed ] Geological disasters
from seepage forcesresultingfrom seepage forces
huge problems for the people of this hilly zone ... not so much for the number of victims ( < 15 in the 340 years analyzed in Table 1 ... but for the extent of the land involved : just think that in some municipal areas such as Serravalle Langhe and Bossolasco , the area involved in landslides represents 40–42 % of the total area [ 5createshuge problems for the people of this hilly zone ... not so much for the number of victims ( < 15 in the 340 years analyzed in Table 1 ... but for the extent of the land involved : just think that in some municipal areas such as Serravalle Langhe and Bossolasco , the area involved in landslides represents 40–42 % of the total area [ 5
at 1 km Fasham road after region at Friday 841(1)29 ... that following it , at two place with 30 m distance was caused a pitch 40 cm amountwas causedat 1 km Fasham road after region at Friday 841(1)29 ... that following it , at two place with 30 m distance was caused a pitch 40 cm amount
landslide because of continuous rainfallcauseslandslide because of continuous rainfall
in slough slides on earthen leveesresultingin slough slides on earthen levees
in the Guilherme Creek watershed ( Nordeste Municipality , S. Miguel Island , Azorestriggeredin the Guilherme Creek watershed ( Nordeste Municipality , S. Miguel Island , Azores
IntroductionAt present , landslide phenomenon(passive) caused byIntroductionAt present , landslide phenomenon
to one major landslide blocking the lake in 2006 and other similar phenomena affecting the main road and the water dam infrastructure alsoledto one major landslide blocking the lake in 2006 and other similar phenomena affecting the main road and the water dam infrastructure also
evacuation order in Central Okanagan West Dozens of people evacuated near Kaslo due to unstable slopes Landslide risk near Knox Mountain promptscausesevacuation order in Central Okanagan West Dozens of people evacuated near Kaslo due to unstable slopes Landslide risk near Knox Mountain prompts
due to a retaining wall built during Portuguese regime ... instead of improving the conditionhas causeddue to a retaining wall built during Portuguese regime ... instead of improving the condition
in extensive landslide material , which was subsequently reworked during a storm to deposit a debris flow that dammed the valleyresultedin extensive landslide material , which was subsequently reworked during a storm to deposit a debris flow that dammed the valley
from the displacement jump , which leads the status of the slope to change and the potential energy of the system also to changeresultsfrom the displacement jump , which leads the status of the slope to change and the potential energy of the system also to change
to the DART sliding away downslopemay have ledto the DART sliding away downslope
to a blockage of the tunnel inlet or the outletcan leadto a blockage of the tunnel inlet or the outlet
a full day search yesterdaypreventinga full day search yesterday
typicallyresultstypically
issues with the park ’s trail leading down to the lower waterfall and until a strategy for stabilizing the slope is madehas createdissues with the park ’s trail leading down to the lower waterfall and until a strategy for stabilizing the slope is made
potential pipeline movement(passive) caused bypotential pipeline movement