Hazards resulting from mass movements Flashcards
Nature/Causes of 2018 mudslides in Southern California
intense rainfall
soft, poorly unconsolidated rock
steep relief of 1547m above sea level
over the San Andreas fault
Impacts of the 2018 Southern California mudslide
23 killed
debris flow 5mtall and 20mph
163 injuries
$207mil of property damage
20,000 lost power and water
Management strategies of the 2018 Southern Californian mudslide
hazard maps with probability of soil liquefaction
land use and building ordinances completed
education and warning programmes
evaluation of attempts to reduce mass movement in Southern California 2018
many ignored evacuation attempts
rock bolts, netting and pinning were not appropriate
Nature/Causes of landslides in Hong Kong
Hilly topography 60% mountains
high population density
monsoon season April-September
impacts on lives and property in Hong Kong
between 1972-2008, 400 fatalities
management and prediction strategies in Hong Kong
first to design and operate a territorial landslide early warning system - 1977
a focus on structural sloe stabilisation
rainfall trackers to help predicition
evaluation of attempts to reduce mass movement in Hong Kong
risk reduced by 50%
ALTHOUGH success has led people to believe they are immune from the dangers
influences on perception of risk
level of education
employment status
religion
family and material status
past experience
personality
socio-economic status
emotional and social responses to risks are:
fatalism
adaptation/adjustment
fear
What does Park’s disaster response cure show
The model shows the deterioration of the quality of life of the people affected and the speed at which the country returns to normality.
What does Park’s model take into account?
hazards are inconsistent
all hazards have different impacts and responses
wealthier countries may recover faster
multiple hazards can occur at once/affect many countries
VARGUS MUDFLOWS: causes of the mudflows
in 52hrs, the rainfall of a year 91cm fell.
slopes had been over-steepened resulting in thousands of shallow landslides which were then liquefied turning them into debris slides
VARGUS MUDFLOWS: characteristics of the mudflows
14.5m per second
river channels were eroded down several m
debris flows overwhelmed pre-existing concrete channels
VARGUS MUDFLOWS: environmental impacts
deposits were a volume of 1.8million cubic m