Case Study: Nepal Earthquake Flashcards
When and where did the earthquake occur?
In the morning of 25th April 2015 NE of Kathmandu in Nepal
What was the magnitude of the quake and the depth of the focus?
Main quake was 7.8 (an aftershock was 7.3)
Focus was very shallow (15km deep)
Is this a high-risk area for earthquakes?
Very. One of the most seismically hazard regions.
Outline at least four different factors that make the area particularly vulnerable to earthquakes – social, economic, physical, and political
- Economic: It is an LIC with a very low GNI - less than $3000 per capita
- Economic & Political : Building construction and infrastructure are of a poor quality e.g., building codes not enforced, unsurfaced roads, power cuts
- Political: The is a problem with corruption
- Social: An area of rapid population growth with high population density in Kathmandu valley
- Physical: Kathmandu is built on river sediments (unconsolidated material) – this amplifies seismic waves
How many people died?
9,000
How many were injured
23,000
How many homes were damaged or destroyed in Nepal?
700,000
What primary hazard caused most of the fatalities and where were most people killed?
Collapse of unreinforced buildings – in rural areas
Which secondary hazards resulted in significant loss of life and injury? Give details.
Landslides – there were 5000 landslides, 200 died in the Langtang landslide alone
Avalanches – e.g., 19 killed at Mt. Everest base camp
Economic cost of the Earthquake
Over $5billion in damages
What secondary impact became a big challenge in rural areas?
Access to clean water – land shifts closed up existing water sources that communities relied upon
Loss of tourism revenue was a short- term loss. Which employment sector suffered in the longer term?
Agriculture
Impacts were felt beyond Nepal. Give details
78 killed in India and 25 in China
20 HEP stations in the region damaged
What surprised scientists about the way the sediments beneath Kathmandu behaved in the earthquake? How was this beneficial?
The sediments absorbed the energy of the seismic waves rather than amplifying it as expected. This resulted in less damage to buildings in the city
There were fewer landslides than expected? What were the possible reasons for this?
- The rock in the region was stronger than expected
- Vegetation on the slopes (including rhododendron
forests) helped stabilise slopes