Raffles Junior College JC 1 Physical Geography Earthquakes Supplementary Pointers Effects of Earthquakes Tsunami (e.g. Indian Ocean Tsunami): It is a large wave caused by an abrupt displacement of water. Water does not travel with the wave but moves up and down as the wave passes. High crests and low troughs. Usually the wave trough arrives to the shore first, causing the sea level to drop, exposing the seabed. Soon the crest arrives flooding the coastal area. Most tsunamis are generated when the sea floor abruptly deforms and vertically displaces the overlying water. This may be caused by earthquakes or submarine volcanic eruption. Liquefaction (e.g. Niigata, Japan / Mexico City): Occurs when water-saturated sediment is reorganized because of violent shaking. The sediment collapses, expelling water and causing the ground surface to subside. The shaking can suspend sand grains in waterlogged soil so that they lose contact and friction with other grains. Soil in a state of liquefaction has no strength and cannot bear any load. A liquefied sand layer can shoot to the surface through cracks, forming a sandblow/sandboil, depositing sand on the ground. With all the material forced to the surface, the surrounding area sinks unevenly causing buildings to topple. Fire may be a serious problem in earthquakes because water lines may be broken by the quakefiremen cannot put our fires with low water pressure (Kobe 1995) Tall buildings will sustain the least damage if they are located directly at the epicenter because they can withstand the P-waves while S-waves on the other hand, occur far away from the epicenter. Brick buildings are the most vulnerable. Mud-brick structures completely disintegrate, burying people in piles of earth and dust, rather than trapping them in voids of air pockets between building slabs, as in a concrete building collapse. A seiche is a standing wave in a body of water. It is caused by resonances in a body of water disturbed by seismic activity. They are tide-like rises and drops in water levels in lakes. Earthquakes may change water levels in wells, indicating a shift in underground fluid pressure. Landslideshampered relief as roads were blocked Death (loss of economically active individuals) and injuries Destruction of buildings (homes and industries) homeless and joblesspovertypeople turning to selling organs and prostitution to make a living. Damage to infrastructureelectricity and phone lines knocked out, railways and roads damaged Damage to economy (due to a combination of other effects) o decline in tourism 1 o Trade deficitincreased borrowing leading to national debtshampers economic growth o Failure of businesses (communications interrupted, production stoppageloss of revenueunemploymentclosure) Shortage of clean waterwater contaminated Diseases rampant Psychological trauma (Fear and panic)social disorder Environmental pollutionspread of sewage and industrial chemicals Management of Earthquakes Earthquake prediction: o Unusual animal behavior (e.g. missing cats and dogs). No scientific evidence. o Changes in well water level, water content (muddy) (Tangshan Earthquake) o Tiltmeter: measures the tilt of the earth’s surface, similar to spirit level. o Seismic monitoring by the network of seismic stations all over the world. o Recurrence Interval: Large fault ruptures require the build-up of great stress, many years pass between repeated surface ruptures on a single fault. o Foreshocks: used to predict whether a more damaging shock will follow. o Using GPS systems to monitor shifts in rock (San Andreas fault) Mitigation: o Build earthquake-proof buildings using the isolated base technology. It involves using a coil and placing it between the structure and the foundation of the building to counteract the motion of seismic waves. Building can stay nearly stationary as the support moves opposite in direction to the earthquake motion. Cross-supports in between frame supports or the corners of the frame hold the structure together. (Japan) o Hazard mapping: It is probabilistic approach taken to show hazard occurrence level. It takes into consideration the uncertainties in size and location of earthquakes and the resulting ground motions that can affect a particular site. It is used to identify areas prone to hazards such as liquefaction, landslides and ground shaking. These maps are used by insurance companies to set premiums for property insurance. It also help engineers to develop safety code for building construction (e.g. identify safe locations for nuclear waste storage). o Controlled earthquakes: Water under high pressure can be pumped into the ground to trigger earthquakes releasing stress accumulated in rocks. The water acts as a lubricant, allowing rocks to move, causing earthquakes. Without water, rock strain would build up until a large quake occurred. With water reducing friction, strain can be released through smaller timed quakes. 2 o Evacuation measures/warning system o Enforcement of building safety codesretrofitting of structures (Golden Gate Bridge, San Francisco) o Replacing pipelines with semi-flexible material to prevent breakage and gaps pipes with automatic shut-off valves. Circuit breakers to ensure a controlled supply of electricity to minimize electrical fire. o Public educationearthquake drills and basic life support skills (Japan) o In Japan, setting up of “Large-scale Disaster and Emergency Medical Information System”info about bed availabilities, capability of performing surgeryprevents patient transfer from one hospital to another during a crisis Earthquake response o Search and rescue o Immediate relief (medical, shelter, sanitation, food & water, communication (after Kobe Earthquake, Japan, NTT and Motorola provided free telephone service for victims), social order, psychological support) o Some countries refused international aid in light of protecting national pride o Setting up of Earthquake Memorial Park to preserved damaged state to remind people to stay vigilant (Kobe Port) o Reconstruction and recovery and long-term development Problems of Earthquake Hazard Management in LDCs o Population Size (densely populatedhigh death rates) o Lack of Preparedness People are preoccupied with working to make ends meet due to their state of povertythus they view dealing with natural disasters as a lower priority Low literacy rate and poor educationunaware of earthquakes o Low technologyNo money to invest in earthquake prediction equipment such as the tiltmeter and warning systems o Lack of past records/datacannot predict future occurrences o Inaccurate prediction (e.g. animal behavior which is not scientifically proven) o Poor government Does not view earthquakes as a problemput more emphasis on economic development and tradeignoring plight of citizens Weak leadership and indecisiveness Unnecessary protocol and standard proceduresslow response to an emergencyforeign aid may find it difficult to seek permission from an 3 inefficient government (Indonesian government during Indian Ocean Tsunami) Corruptionself-interest o Poor building designlack of funds and certified engineerslow quality materials and outdated building methods (Kashmir Earthquake) o Poor infrastructure/Communications networksome locations are inaccessible to aid, telephone network disrupted o Resistance towards foreign aiddoes not want to depend on otherswants to be self-reliant o Poor Living conditions slum areas are unhygienicovercrowding facilitates rampant spread of diseases. Povertyincreased crime and social disorder 4