Hazards - Seismic hazards, Storm hazards, Fires in nature & Case studies Flashcards
(90 cards)
what is the primary hazard associated with a seismic event?
-an earthquake = a short period of violent ground-shaking resulting from the sudden release of large amounts of energy in the lithosphere
why do earthquakes occur?
-at all boundaries, plates can become stuck due to friction
-when the plates are stuck, the convection currents in the asthenosphere continue to push, which builds the pressure
-all of this pressure is released in a sudden movement, causing a jolting motion in the plates which is responsible for shockwaves spreading out from the focus
what is meant by the focus?
-the point at which the pressure is released within the crust, i.e. where the earthquake originates from
what is meant by the epicentre?
-the point on the earth’s surface that is directly above the focus, i.e. where the earthquake is felt first
what is the spatial distribution of earthquakes?
-the most powerful earthquakes occur along destructive margins, at depth in the Wadati-Benioff zone, e.g. over 80% of large earthquakes occur along the Circum-Pacific belt ( i.e. the Ring of Fire ), where the Pacific plate is being subducted beneath the surrounding plates
-large, shallow-focus earthquakes are produced at conservative margins, e.g. the San Andreas Fault in California, which represents the boundary between the North American and Pacific plates
-earthquakes at constructive margins tend to be lower magnitude than at destructive or conservative margins
-some minor earthquakes occur away from plate boundaries, e.g. in February 2018, an earthquake of intensity 4.6 on the Mercalli Scale was felt over much of Wales and south-west Britain
how is seismicity measured?
-the Richter scale = a measure of the strength of seismic waves ( i.e. the magnitude of an earthquake ) which doesn’t have an upper limit and is logarithmic, meaning that a magnitude 5 earthquake has an amplitude ten times greater than a magnitude 4 earthquake
-the moment magnitude scale ( MMS ) = a measure of the total amount of energy released at the source of an earthquake which, like the Richter scale, is logarithmic and has no upper limit, however it is more accurate
-the Modified Mercalli Intensity scale ( MMI ) = a measure of the intensity of an earthquake and its impacts using observations of the event ( e.g. reports and photos ) running from 1 to 12, with 1 being an earthquake that is only detected by instruments and 12 being one that causes total destruction, however it is subjective
what is the frequency of earthquakes?
-earthquakes are frequent around the world and hundreds of low magnitude earthquakes that cannot be felt by humans occur every day at boundaries, whereas the larger earthquakes are less frequent
what is the regularity of earthquakes?
-earthquakes don’t seem to follow any clear pattern or trend and are largely random, so there is irregularity between events
what is the predictability of earthquakes?
-scientists can monitor the movement of tectonic plates to predict which areas are at risk from seismic hazards, and microquakes may give some indication
-close studies of fault lines can sometimes indicate the point along the fault where the next earthquake could be due ( i.e. a seismic gap ) because earthquakes push pressure and stress to the surrounding rock, which increases that area’s future earthquake hazard risk
-however, it’s currently not possible to accurately predict when an earthquake will strike a particular place, and what magnitude it’s likely to be as how strong they are is random
what are the three types of seismic waves?
-body waves = P and S, surface waves = love and Rayleigh
-primary / pressure ( P ) waves = longitudinal, fastest, least destructive ( lowest amplitude ), can travel through water, air and solids ( mantle and core )
-secondary ( S ) waves = transverse, medium speed, second most destructive, can only travel through solids ( mantle )
-surface waves = can be longitudinal or transverse, slowest, most destructive
what are the secondary seismic hazards caused by earthquakes?
-landslides and avalanches
-soil liquefaction
-tsunamis
what are landslides and avalanches and why are they hazardous?
-shaking of the ground can dislodge rock, soil or snow, causing landslides or avalanches that move downslope quickly
-shaking can also loosen ground material, making it easier for water to infiltrate, and the weight of the extra water may trigger a landslide even after ground shaking has stopped
-e.g. following the Gorkha earthquake in Nepal in 2015, scientists from NASA found that 4,312 landslides occured between the time of the earthquake in April and the onset of the monsoon rains in June, some of which were large enough to block whole valleys and almost completely bury villages, such as Langtang
what is soil liquefaction and why is it hazardous?
-when violently shaken, soils with a high water content ( i.e. saturated / waterlogged soil ) lose their mechanical strength as particles lose contant with each other, causing the soil to act like a liquid
-this makes the soil weaker and easier to deform, so it’s more likely to subside, and buildings tilt or even collapse as the soil can no longer support its own weight, which causes threat to human life
-e.g. the Palu ( Indonesia ) earthquake of 2018 caused major soil liquefaction within and close to the city of Palu, which led to mudflows that submerged many buildings and a whole village
what are tsunamis and why are they hazardous?
-giant sea waves caused by the displacement of large volumes of water
-generated by shallow-focus underwater earthquakes, volcanic eruptions, underwater debris slides and large landslides into the sea
-around 90% of all tsunamis are generated within the Pacific Basin, particularly at convergent plate boundaries where subduction is taking place
-the waves will wash boats and wooden coastal structures inland, and the backwash may carry them out to sea
-people are drowned or injured by the tsunami as both the water itself and the debris that it contains are hazards
-tsunamis are usually more powerful if they start close to the coast because the waves lose energy as they travel towards land
-the waves travel very fast in deep water so they can hit the shore without much warning, meaning that they can cause a high death toll
-e.g. tsunamis generated by the explosion of the volcano Krakatoa, Indonesia in 1883 have been estimated to have drowned over 35,000 people and produced waves that travelled around the world, the highest being over 40 m
what is the formation of a tsunami?
-tectonic upthrust in the form of underwater earthquakes and ocean floor volcanoes displace large volumes of water in a very short space of time, generating a massive amount of energy
-this energy causes a series of progressive oscillatory waves to propogate over the ocean surface in ever-widening circles at speeds as fast as 500 mph
-as the tsunami waves approach the coastline of a landmass, they are slowed by the friction of their collision with the rising seabed, and their wavelengths become shorted and amplitude increases
-finally, with the wavelength compressed and heightened to large levels ( often between 5 and 10 m ), the giant waves collide with the shore causing massive damage e.g. by uprooting trees and washing away people and property
what is an example of a recent tsunami?
-March 2011, off the Pacific coast of the Tohoku region of Japan
-the most powerful earthquake ever recorded in Japan ( magnitude 9 ) occurred 70 km offshore
-tsunamis generated reached over 40 m in height and in some places penetrated over 10 km inland
-these tsunamis devastated part of Japan’s Pacific coast, causing nearly 16,000 deaths with over 6,000 people injured and 2,500 missing
-over 300,000 people were displaced from their homes
-the built environment suffered with 127,000 buildings destroyed and many more damaged
-people living within 20 km of the Fukushima nuclear power plant were evacuated
-the assessed cost of the damage by insurers was over $30 billion, and the estimated economic cost to Japan was $235 billion
-tsunami waves ran right across the Pacific to North and South America, and in Chile the tsunami created waves 2 m high
what are the social impacts of seismic hazards?
-primary = earthquakes can cause buildings to collapse, killing, injuring and trapping people, and leaving others homeless
-secondary = earthquakes and liquefaction can cause gas and power lines to break which starts fires that kill people, water supplies are contaminated as pipes burst which causes flooding and spreads disease due to lack of clean water, tsunamis can flood large areas which causes death and widespread damage to property
what are the environmental impacts of seismic hazards?
-primary = earthquakes can cause fault lines which destroy the environment, liquefaction
-secondary = earthquakes and tsunamis can damage industrial units e.g. power plants which causes leaks of chemicals or radioactive material that damage the environment, fires can destroy ecosystems, saltwater from tsunamis can flood freshwater ecosystems, killing plants and animals, and salinising water and soil
what are the economic impacts of seismic hazards?
-primary = businesses destroyed through ground-shaking and liquefaction
-secondary = economic decline as businesses are destroyed ( tax breaks etc. ), high cost of rebuilding and insurance payout, sources of income lost, damage to industry may lead to reliance on expensive imports of goods and energy
what are the political impacts of seismic hazards?
-primary = government buildings destroyed
-secondary = political unrest from food, water and energy shortages, borrowing money for international aid and to repair damage puts the country in debt, can be initial choas and lawlessness e.g. looting, money that is earmarked for development may have to be spent on repairing damage rather than on development
how is hazard risk managed?
-preparedness = a state of readiness in preparation for an event
-mitigation = the act of reducing the severity of an event
-prevention = the act of stopping something from happening
-adaptation = the act of changing in order to cope with a new situation
how can the impacts of seismic hazards be reduced through preparedness?
-authorities can install earthquake warning systems which detect weaker seismic waves that may be a sign of a more powerful earthquake to come and tsunami warning systems which send out warnings after an earthquake by TV, radio and SMS, giving people a short time to make themselves safe by e.g. going to evacuation centres or higher ground, e.g. in Japan, the ‘Earthquake Early Warning’ system aims to reduce earthquake-related damage by slowing down trains immediately, controlling lifts and enabling people to protect themselves quickly
-earthquake prone areas such as Japan have extensive awareness strategies and education in place ( e.g. Drop, Cover, Hold On )
-evacuation plans and training so people know how to respond during an earthquake e.g. stay away from buildings if possible or find a strong door frame / desk to shelter under if inside
-within the home, heavy items can be secured and breakable items can be stored at a low level
-families can create a communication plan ( e.g. a groupchat ) and establish an emergency meeting place
-households can create emergency supply kits to last a few days which include essential items e.g. tinned food and water, clothing, a radio, a first-aid kit etc.
-communities can set up search and rescue teams or fire response units to tackle the impacts of a hazard
how can the impacts of seismic hazards be reduced through mitigation?
-older, unsafe buildings can be demolished and replaced with ones specially designed to withstand earthquakes ( i.e. earthquake resistant buildings ) which contain features such as strong materials that can flex and sway but rarely collapse e.g. wood rather than concrete or brick, large rubber shock absorbers in the foundations that will allow some movement without structural failure, cross-bracing to better hold buildings together when they shake and a large concrete weight on top of them that, with the aid of a computer program, will move in the opposite direction to the force of the earthquake to counteract stress
-short-term responses e.g. immediate emergency aid, evacuation, and search and rescue
-regions with a high tsunami risk use warning systems ( such as klaxon ) to warn the population before the wave reaches land, which can reduce loss of life if people react immediately and evacuate, but not loss of property
-some countries have built prevention walls up to 12 m in height to break tsunami waves ( i.e. sea walls ), however these have not proved very effective as large tsunamis are likely to overwhelm them
how can the impacts of seismic hazards be reduced through prevention?
-the majority of seismic hazards cannot be prevented and will occur regardless, however it’s sometimes possible to prevent them from posing a risk to people, e.g. authorities can prevent land that is prone to liquefaction from being built on, or build giant sea walls to prevent tsunamis hitting land
-soil liquefaction can be prevented through soil stabilisation, i.e. gravel columns can be put in the ground
-avalanches can be prevented through controlled explosions