Distribution of hazards
What is used to measure earthquakes
Used to use Richter scale
Now they use the moment magnitude scale
Moment magnitude - current + more accurate measurementÂ
Interpret and record a broader segment of seismic systemsÂ
How are recurrence intervals of earthquakes useful for risk management?
Recurrence interval = the average time interval that occurs between two recorded events of seismic activity, of equal magnitude, along the same fault.
San Andreas fault = transform boundary |(no volcanoes formed) - two plates moving at different speeds - build up of pressure -- earthquakeÂ
Parkfield section (straight section of the San Andreas fault)Â = magnitude 6Â
Many fault lines in californiaÂ
Recurrence interval = every 20 yearsÂ
Scientists use computer simulations to work out if there's going to be an earthquakeÂ
How wide scale, how many people affected, what areas affected, is there any construction that should not be allowed in an area like this - high risk of damage, eg. airport on this land.
San andreas = big threat to san francisco = less to los angelesÂ
Lower section on fault = recurrence interval is less - 190 yearsÂ
How to prepare for an earthquake - Short and long term
Short term - What individuals can doÂ
Schools - special session on what to do if earthquake
In japan - earthquake prepare drillÂ
Families - first aid kits, water and food, radioÂ
Long termÂ
Reinforce building codes - accentuatedÂ
Power lines - reinforce and redundanciesÂ
Avoid building highways that collapse - redesign the roadsÂ
Hazard zoning
What is used to measure magnitude of volcanoes
VEI = Volcanic explosivity index - 0 to 8 scaleÂ
Amount of erupted tephraÂ
Eruption column heightÂ
Eruption type
VEI levels and examples
0 = trickle of lava - Hawaiian volcano of Kilauea - not tallest part of island but erupts more actively - shield volcanoÂ
1 - gentle eruption - italy stromboli = erupted for almost - Strombolian volcanoÂ
2 - several mild explosions - indonesia mount sinabung has been erupting since 2013Â
3 - catastrophic - lassen peak northern californiaÂ
4 - happen every other year - 2010 iceland Eyjafjallajokull - high in airÂ
5 - things more dramatic - mt vesuvius + mt st helens - blue top + lost altitude + erupt out of side - VolcanionÂ
6 - colossal eruptions - krakatoa - triggered tsunami - 1883Â
7 - every 1000 years - indonesia mt tamboraÂ
8 every 50,000 - yellowstone caldera would reach this level if it were to erupt again - us - national park - so massive that people don't understand it is a volcano - supervolcano - if it erupted = would make big difference - many deaths, people, animals - climate would change. = PlinianÂ
Disaster risk equation
Hazard risk factors - Haiti port au prince 2010
Risk
Risk: To be susceptible to physical or even emotional attack
Capacity
Capacity: The ability of a communtity to absorb and ultimately recover from a natrual disaster
Resilience
Resilience: The ability of a community to bounce back after hazardous eventÂ
Affected by income of countryÂ
Japan = better than Haiti
Hazard
Hazard: The exposure of people to hazardous event which make present a potential threat to people or their possessions including buildings and structures
Vulnerability
Vulnerability:Â
Characteristics + circumstances of community, asset or system that make it available to the damaging effects of a hazard.
Aspects of vulnerability:Â
PhysicalÂ
Social
EconomicÂ
EnvironmentalÂ
Examples:Â
Poor design and construction of buildings - due to governanceÂ
Linadequate protection of asset - people who choose to hold money under bed rather than a bank account - hazard will destroy thisÂ
lack of public information and awareness,
limited official recognition of risks and preparedness measures, and
disregard for wise environmental management.Â
Vulnerability varies across communities and within communities - also over timeÂ
4 aspects of vulnerability
4 types of vulnerability:Â
Physical vulnerabilityÂ
AspectsÂ
 population density
Remoteness of a settlementÂ
SiteÂ
Design and materials used for infrastruatire/housing
Example:Â
Wooden homes are less likely to collapse in earthquake - more vulnerable to fireÂ
Social vulnerabilityÂ
AspectsÂ
Inability of people/organisations/societies oto withstand impacts due to:Â
Inherent social interactions/instituions/systems of cultural valuesÂ
Linked to level of well beingÂ
Levels of literacy and educationÂ
Existence of peace and security + acess to basic human rights
Systems of good fovernanceÂ
Social equity
Positive traditional values
Customs and ideological beliefsÂ
Overall collective organisational systemsÂ
Example:Â
When flooding occurs some citizens - children/elderly/differently-able - unable to protect themselves or evacuate if necessaryÂ
Economic vulnerabilityÂ
AspectsÂ
Economic status of individuals/communities/nationsÂ
Poor = more vulnerable to disasters - bc they lack the recoutrse to build sturdy structures and put other enginneering measures in place to protect themselves from being negatively impacted by disastersÂ
Example:Â
Poorer families may live in squatter settlements because they cannot afford to live in safer (more expensive) areasÂ
Environmental vulnerability
AspectsÂ
Natural resource depletionÂ
Recourse degradationÂ
Example:Â
Wetlands - Caroni Swamp - are sensitive to increasing salinity from sea water, and pollution from stormwater runoff containing agricultureÂ
Progression of vulnerability
People who are more vulnerable than others
PoorÂ
ChildrenÂ
DisabledÂ
ElderlyÂ
Females - Carer roleÂ
For example, according to an Oxfam survey, four times as many women than men were killed in Indonesia, Sri Lanka, and India during the 2004 tsunami because men were taught how to swim and climb trees at young ages, while women were not.
Urban populations can have better access to healthcare and their needs can be more easily met following a disaster.
Initiative that could be taken to reduce vulnerability ro natural disasters
Increase level of preparedness - emergency kits - educationÂ
building prevention in hazard areas
Improve quality of housing and infrastructure
What geographic factors contribute to geophysical hazards becoming disasters?
- Geographic factors = physicalÂ
SlopeÂ
Location - near coast line → create tsunamiÂ
Liquefaction = secondary hazard of earthquakeÂ
Rural vs urban locationÂ
If epicentre in urban location = affect more peopleÂ
Time of dayÂ
Degree of isolation
What geographic factors contribute to geophysical hazards becoming disasters? - examples
2004 Indian Ocean tsunami in Banda Aceh, IndonesiaÂ
Altitude - how close to sea level
Location/Direction of the wave = affect landÂ
Relief plane - how flat or hillyÂ
2021 Nyiragongo eruption in Dominican republic of congoÂ
Gradient of slope - influence where lava flow goes
Valleys were affecting flow of lava Â
Where plumes are - living directly above a plume = must higher riskÂ
Type of eruption - lava erupted from flank of volcanoÂ
2010 7.0 earthquake in HaitiÂ
Tsunami riskÂ
SlopeÂ
Underlying geology that effects shaking ons surface Â
No liquefaction on hillside but near coastÂ
ReliefÂ
2018 in Palu earthquake and tsunami Sulawesi
When tide goes far out it is a sign of the wave - wave = very largeÂ
- Epicentre triggered earthquake which then caused tsunami which channelled into that small area - waves became bigger because less space bc is channelled + triggered liquefaction and landslide
- inletÂ
TIming of event
Most people were asleep - but scientists figured out it is better when they were sleep because if it was during the day thousands of people would have died because of poor infrastructiureÂ
A small matter of what time it occurs can make a huge impact on the exposure to risk.
L'Aquila in italy
Rural vs urban
In urban places - can get help faster in terms ofÂ
emergency aid
search and rescueÂ
temporary shelters
In remote/rural areas it is much more difficult to get in the help fast
Local factors
Type of eruptionÂ
Altitude
Location relative to the direction of tsunami wavesÂ
InletÂ
GeologyÂ
Soil type