5.4: Seismic Hazards Flashcards
What is an earthquake?
As the crust of the Earth is constantly moving, there tends to be a slow build up of stress within the rocks. When this pressure is released, parts of the surface experience, for a short period, an intense shaking experience.
What is the focus of an earthquake?
The point at which the pressure release occurs within the crust.
What is the epicentre?
The point immediately above the focus on the Earth’s surface.
How deep is a shallow focus earthquake?
0-70km
How deep is an intermediate focus earthquake?
70-300km deep
How deep is a deep focus earthquake?
300-700km deep
What kind of earthquake causes the greatest damage (shallow, intermediate or deep focus earthquake)?
Shallow focus (0-70km deep).
Accounts for 75% of all the earthquake energy released.
Where do the vast majority of earthquakes occur?
Along destructive plate margins.
Name the most famous fault line (constructive plate margin) that can cause earthquakes.
The San Andreas Fault in California.
What are the different ways in which the magnitude of earthquakes can be measured?
- Richter scale
- Moment magnitude scale (MMS)
- Mercalli scale
Outline the Richter scale.
Measures the magnitude of earthquakes. Uses logarithmic scale on a scale of 1-10.
Outline the the MMS (moment magnitude scale)
Has replaced the Richter scale to identify the energy release from earthquakes - thus measuring magnitude.
Outline the Mercalli scale.
Mercalli scale measures the intensity of an event and its impact. On a 12 point scale (from ‘I. not felt’ to ‘XIII. extreme’).
Give examples of events that occur just before an earthquake strikes.
- bulging of the ground
- microquakes before the main tremor
- raised groundwater levels
- curious animal behaviour
- increased argon gas content in the soil
How can GIS be useful to earthquakes?
GIS are used to prepare hazard maps that show the areas at greatest risk, and thus can planning of urban growth and development.
Outline some primary effects of earthquakes.
- ground shaking: causing buildings to collapse, windows to shatter, sewers to fracture, power lines to collapse.
- ground rupture: the visible breaking and displacement of the Earth’s surface.
- immediate deaths and injuries from crushing, falling glass and transport accidents.
Outline some secondary effects of earthquakes.
- soil liquefaction: when violently shaken, soils with a high water content lose their mechanical strength and start to behave like a fluid.
- tsunamis: giant sea waves generated by shallow focus underwater earthquakes involving movements of the sea bed.
- fires: due to broken gas pipes and collapsed electricity transmission systems.
- landslides: slope failure due to ground shaking.
- effects on people: collapsing buildings, destruction of transport links, flooding, disease spreading, food heritages
What is a tsunami?
Giant sea waves generated by shallow focus underwater earthquakes, violent volcanic eruptions, underwater debris slides and landslides into the sea.
Do tsunamis have a short or long wavelength in open ocean?
Long wavelength
Do tsunamis have a low or high wave height in open ocean?
Low wave height (under 1metre)
How quickly to tsunamis travel in the open ocean?
700km per hour
What happens to the wave height of tsunamis as they reach shallow water bordering land?
Rapidly increase in height
What is the first warning sign of a tsunami?
The wave trough in front of the tsunami, which results in a reduction in sea level (known as a drawdown)
Once on land, how high can a tsunami reach?
In excess of 25m.