Hazard Magnitude & Frequency (DP IB Geography)
Revision Note
Written by: Bridgette Barrett
Reviewed by: Jenna Quinn
Risk Management & Hazard Magnitude
Magnitude and risk management
The magnitude is the strength of a hazard and often refers to the amount of energy released
Most hazards are measured using a scale:
Earthquakes – Moment Magnitude Scale, Mercalli Scale and Richter Scale
Volcanoes – Volcanic Explosivity Scale
Higher magnitude events usually result in greater impact
Earthquake magnitude
Magnitude is the most common way to measure an earthquake
This is a measure of the energy released at the source (focus):
The magnitude can be measured on different scales
The most well-known scale is the Richter Scale
The one that is increasingly used now and is reported on the news when an earthquake occurs is the Moment Magnitude Scale (MMS)
The MMS goes from 1, which is not felt by humans, to 10
The MMS is a logarithmic scale, which means that a 6 on the scale is a ten-times increase in amplitude from a 5:
The energy release is 32 times greater
Diagram to show the magnitude of earthquakes
Earthquake intensity
The intensity of an earthquake is its impact on people, as well as the built and natural environments
The Modified Mercalli Intensity Scale is used to measure the intensity
The scale goes from I to XII
The Modified Mercalli Intensity Scale
Examiner Tips and Tricks
Remember not to confuse magnitude and intensity.
Magnitude is the amount of energy released, whereas intensity is the severity of ground shaking at a particular place based on the effects on humans, buildings and the environment.
Measuring volcanic eruptions
Every eruption is unique; some are gentle, others are hugely explosive
The Volcanic Explosivity Index (VEI) is used to measure the size of an eruption
This can not be measured on a scientific instrument so is calculated based on a series of measurements and observations:
These include:
Height of material ejected into the atmosphere
Volume of material
Duration of the eruption
This is a logarithmic scale from 0–8
Diagram to illustrate the Volcanic Explosivity Index (VEI)
Risk Management & Hazard Frequency/Recurrence
The recurrence interval of a hazard event is measured in years
It is the expected occurrence of an event of a particular size
Large magnitude events have a longer recurrence interval than smaller magnitude events
This means there are many small-scale earthquakes, eruptions and landslides and few large-scale ones
Recurrence of Earthquakes of Different Magnitudes
Magnitude | Average number annually |
---|---|
8+ | 1 |
7 – 7.9 | 15 |
6 – 6.9 | 134 |
5 – 5.9 | 1319 |
4 – 4.9 | 13,000 |
3 – 3.9 | 130,000 |
2 – 2.9 | 1,300,000 |
Based on data from USGS
Recurrence of Volcanic Eruptions of Different Magnitudes
Magnitude | Occurrences In last 10,000 years |
---|---|
8 | 0 |
7 | 7 |
6 | 51 |
5 | 166 |
4 | 421 |
3 | 868 |
2 | 3,477 |
1 | Many |
0 | Many |
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