Earthquakes Flashcards
Faults
fractures in along which displacement occurs
Focus (hypocentre)
source location of the earthquake on the failt
epicenter
point on Earth’s surface directly above the focus
seismic
of, subject to, or caused by an earthquake or Earth vibration
What are body waves and which types of body waves are there?
- Body waves travel through earth
- P-waves (Primary) travel faster
- S-waves (secondary) travel slower
What are surface waves and which types of body waves are there?
Surface waves are slower and cause greatest destruction
- L-waves have largest amplitude, shearing motion
- Rayleigh waves have rolling motion
How to seismometers work?
- mass attatched to moveable frame
- motion of mass damped by its interia
- relative motion recorded on rotating drum, magnetic tape, or digitally
How to locate an earthquake
- Mearuee amplitude of largest wave on record
- Use time between P and S waves to find distance to epicenter
- Line between distance and ampllitude gives Richter magnitude
How many seismic records are needed to locate the epicenter of an earthquake?
3
Focal dapth classifications:
- Shallow: 0-70km
- intermediate: 70-300km
- deep: > 300km
Intraplate earthquakes
- destructive
- strain accumulation not directly related to plate movements, but due to localised strain accumulation
Natural vs anthropogenic earthquake examples
Natural:
- volcanic
- tectonic
- landslide-generated
Anthropogenic:
- rock burst
- fluid injection or extraction
- reservoir-triggered
- explosion
How are the Mercalli Scale and Richter Scale different
- Mercalli Scale is based on damage and effects as a measure of earthquake intensity
- RIchter scale is based on seismographic record
Mercalli Scale advantages
- no strong ground motion seismometers in mainly seismically active regions
- help construct a record of past seirmic activity, important for risk assessment
Mercalli Scale drawbacks
- subjective, inconsistent
- affected by factors such as geology
- no use in uninhabited areas
- cannot distinguish between proximal and distal quakes
- local assessment often reflects maximum rather than average