Lecture 4 - Earthquakes, the basics Flashcards
What is the difference between a right stepping and a left stepping right lateral fault?
Right stepping - The land is pulled apart at the fault bend whenever the fault moves, It creates a hole that could become a basin. Left stepping - The land is pushed together when the fault moves. Eventually could grow into a mountain
Where is the epicenter on the Earth’s surface?
Directly above the hypocenter.
What is the hypocenter?
Where the rupture began
Why does the epicenter not fall on the trace of the fault at the surface?
The dip of the fault.
What are the basic principles of how a seismometer works?
- The earth moves moving the framework of the seismometer. - The suspended heavy weight and then pen beneath remain relatively stationary. - As the concrete base moves the stationary pen draws an ink line on paper on the rotating drum.
Define amplitude, wavelength and the period of waves
- Amplitude: height of the waves above starting point - Wavelength: distance between successive waves - Period: time between successive waves = 1/frequency
Give standard strengths of body and surface waves
Body waves - 0.5 to 20 Hz Surface waves - 0.005 to 0.1 Hz
Name and describe the two types of body waves
- P-waves: Travel fastest, like the push-pull motion of slinky toy (4.8km/sec in granite) - S-waves: Move in an up and down motion perpindicular to direction of advance, like the waves in a shaken rope. (3km/sec in granite)
What are surface waves?
- Created when body waves hit surface. - They are similar to the waves created by throwing a rock into a lake
What kinds of waves compose the surface waves?
- Love waves (horizontally polarized) and Raleigh waves (cause horizontal and vertical movement) - Travel slower than body waves but less attenuation because of long wavelength and low frequency
LEARN
How are earthquakes located using triangulation?
- Need three seismic stations
- Measure the P-S arrival times and convert these to distance
- Triangulate using radius given by P-S travel times
Name and briefly describe the use of the three magnitude scales
- Mercalli: measures damage done by an earthquake
- Richter scale: measures the energy released during an earthquake (ML=log10A-0.15+1.6log10D) where A is the amplitude of the P-wave in mm
- Moment magnitude (M): The seismic moment of the earthquake; the rigidity of the Earth x the amount of slip on the fault plane during the earthquake
Potential energy is stored in the crust in the form of built-up stress. During an earthquake, this stored energy is transformed. What does it result in?
- Cracks and deformation in rocks
- heat
- radiated seismic energy (Es)
What is the seismic moment a measure of?
The total amount of energy that is transformed during an earthquake. Only a small fraction of the seismic moment is converted into radiated seismic energy which is what seismographs register.
This means that 99% of the energy produced by earthquakes we cannot measure!