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It shows how great the Alabama Shakes can be when they're not just paying homage to the past.
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Scientists are now willing to accept that the symptoms once equated with shaking can be caused in other ways.
Nevertheless, they continue to decipher how fault ruptures start and stop and how much shaking can be expected near large earthquakes.
This "trunk-shake" can be compared to a human handshake in that it may be associated with similar functions such as assurance and greeting or as a way of assessing strength.
In unveiling the maps last week, scientists at the Southern California Earthquake Center at the University of Southern California advised people living in "hot spots" where shaking can be amplified to stay put and consider retrofitting their homes.
In a FFT analysis, the dominant frequencies of the earthquake shaking can be observed from the amplitude peaks.
Hard sediments or rocks experience lower shaking intensity, but the shaking can be felt at much larger distances from the epicenter.
Dynamic response of most seismological instruments and many engineering structures to ground shaking can be represented via response of a pendulum (single-degree-of-freedom oscillator).
Image with non-uniform blurring caused by camera shake can be modeled as a linear combination of the homographically transformed versions of the latent sharp image during exposure.
We show that, this being the case, a computational method based on a matrix inversion of the linearized constraint equations (MILC SHAKE) can be orders of magnitude faster than the simple SHAKE or RATTLE methods.
The intensity/force of shaking can be adjusted based upon the cell type.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com