Seismology highlights from BSSA February issue
Feb 5, 2010 - 5:00:00 AM
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Small earthquakes can generate exceptional peak accelerations (over 5 m/s2). This compilation includes earthquakes with magnitudes as small as 4.1. The smallest earthquake causing one of the 100 largest PGA on the list had a magnitude 4.8, and the smallest earthquake causing one of the 100 largest PGV was a magnitude 5.7.
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By Seismological Society of America,
[RxPG] Feb. 5, 2010 (San Francisco, CA) -- A new study identifies earthquakes through July 2007 that have produced 100 of the strongest peak accelerations (PGA) and 100 of the strongest peak velocities (PGV) ever recorded. The threshold for the first list is acceleration of the ground exceeding 7.31 m/s2 (74% of gravity), while the threshold for the second is velocity exceeding 0.65 m/s. Crustal earthquakes dominate the lists. Exceptionally strong ground motions exceeding these levels have been observed on sites with the softest soils and sites with the hardest rock. [A copy of the paper is attached below.]
Acceleration measures how fast speed (velocity) increases.
The size of these ground motions matter to the engineers as they design structures to resist earthquakes, said John Anderson of the Nevada Seismological Laboratory and Department of Geological and Engineering Sciences at the University of Nevada. But ground motions that have not yet been recorded also matter. There may be a limit that earthquake motions will never exceeded. Although we expect to eventually record earthquake shaking stronger than what I report in this paper, those higher motions appear to be quite rare, and a motivation for this study was to help to constrain upper limits.
Small earthquakes can generate exceptional peak accelerations (over 5 m/s2). This compilation includes earthquakes with magnitudes as small as 4.1. The smallest earthquake causing one of the 100 largest PGA on the list had a magnitude 4.8, and the smallest earthquake causing one of the 100 largest PGV was a magnitude 5.7.
Of the 255 time histories identified in this study, 40 records have PGV exceeding 1.0 m/s. The largest PGV is 3.18 m/s, recorded on the hanging wall of the thrust fault during the Chi-Chi, Taiwan earthquake on September 20, 1999 (Magnitude 7.6). Also, 35 records have PGA greater than gravity (9.8 m/s2, or 1 g). The largest acceleration in this data set is about 23.8 m/s2 (about 2.4 times gravity), recorded on the hanging wall of the thrust fault during the Nahanni earthquake in northern Canada on December 23, 1985 (Magnitude 6.9). It has already been exceeded by a 2008 record from Japan with PGA that was greater than 4.1 g,, but that later record was not available when this data was compiled. While motions that large appear to be quite rare, with recent expansions of instruments, more records as large as those in the current top 100 are being obtained every year.
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