Final answer:
Chebyshev's Theorem suggests that approximately 94% of the times between seismic events fall within 4.2 standard deviations of the mean, after rounding to the nearest whole number.
Step-by-step explanation:
According to Chebyshev's Theorem, the inequality 1 - \(1/k^2\), where k is the number of standard deviations from the mean, can be used to determine the minimum proportion of observations that fall within k standard deviations of the mean. For k = 4.2, we first calculate k^2 which is 4.2^2 = 17.64. Then, applying Chebyshev's inequality, we get:
1 - \(1/17.64\) = 1 - 0.0567 = 0.9433 or 94.33%
Rounded to the nearest whole number, this gives us 94% as the approximate percentage of times between seismic events that are within 4.2 standard deviations of the mean.