Step 1 :The magnitude of an earthquake is measured relative to the strength of a 'standard' earthquake, whose seismic waves are of size \(W_{0}\). The magnitude, \(M\), of an earthquake with seismic waves of size \(W\) is defined to be \(M=\log \left(\frac{W}{W_{0}}\right)\). The value of \(M\) is called the Richter scale rating of the strength of an earthquake.
Step 2 :Let \(M_{1}\) and \(M_{2}\) represent the magnitude of two earthquakes whose seismic waves are of sizes \(W_{1}\) and \(W_{2}\), respectively. We know that \(M_{1}=\log \left(\frac{W_{1}}{W_{0}}\right)\) and \(M_{2}=\log \left(\frac{W_{2}}{W_{0}}\right)\). So, \(M_{2}-M_{1}=\log \left(\frac{W_{2}}{W_{0}}\right)-\log \left(\frac{W_{1}}{W_{0}}\right)\). Using the properties of logarithms, we can simplify this expression to \(\log \left(\frac{W_{2}}{W_{1}}\right)\).
Step 3 :The April 2017 earthquake 69 km SSE of Adak, Alaska, had a rating of 5.1 on the Richter scale. The 1883 Krakatoa eruption released the energy equivalent of a magnitude 8.5 earthquake. So, the difference in their magnitudes is \(8.5-5.1=3.4\). Using the formula we derived, we can find the ratio of the seismic waves' sizes.
Step 4 :The seismic waves of the Krakatoa eruption were approximately \(\boxed{30}\) times larger than those of the Alaska earthquake.