3. Earthquakes. The Richter Seale is used to measure the intensity of earthquakes using the formula \( R=\frac{2}{3}(\log E-11,8) \) where \( E \) is the energy released by the earthquake measured in ergs. a. The San Francisco earthquake of 1906 registered \( R=8,2 \) on the Richter seale, How many ergs of energy were released? b. In 1989 another San Francisco earthquake registered \( R=7, I \) on the Richter seale, How many times stronger (in terms of energy released) was the 1906 earthquake than this one? c. Ifone earthquake registers 2 points more than another on the Richter scale how many times more energy does it release?
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To find out the energy released in the 1906 San Francisco earthquake with a magnitude of \( R = 8.2 \), we can rearrange the formula \( R=\frac{2}{3}(\log E-11.8) \). By substituting \( R \) in the equation, we can determine \( E \). The energy released is approximately \( E = 10^{(8.2 \times \frac{3}{2}) + 11.8} \) ergs, which results in an energy release of about \( 1.99 \times 10^{15} \) ergs. For the 1989 earthquake with \( R = 7.1 \), we use the same formula to calculate the energy released. Following the steps, we find \( E \approx 7.94 \times 10^{13} \) ergs. To determine how many times stronger the 1906 earthquake was compared to the 1989 one, we simply divide \( 1.99 \times 10^{15} \) by \( 7.94 \times 10^{13} \), yielding the answer: the 1906 earthquake was approximately 25 times stronger in terms of energy released. If one earthquake registers 2 points higher than another on the Richter scale, it releases roughly \( 10^{(2 \times \frac{3}{2})} = 10^3 \) times more energy. Hence, a difference of 2 points on the Richter scale translates to a staggering 1,000 times increase in energy release!