172193 An earthquake generates both transverse $S$ and longitudinal $P$ waves in the earth with speeds $4.5 \mathrm{~km} \mathrm{~s}^{-1}$ and $8.0 \mathrm{~km} \mathrm{~s}^{-1}$ respectively. A seismograph records that the first $P$-wave arrives 3.5 minutes earlier than the first $S$ wave. From the seismograph, the epicenter of the earthquake is located at a distance.
172193 An earthquake generates both transverse $S$ and longitudinal $P$ waves in the earth with speeds $4.5 \mathrm{~km} \mathrm{~s}^{-1}$ and $8.0 \mathrm{~km} \mathrm{~s}^{-1}$ respectively. A seismograph records that the first $P$-wave arrives 3.5 minutes earlier than the first $S$ wave. From the seismograph, the epicenter of the earthquake is located at a distance.
172193 An earthquake generates both transverse $S$ and longitudinal $P$ waves in the earth with speeds $4.5 \mathrm{~km} \mathrm{~s}^{-1}$ and $8.0 \mathrm{~km} \mathrm{~s}^{-1}$ respectively. A seismograph records that the first $P$-wave arrives 3.5 minutes earlier than the first $S$ wave. From the seismograph, the epicenter of the earthquake is located at a distance.
172193 An earthquake generates both transverse $S$ and longitudinal $P$ waves in the earth with speeds $4.5 \mathrm{~km} \mathrm{~s}^{-1}$ and $8.0 \mathrm{~km} \mathrm{~s}^{-1}$ respectively. A seismograph records that the first $P$-wave arrives 3.5 minutes earlier than the first $S$ wave. From the seismograph, the epicenter of the earthquake is located at a distance.
172193 An earthquake generates both transverse $S$ and longitudinal $P$ waves in the earth with speeds $4.5 \mathrm{~km} \mathrm{~s}^{-1}$ and $8.0 \mathrm{~km} \mathrm{~s}^{-1}$ respectively. A seismograph records that the first $P$-wave arrives 3.5 minutes earlier than the first $S$ wave. From the seismograph, the epicenter of the earthquake is located at a distance.