Example  3

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When an earthquake occurs, different kinds of seismic waves are produced. Two types of seismic waves are S-waves and P-waves, which travel at different velocities. A seismic station can estimate the distance to an earthquakeโ€™s epicentre by comparing the amount of time that elapses between the two types of waves reaching the station.

An earthquakeโ€™s epicentre occurs \(48 \thinspace \rm{km}\) away from seismic station 1, and \(91 \thinspace \rm{km}\) away from seismic station 2. If the seismic stations are known to be \(112 \thinspace \rm{km}\) apart, what is the angle formed at seismic station 2 between seismic station 1 and epicentre 1?


There are three known sides and an unknown angle involved, so you can use the cosine law. It helps to draw a diagram.



Write down what is given.

\(\angle C = \thinspace ?\)
\(a = 112\thinspace \rm{km}\)
\(b = 91\thinspace \rm{km}\)
\(c = 48\thinspace \rm{km}\)

\(\begin{align}
 \cos C &= \frac{{a^2 + b^2 - c^2 }}{{2ab}} \\
 \cos C &= \frac{{\left( {112} \right)^2 + \left( {91} \right)^2 - \left( {48} \right)^2 }}{{2\left( {112} \right)\left( {91} \right)}} \\
 \cos C &= 0.908... \\
 \angle C &= \cos ^{ - 1} \left( {0.908...} \right) \\
 \angle C &= 24.686...^\circ  \\
 \angle C &\doteq 24.7^\circ  \\
 \end{align}\)


The angle formed at seismic station 2, between seismic station 1 and epicentre 1, is approximately \(24.7^\circ\).