Problem 76
Question
Two separate seismograph stations receive indication of an earthquake in the form of a wave traveling to them in a straight line from the epicenter and shaking the ground at their locations. Station \(\mathrm{B}\) is \(50 \mathrm{~km}\) due east of station A. The epicenter is located due north of station A and \(30^{\circ}\) north of due west from station B. (a) Draw a sketch and use it to determine the distance from the epicenter to A. (b) Determine the distance from the epicenter to B. (c) Station \(C\) is located an additional \(20 \mathrm{~km}\) east of \(\mathrm{B}\). At what angle does \(\mathrm{C}\) report the direction of the epicenter to be?
Step-by-Step Solution
Verified Answer
(a) Approximately 43.30 km to A, (b) 50 km to B, (c) Report angle approximately 76.87° to north-west.
1Step 1: Set Up the Geometry
To solve this problem, first sketch the scenario. Place Station A at the origin of a coordinate plane. Since the epicenter is due north of Station A, draw a vertical line north from A to label the epicenter E. From Station B (50 km east of A), draw a line at 30° north of west to the epicenter E. Station C is 20 km east of Station B.
2Step 2: Use Trigonometry to Find Distance from Epicenter to A
We know Station B (denoted as point B) is 50 km east from Station A. The line BE makes a 30° angle with the westward horizontal line at B. Using trigonometry, \( AE = BE \cdot \cos(30°) \). Substitute \( BE \) with the distance from B to E when it becomes known.
3Step 3: Apply Law of Cosines for Distance from Epicenter to B
In triangle ABE, apply the law of cosines to find BE: \( BE^2 = AB^2 + AE^2 - 2 \cdot AB \cdot AE \cdot \cos(B) \), with \( AB = 50 \text{ km} \), and \( B = 30° \). Solve for \( BE \).
4Step 4: Calculate the Exact Distance from Epicenter to B
Given \( B = 30° \), with triangle sides as \( AB = 50 \text{ km} \) and \( AE = BE \cdot \cos(30°) \), use the cosine angle to solve for \( BE \) (distance from epicenter to B). Be sure to rearrange and simplify:
5Step 5: Tackling Station C's Angle to the Epicenter
Station C is an additional 20 km east of B, making it 70 km east of A. Use the tangent in triangle ECB to find the angle where \( x = AE \), and \( z = 70 \) (since AC = 70) : \( \tan(\theta) = z/x \). Use arc tangent to find the angle \( \theta \) reported by Station C.
Key Concepts
Seismograph StationsTrigonometryLaw of Cosines
Seismograph Stations
Seismograph stations are crucial in detecting the occurrence of earthquakes. These stations use specialized instruments called seismographs to receive signals or waves from underground seismic activities. Each seismograph records the waves through time, marking the distinct arrival of wave types. This information is integral to pinning down the earthquake's epicenter or the point on the earth's surface directly above where the earthquake starts.
In this particular exercise, two seismograph stations, A and B, are mentioned. Station A is positioned at the origin point of a coordinate grid, and station B is located 50 km eastward. The exercise assumes these positions to effectively utilize trigonometry and geometry, enabling easy calculation of distances and angles in relation to the earthquake's epicenter. The geographic placement of these stations helps triangulate the epicenter using the arrival times of the seismic waves. By integrating other stations, like station C which is placed further east, it's possible to enhance the accuracy of locating the epicenter and measuring earthquake-related data.
In this particular exercise, two seismograph stations, A and B, are mentioned. Station A is positioned at the origin point of a coordinate grid, and station B is located 50 km eastward. The exercise assumes these positions to effectively utilize trigonometry and geometry, enabling easy calculation of distances and angles in relation to the earthquake's epicenter. The geographic placement of these stations helps triangulate the epicenter using the arrival times of the seismic waves. By integrating other stations, like station C which is placed further east, it's possible to enhance the accuracy of locating the epicenter and measuring earthquake-related data.
Trigonometry
Trigonometry plays a fundamental role in solving geometric problems, especially those involving angles and distances. In the context of the problem at hand, trigonometry helps find the distance from the epicenter to each seismograph station and also the angle at which the epicenter is seen from a particular station.
One of the key trigonometric functions used here is the cosine function. For instance, when we know the direction from station B to the epicenter forms a 30° angle north of west, the cosine function aids in relating the known distances with the unknown distance from the epicenter to station A by the formula \( AE = BE \cdot \cos(30°) \). This allows us to determine the horizontal distance traveled by the wave in the direction of A.
Moreover, when looking from station C, which lies further east, we use the tangent function. It helps divide the distance traveled east from station A (70 km in total) by the distance from A to the epicenter to calculate the angle \( \theta \) using the formula \( \tan(\theta) = \frac{z}{x} \). This assures accurate angular measurements from different viewpoints on this imaginary grid.
One of the key trigonometric functions used here is the cosine function. For instance, when we know the direction from station B to the epicenter forms a 30° angle north of west, the cosine function aids in relating the known distances with the unknown distance from the epicenter to station A by the formula \( AE = BE \cdot \cos(30°) \). This allows us to determine the horizontal distance traveled by the wave in the direction of A.
Moreover, when looking from station C, which lies further east, we use the tangent function. It helps divide the distance traveled east from station A (70 km in total) by the distance from A to the epicenter to calculate the angle \( \theta \) using the formula \( \tan(\theta) = \frac{z}{x} \). This assures accurate angular measurements from different viewpoints on this imaginary grid.
Law of Cosines
The law of cosines is a useful formula when dealing with non-right triangles, enabling the calculation of a side or angle, given sufficient information about the other sides and angles. It is especially crucial in scenarios where right-angle trigonometry doesn't apply, like in our problem.
The law of cosines is expressed as: \[ c^2 = a^2 + b^2 - 2ab \cdot \cos(C) \] where \( c \) is the side opposite the angle \( C \), and \( a \) and \( b \) are the other two sides of the triangle.
In the context of this exercise, we apply the law of cosines in triangle ABE. By setting the known distances, \( AB = 50 \text{ km} \) and \( \angle B = 30° \), this formula helps determine the distance from the epicenter, denoted as \( BE \). Substituting these values into the formula helps solve for \( BE \), establishing a crucial measurement that informs subsequent calculations, like determining angles for station C’s observations. This meticulous approach ensures a comprehensive understanding and accurate solutions.
The law of cosines is expressed as: \[ c^2 = a^2 + b^2 - 2ab \cdot \cos(C) \] where \( c \) is the side opposite the angle \( C \), and \( a \) and \( b \) are the other two sides of the triangle.
In the context of this exercise, we apply the law of cosines in triangle ABE. By setting the known distances, \( AB = 50 \text{ km} \) and \( \angle B = 30° \), this formula helps determine the distance from the epicenter, denoted as \( BE \). Substituting these values into the formula helps solve for \( BE \), establishing a crucial measurement that informs subsequent calculations, like determining angles for station C’s observations. This meticulous approach ensures a comprehensive understanding and accurate solutions.
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