Final answer:
In the laboratory experiment, the primary purpose is to locate the epicenter of an earthquake by interpreting seismograms. The arrival times of P waves and S waves are estimated to find their difference, which helps in calculating the distance to the epicenter using a travel-time graph. The epicenter is then triangulated using this information from at least three seismograph stations.
Step-by-step explanation:
The primary purpose of the laboratory experiment, where you are acting as an amateur seismologist to locate the epicenter of a fictional earthquake, is C. To locate the epicenter of the earthquake. This is achieved by interpreting seismograms from three seismograph stations.
The main reason for estimating the arrival times of the P waves and the S waves is C. To find the difference between the arrival time of the P wave and the S wave. This time difference is crucial for determining the distance from the seismograph station to the earthquake's epicenter.
Conversion of the time interval between the P wave and S wave arrivals into distance is accomplished D. Using a travel-time graph. This graph correlates the time difference to the distance, using known speeds at which P waves and S waves travel through the Earth.
The primary purpose of drawing a circle around a seismograph station with a radius equal to the distance to the epicenter is C. To triangulate the epicenter of the earthquake. By drawing circles around at least three stations, their intersection will show the epicenter's location.
The correct sequence of steps in the seismology experiment is A. Interpreting seismograms, estimating the distance to the epicenter, locating the seismograph station. These steps are followed to accurately identify the earthquake's epicenter.