The distance from the earthquake to the observation point is estimated using the arrival time difference of the P-wave and S-wave information needed to determine the distance from the focus of an earthquake to the seismic receiving station.
The distance from the epicenter of an earthquake to the seismic station is determined by the time difference between the first arrival of the P and S waves. This is known as the S-P interval.
Requires triangulation to determine the exact location. Three seismometers are required. A circle is drawn from each of the three different seismometer sites, with the radius of each circle equal to the distance from that seismic receiving station to the epicenter.
Learn more about seismic receiving station at
brainly.com/question/2552673
#SPJ4
Answer:Sphere A has a diameter of 12 and is dialated by a scale factor of 1/2 to create sphere B. What is the ratio of the volume of sphere A to sphere B? oh ok i know what is it A the second one is B
Explanation:
Answer:
Erosion is a geological surface process described as <u>the weathering and sorting of rock and soil.</u>
Explanation:
Erosion -
The geological process by which the earthen material like rock and soil are worn away or carried away by natural forces , which can be wind or water , is called Erosion.
Erosion is exactly opposite to the process of deposition , the geological process of depositing earthen material is called deposition .
Hence,
Erosion is a geological surface process which is described as -
the weathering and sorting of rock and soil.
Answer:
dramatic changes occurred in the way people lived
The answer is D.
(Edited to combat confusion)
