4 min 55 s
100 minutes.
0.0067 minutes.
It is 100 minutes, which is 1 hour and 40 minutes.
21,600 seconds.
To convert hours to minutes, you would use the ratio 1 hour = 60 minutes. Therefore, to convert 2.4 hours to minutes, you can multiply 2.4 by 60 to get 144 minutes.
P-waves, or primary waves, travel faster than other seismic waves, typically at speeds of about 6 to 8 kilometers per second. If the earthquake occurred 4,000 kilometers away and the P-wave arrived at 7:32 PM, it would have taken approximately 500 to 667 seconds (about 8 to 11 minutes) to reach the station. Subtracting this time from 7:32 PM, the earthquake likely occurred between 7:21 PM and 7:24 PM at the station.
To estimate the distance from the seismograph station to the earthquake epicenter, we can use the typical speed of P waves (approximately 6 km/s) and S waves (approximately 3.5 km/s). The time difference between the P wave and S wave arrival is 2 minutes (or 120 seconds). Given that P waves travel faster, we can calculate the distance using the time difference, which would be approximately 360 km from the epicenter to the station.
The 1923 Kamchatka earthquake, also known as the Great Kamchatka earthquake, lasted only about 10 minutes. It occurred on February 3, 1923, and had a magnitude of 8.2. This powerful earthquake caused significant damage in the Kamchatka Peninsula region.
about 100 or less kilometers. the Alaskan earthquake lasted about 5 minutes and had a magnitude of 9.2 in Richter scale. that was a very destructive earthquake since it is the third strongest earthquake read by the seismograph in the world and the strongest in north America.
It would take about 5-7 minutes for the primary or P-waves to reach a seismograph station in Miami, Florida from Seattle, Washington. These waves travel faster than secondary or S-waves, which would arrive a few minutes later.
The 1964 Alaska earthquake, also known as the Great Alaska Earthquake, lasted approximately 4 minutes. It occurred on March 27, 1964, and is the most powerful recorded earthquake in North American history.
To calculate the distance from the earthquake epicenter based on the difference in arrival times of P-waves and S-waves, we use the fact that P-waves travel faster than S-waves. The average difference in arrival time is approximately 1 minute for every 8 kilometers (5 miles) from the epicenter. Given an arrival time difference of 8 minutes and 40 seconds (which is 8.67 minutes), the distance would be about 69.36 kilometers (or approximately 43.2 miles) from the epicenter.
The Great Alaska Earthquake, also known as the Good Friday Earthquake, lasted for about four and a half minutes. It occurred on March 27, 1964, and remains one of the most powerful recorded earthquakes in history.
The L'Aquila earthquake in Italy occurred on April 6, 2009 and lasted for just a few moments. However, the effects of the earthquake were long-lasting, leading to significant damage, casualties, and ongoing recovery efforts.
The Japan earthquake in 2011 lasted for about 6 minutes.
There was an earthquake five minutes ago
The tsunami took approximately 2 hours to reach Sri Lanka after the earthquake that triggered it occurred in 2004.