S waves arrive second after an earthquake.
P waves
S waves
Triangulation. First, they calculate the time between the first and second - primary and secondary - seismic waves created in an earthquake and use this information to determine how far the seismometer is from the epicenter of the earthquake. A circle is drawn around the seismometer so that it is in the center and the radius is equal to the calculated distance. Using this information from three different seismometers, two more circles are drawn and the intersecting point of the three circles is where the epicenter of the earthquake is located.
s and p waves
Primary waves are the fastest seismic waves originating from an earthquake, traveling at 6 to 7 km per second. Secondary waves travel at about 3.5 km per second.
Missouri lies on the second largest fault line in North America. This fault line is over twenty years past due for major seismic activity. The last great earthquake in Missouri was so violent that it created East St. Louis.
S waves
Triangulation. First, they calculate the time between the first and second - primary and secondary - seismic waves created in an earthquake and use this information to determine how far the seismometer is from the epicenter of the earthquake. A circle is drawn around the seismometer so that it is in the center and the radius is equal to the calculated distance. Using this information from three different seismometers, two more circles are drawn and the intersecting point of the three circles is where the epicenter of the earthquake is located.
s and p waves
seismic waves
The worst US earthquake in terms of impact on people was probably the 1906 San Francisco Earthquake which is estimated to have led to the deaths of over 3,000 people and to have left between 227,000 and 300,000 people homeless out of a population of 410,000. In terms of magnitude, the worst earthquake in recorded US history was the 1964 Alaska earthquake which had a moment magnitude of 9.2. This makes it the most powerful earthquake recorded in the US and Canada and the second most powerful earthquake recorded on Earth by seismometer.
Primary waves are the fastest seismic waves originating from an earthquake, traveling at 6 to 7 km per second. Secondary waves travel at about 3.5 km per second.
A surface wave is the last seismic wave to arrive after an earthquake.
Missouri lies on the second largest fault line in North America. This fault line is over twenty years past due for major seismic activity. The last great earthquake in Missouri was so violent that it created East St. Louis.
These are known as the seismic waves or the s waves. They will reach the earthquake location second after the first shock.
A Mask
the ship carring iago, emilia, desdemona and roderigo arrive second. Not sure about why it would be suprising about othllo
They use the Richter scale to measure the speed of the earthquakes. Levels of earthquakes 2.0 ---> can't be felt 4.0 ---> do not cause damage 5.0---> can cause damage 6.0 ---> considered strong 7.0---> is a major earthquake +++ That is not correct. You have confused speed with intensity. The Richter scale, which is logarithmic, measures the intensity ("strength" if you like). The speed is measured in ordinary linear units like metre/second or km/hr, calculated from observing the earthquake's waves' progress past seismographs around the world.
1. Waves of energy that travel through the Earth. 2. Result of an earthquake, explosion, or a volcano that imparts low-frequency acoustic energy. 3. Seismic waves are studied by geophysicists called seismologists. 4. Recorded by a seismometer, hydrophone (in water), or accelerometer. 5. Types of seismic waves: body wave, surface waves S waves and P waves. 6. Scientists have used indirect measurements and seismic waves from earthquakes to determine the internal structure of the Earth. 7. Scientists have seismographs set up all over the world to track movement of the Earth's crust. 8. Surface waves travel along the surface of the earth. 9. Typically the most destructive type during an earthquake. 10. Seismic waves are not always detectable by seismometers.