The three waves that are shown on a seismogram in order are P waves, S waves, and surface waves.
Seismologists align the seismogram with the time-distance graph by identifying the arrival times of seismic waves, specifically the Primary (P) and Secondary (S) waves, on the seismogram. They measure the time difference between these wave arrivals to determine the distance to the earthquake's epicenter using the time-distance graph, which correlates these arrival times to distances. By matching the observed arrival times on the seismogram with the corresponding distances on the graph, they can accurately locate the earthquake's source. This process helps in understanding the event's magnitude and depth.
The word is seismogram.
Relative age can be determined using superposition and cross-cutting relationships. Absolute age can only be determined using radiometric dating methods, such as Rb-Sr.
color
Seismogram is a proper noun.When you type Seismogram you capitilize the S.
seismogram
Tsunamis
Most of vibrations can be detected and recorded by sensitive instruments called seismograph, or seismometers. The record produced by a seismometer is called a seismogram.
"Shake, Rattle, and Roll". But seriously folks, it's called a "seismogram".
The three waves that are shown on a seismogram in order are P waves, S waves, and surface waves.
The highest amplitudes on a seismogram are typically associated with the strongest seismic waves, such as surface waves. These waves have the most energy and cause the largest vibrations in the ground, resulting in the highest amplitudes recorded on the seismogram.
I am determined not to answer your question.
Seismologists align the seismogram with the time-distance graph by identifying the arrival times of seismic waves, specifically the Primary (P) and Secondary (S) waves, on the seismogram. They measure the time difference between these wave arrivals to determine the distance to the earthquake's epicenter using the time-distance graph, which correlates these arrival times to distances. By matching the observed arrival times on the seismogram with the corresponding distances on the graph, they can accurately locate the earthquake's source. This process helps in understanding the event's magnitude and depth.
epicenter
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seismogram and seismograph!