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 graph used to measure earthquakes is called a seismogram. It records the ground motion during an earthquake and helps seismologists analyze the earthquake's characteristics, such as magnitude and duration.
The tool that graphs seismic waves as wavy lines is called a seismograph. It records the motion of the ground caused by seismic waves during an earthquake, producing a visual representation of the intensity and duration of the seismic activity. The resulting graph is known as a seismogram.
A travel time graph illustrates the relationship between the time it takes for seismic waves to travel from an earthquake's epicenter to various seismic stations. By measuring the arrival times of primary (P) and secondary (S) waves at different stations, seismologists can determine the distance from each station to the epicenter. Using triangulation, they can plot these distances on a map to pinpoint the exact location of the earthquake's epicenter, as the intersection of circles drawn around the stations will reveal the epicenter's location.
The momentum-time graph is the integral of the force-time graph. that is, it is the area under the curve of the f-t graph.The momentum-time graph is the integral of the force-time graph. that is, it is the area under the curve of the f-t graph.The momentum-time graph is the integral of the force-time graph. that is, it is the area under the curve of the f-t graph.The momentum-time graph is the integral of the force-time graph. that is, it is the area under the curve of the f-t graph.
Earthquake waves are detected and measured using instruments called seismometers or seismographs. These devices sense the vibrations caused by seismic waves and convert them into electrical signals, which are then recorded on a graph. The data collected helps seismologists analyze the earthquake's magnitude, depth, and location. Additionally, networks of seismometers can provide real-time monitoring of seismic activity.
one is a graph and the other isnt
The graph used to measure earthquakes is called a seismogram. It records the ground motion during an earthquake and helps seismologists analyze the earthquake's characteristics, such as magnitude and duration.
A seismogram is a graph that displays the ground motion recorded by a seismometer during an earthquake. Seismograms are used to determine important characteristics of the earthquake, such as its magnitude, depth, and location.
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.
A seismogram is a record of an earthquake that's obtained from a seismic instrument. It's in the form of a graph.
The seismogram usually consists of squiggly lines because it records the vibrations of the Earth caused by seismic waves, while the one you first investigated might have been a simpler chart or graph. Seismograms provide more detailed information about the intensity, duration, and frequency of earthquakes compared to other types of earthquake data.
Graphs are typically read from left to right, as this is the direction in which the independent variable (usually time or data points) is increasing. Reading from right to left would be the opposite direction and may not align with the intended interpretation of the data on the graph.
The tool that graphs seismic waves as wavy lines is called a seismograph. It records the motion of the ground caused by seismic waves during an earthquake, producing a visual representation of the intensity and duration of the seismic activity. The resulting graph is known as a seismogram.
A seismograph is a machine that measures the shaking of an earthquake. It consists of a ground motion sensor, which records the movement caused by seismic waves, and produces a seismogram, which shows the intensity and duration of the shaking. Scientists use this data to analyze the characteristics of earthquakes and to monitor seismic activity.
the five graph is line graph,bar graph,pictograph,pie graph and coin graph
bar graph, double bar graph, line graph, and picto graph
its a graph