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 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.
To create an acceleration-time graph from a velocity-time graph, you need to find the slope of the velocity-time graph at each point. The slope represents the acceleration at that specific instant. Plot these acceleration values against time to get the acceleration-time graph.
To determine the volume from a graph, you would need to calculate the area enclosed by the graph and the axes. If the graph represents a shape with known cross-sectional area, you can integrate the shape's area over the interval represented by the graph to find the volume.
The y-axis is the vertical line on a line graph.
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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.
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
bar graph,line graph and pie graph