A time-distance graph shows how long it takes for different seismic waves to travel a certain distance.
A seismograph is used to sense seismic waves in the earth. The seismic waves are sent down by scientist and how fast and how straight the line is when the seismograph reads them is how they tell which mineral or if its a liquid or solid. Which is how they know about the inner and outter core, and the mantel.
Seismic studies show evidence of mid-ocean ridges where new oceanic crust is forming, supporting the theory of seafloor spreading. By analyzing seismic waves, scientists can map the structure of the ocean floor and identify areas of tectonic activity where plates are moving apart. Additionally, seismic data reveals the presence of magnetic striping on the seafloor, further supporting the idea of seafloor spreading.
The outer core is liquid and convects. The mantle also convects, although it is almost entirely solid and it is a matter of debate whether the entire mantle convects, or whether there are seperate layers each individually convecting.
A seismograph typically consists of a drum or digital display connected to a sensing device that records ground vibrations caused by earthquakes. The sensing device, typically a pendulum or mass on a spring, produces a trace on the paper or screen to show the intensity and duration of the seismic waves. Modern seismographs can also use electronic sensors to capture seismic data digitally.
Like a polyghraph squiggles show the techtonic plates moving.
Comparison of waves going through the solid inner core and those just skimming it can show the rotation of the inner core.
A seismograph records earthquake waves.the correct answer is a seismometer a seismograph is the graph to show the recordings
Seismic waves are measured using seismometers, which detect the ground vibrations created by seismic events like earthquakes. Seismometers record the data in the form of seismograms, which show the amplitude and arrival times of different types of seismic waves such as P-waves and S-waves. By analyzing these seismograms, scientists can determine the characteristics of the seismic event and its location.
very carfully
The epicenr can be found by location the sound in the waves carried.
To read a seismograph and interpret seismic activity accurately, first, understand that a seismograph records ground motion caused by earthquakes. Look at the seismograph's wavy lines, called seismograms, which show the intensity and duration of seismic waves. Identify the P-waves (primary waves) and S-waves (secondary waves) to determine the earthquake's location and magnitude. Compare the seismogram with data from other seismographs to confirm the earthquake's characteristics.
sunlight blocks out S waves in certain regions.
I can simulate various types of surface waves, such as ocean waves or seismic waves, using numerical methods to model their behavior and propagation characteristics. The simulation can show how the wave moves and interacts with different types of surfaces or boundaries.
they both show in crease but a line graph may show decrease
A graph does not cook your meals when you are hungry! A graph does not show causation.
The seismograph for a larger earthquake would show stronger and more prolonged seismic waves compared to a smaller earthquake. The amplitude and duration of the seismic waves recorded by the seismograph would be greater for the larger earthquake.
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