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they check the intensity or magnitude of the earthquake.

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14y ago

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Related Questions

What can be used to detect hidden faults?

They can use seismographs


How many seismographs are needed to detect an earthquake?

three


Can seismographs predict hurricane intensity?

No, seismographs cannot predict hurricane intensity. It can only detect and predict any ground movement


How are Seismographs data used?

Seismographs and fault-monitoring devices provide data used to map faults and detect changes along faults.


What are the two types of seismographs?

The two types of seismographs are analog seismographs, which use a pen and rotating drum to record seismic activity on paper, and digital seismographs, which use electronic sensors to detect and record seismic waves digitally.


Can Seismographs only detect earthquakes within 100 miles?

Seismographs can detect earthquakes from far beyond 100 miles if sensitive enough. Sometimes many instruments at great distances are used to calculate the severity of the quake.


Is there any seismograph in Bakersfield?

Yes, there are seismographs in Bakersfield, California, which is located in a seismically active region. Seismographs are used to detect and record seismic activity such as earthquakes. It is important to have seismographs in this area for monitoring and early warning purposes.


What is the shawdow zone?

An area of Earth's surface where seismographs cannot detect an earthquake after waves has passed.


How is an earthquake located?

Seismographs placed around the planet detect the vibrations and calculate the epicenter using triangulation.


How is an earthquake epicentre located?

Seismographs placed around the planet detect the vibrations and calculate the epicenter using triangulation.


What are three ways in which geologists use seismographs data?

They map faults, detect changes along faults, and develop a method of predicting earthquakes


Why do all seismograph around the world detect P waves about me some seismographs around the world detect S waves?

Seismographs around the world detect P waves because these primary waves, or compressional waves, travel faster than S waves (secondary waves) and can move through both solid and liquid layers of the Earth. In contrast, S waves can only travel through solids, which is why some seismographs may not detect them if they are located in areas where the waves encounter liquid layers, such as the Earth's outer core. This difference in wave propagation explains why P waves are universally detected, while S waves are only recorded in specific locations.