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This is known as a seismogram.

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15y ago

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The trace that records an earthquake from seismic instruments is called a?

the ground movement caused by seismic waves


What is a seismic trace?

A seismic trace is a graphical representation of seismic data collected during seismic surveying. It shows how the amplitude of seismic waves changes over time and can be used to identify subsurface structures like rock layers or hydrocarbon reservoirs. Seismic traces are essential in geophysics for interpreting subsurface geology.


How does a seismograph measure ground movement?

A seismograph measures ground movement by detecting and recording seismic waves generated by earthquakes. It consists of a mass on a spring that remains stationary while the ground moves during an earthquake, resulting in the mass moving relative to the instrument's frame. This movement is then amplified and recorded as a seismic trace.


What produces a record of seismic waves?

A seismograph is an instrument that produces a record of seismic waves by detecting and measuring the vibrations caused by earthquakes or other seismic events. It consists of a seismometer to detect ground motion and a recording device to produce a trace of the detected seismic waves.


How a seismograph looks like?

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.


How do scientists work out the epicentre of an earthquake?

S-waves and P-waves emit from the focus (epicenter) at the same time, yet one of them is faster than the other. therefore the S waves and P waves are directly proportional to each other. So all one needs is to do the math and trace the distance between the waves and there, you have found the Focus (epicenter) of the earthquake.


How long was the fault and how did scientists find this information out?

The fault that caused the 1906 San Francisco earthquake has an estimated length of about 296 miles (477 km). Scientists determined this information by studying the surface rupture, seismic waves, and geologic features left behind by the earthquake, combined with geological mapping and trenching techniques along the fault trace.


How can I background check my daycare provider?

Childcarebackground.com is a website which provides background information on daycares and nannys. They will check their criminal records, DMV records, and address trace.


Is there a way to trace an empty 1955 40MM Artillery Shell?

No, no records kept for fired artillery cases.


What type of manufacturer is Trace Elliot?

The Trace Elliot company was based in the UK and made bass amplification devices and acoustic instruments. The company was sold in 1998 and the UK based factory was closed in 2002.


What is the difference between a seismograph and the Richter scale?

Seismic waves are the vibrations from earthquakes that travel through the Earth; they are recorded on instruments called seismographs. Seismographs record a zig-zag trace that shows the varying amplitude of ground oscillations beneath the instrument. Sensitive seismographs, which greatly magnify these ground motions, can detect strong earthquakes from sources anywhere in the world. The time, locations, and magnitude of an earthquake can be determined from the data recorded by seismograph stations. The Richter magnitude scale was developed in 1935 by Charles F. Richter of the California Institute of Technology as a mathematical device to compare the size of earthquakes. The magnitude of an earthquake is determined from the logarithm of the amplitude of waves recorded by seismographs.


Which part of the seismograph moves as the ground shakes during an earthquake?

The part of the seismograph that moves during an earthquake is called the pen.