A seismograph.
A longer answer
A seismograph or seismometer is one kind of instrument that is used to measure the effects of earthquakes. There are a number of different types of seismometers and they all work in slightly differing ways but generally are based around the same principle.
That principle is inertia. Inertia basically means that stationary masses will remain stationary until a force is applied to them. Conceptually a seismometer can be thought of as a weight or mass, suspended by springs in a frame which is bolted to the floor.
When an earthquake occurs the frame which is attached directly to the floor is caused to move by the seismic waves, however the mass / weight on the spring does not as the seismic waves do not directly affect it (their effect is dampened by the inertia of the mass and the springs). If you were to attach a pencil or pen to the weight and a piece of graph paper to the frame so that they were touching the movement of the frame relative to the stationary mass would be recorded.
Modern seismometers are much more complex than this but in essence rely on this principle.
During an earthquake there can also be substantial permanent ground deformations. As such, seismologists will attempt to measure the movement of the crust around a fault zone to estimate the total strain that has accumulated. This measurement is often made using high precision GPS to measure relative positions of surface features around the fault zone. They may also use terrestrial laser scanning equipment which can measure changes in the ground shape (recording deformation) or by using a special form of radar and a technique called synthetic aperture radar interferometry (InSAR for short). This process essentially involves the use of a radar to create a series of very accurate relief maps of the ground surface over time and then to compare the maps to create a final plot showing the changes between them which is a record of the land surface deformation.
They may also use strain gauges and tilt metres within boreholes to observe ground deformations as well as a technology known as time domain reflectometry which is an electrical technique used to locate damage and deformation in electrical cables and which in turn can be used to measure subsurface deformations.
what are the instruments that is used to measure the earthquakes
A seismometer.
A type of geophysicist known as a seismologist measures the strength of earthquakes.
there hands
Used to measure earthquake activity with sound waves.
VibrationsA seismoscope is an instrument used to measure vibrations of the earth's crust. Generally, scientists use these readings to predict when an earthquake will strike. They can also use this to measure the length and magnitude of an earthquake. More Information:The seismoscope is the earliest instrument; excluding people, puddles, and bowls of standing water; used to detect seismic events (movements or shifts within the Earth's crust, or earthquakes). Even the earliest known model (132 AD. Chinese, Zhang Heng) recorded the direction of these disturbances. Later models detected and indicated the direction, time, and crudely, the power of each disturbance. This instrument is rarely used by scientists today, having been replaced by a more sensitive, and more capable instrument, the seismometer. Both instruments should be distinguished from seismographs,which are the graphs of seismic activity, produced by the modern equivalents of these instruments.
seismograph is one instrument that could measure earthquakes and volcanoes etc but seismograph is many times use at earthquake!
Scientists use seismographs.
the rictor scale
A seismometer is used to measure the strength of earthquakes.
A seismogragh and/or seismometer.
The strainmeter, by which its seismometer component detects the vibrations or shock waves that its seismograph records, is the scientific instrument that's used to predict and measure earthquakes.
A seismograph is an instrument used to measure the strength of earthquakes.
Seismograph
a tool used by scientists to measure earthquakes by movement
A seismometer or seismograph will measure the amplitude and frequency of seismic waves which are produced by earthquakes.
Scientists use a recording instrument called a seismograph to detect ground motions caused by seismic waves from earthquakes.
A seismograph is an instrument that records movements within the earth. A seismogram is the actual recording that scientists look at when studying earthquakes.