seismometer
A seismometer is a device that measures ground motion during earthquakes. It detects and records the intensity and duration of seismic waves, providing valuable data for studying and monitoring seismic events.
Surface waves are the earthquake waves that move in a horizontal direction along the ground. They are responsible for the most damage during an earthquake due to their side-to-side shaking motion.
Rayleigh waves move the ground in a rolling motion, similar to ocean waves. They cause particles of material to move elliptically in the direction of wave propagation, leading to both vertical and horizontal motion. This motion is what can cause significant horizontal shaking and damage during an earthquake.
The tracing of an earthquake motion created by a seismograph is known as a seismogram. It represents the ground motion recorded by the seismograph during an earthquake, displaying the amplitude and duration of seismic waves. Seismologists use seismograms to determine the magnitude, location, and depth of an earthquake.
These are known as seismic surface waves. They travel along the Earth's surface and cause the ground to move in a rolling motion. They are responsible for the most damage during an earthquake as they can generate strong shaking and displacement of structures.
A seismograph is the instrument used for recording the intensity and duration of an earthquake. It detects and measures the motion and vibrations of the ground caused by seismic waves.
A seismometer is a device that measures ground motion during earthquakes. It detects and records the intensity and duration of seismic waves, providing valuable data for studying and monitoring seismic events.
Surface waves are the earthquake waves that move in a horizontal direction along the ground. They are responsible for the most damage during an earthquake due to their side-to-side shaking motion.
Surface waves (e.g. Rayleigh waves, Love waves) that produce vertical motion of the ground surface produce the most damage during an earthquake.
A seismograph is used to record shaking or vibrations in the Earth's crust. It consists of a sensitive instrument that detects ground motion caused by seismic waves during an earthquake. The information recorded by a seismograph helps scientists determine the location, intensity, and duration of an earthquake.
Seismometers are instruments that measure ground motion during an earthquake. They detect the movement of the ground caused by seismic waves passing through the Earth. The data recorded by seismometers can help scientists analyze and characterize earthquakes.
A seismograph is a device that detects and measures the magnitude and duration of seismic waves caused by earthquakes and other sources of ground motion. It records the ground motion as a seismogram, which helps seismologists analyze and understand the characteristics of earthquakes.
Rayleigh waves move the ground in a rolling motion, similar to ocean waves. They cause particles of material to move elliptically in the direction of wave propagation, leading to both vertical and horizontal motion. This motion is what can cause significant horizontal shaking and damage during an earthquake.
The tracing of an earthquake motion created by a seismograph is known as a seismogram. It represents the ground motion recorded by the seismograph during an earthquake, displaying the amplitude and duration of seismic waves. Seismologists use seismograms to determine the magnitude, location, and depth of an earthquake.
These are known as seismic surface waves. They travel along the Earth's surface and cause the ground to move in a rolling motion. They are responsible for the most damage during an earthquake as they can generate strong shaking and displacement of structures.
the motion is called seismogram
A seismometer is used to measure the intensity of an earthquake by detecting and recording the ground motion caused by seismic waves. It provides data on the amplitude and frequency of the seismic waves, which helps in determining the earthquake's magnitude and duration.