भूकंपमोमीटर इसके अंग्रेजी अर्थ का उदाहरण

The maximum measured intensity was IX at a seismometer about 4"nbsp;km from the epicentre, with a peak ground acceleration of 147.

Analysis of seismometer records suggests that the rupture propagated towards the east faster than the S-wave velocity (supershear) and to the west slower than the S-wave velocity.

Larger landslide events would most likely be the result of magma intrusion, and thus they would be predicted by seismometers and volcanic surveying devices.

In 1930 a seismometer from Gonzaga University was moved to a basement laboratory at Mount St.

Not only the output of the main photodiode is registered, but also the output of a number of secondary sensors, for example photodiodes that measure auxiliary laser beams, microphones, seismometers, accelerometers, magnetometers and the performance of all the control circuits.

17th-century English male writers The primary purpose of a seismometer is to locate the initiating points of earthquake epicenters.

Modern earthquake location still requires a minimum of three seismometers.

By analyzing the records of earthquakes obtained from this dense grid of seismometers, scientists can learn about Earth structure and dynamics and the physical processes controlling earthquakes and volcanoes.

The Transportable Array is composed of 400 seismometers that are being deployed in a rolling grid across the United States over a period of 10 years.

The PBO network includes several major observatory components: a network of 1100 permanent, continuously operating Global Positioning System (GPS) stations many of which provide data at high-rate and in real-time, 78 borehole seismometers, 74 borehole strainmeters, 26 shallow borehole tiltmeters, and six long baseline laser strainmeters.

Normally, seismometer self noise will be well below the seismic noise level, and every station will have a characteristic noise pattern that can be calculated or observed.

Using signals recorded by the array of seismometers, the EarthScope project will be able to animate seismic waves as they sweep across the USArray transportable array for selected larger earthquakes.

The Global Strain Rate Map (GSRM) is a project of the International Lithosphere Program whose mission is to determine a globally self-consistent strain rate and velocity field model, consistent with geodetic and geologic field observations collected by GPS, seismometers, and strainmeters.