भूकम्पमापी इसके अंग्रेजी अर्थ का उदाहरण

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

PBO measured Earth deformation through a network of instrumentation including: high-precision Global Positioning System (GPS) and Global Navigation Satellite System (GNSS) receivers, strainmeters, seismometers, tiltmeters, and other geodetic instruments.

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.

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

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 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.

Geodetic imaging data was transmitted, often in realtime, from a wide network of GPS stations, augmented by seismometers, strainmeters and tiltmeters, complemented by InSAR (interferometric synthetic aperture radar), LiDAR (light-activated radar), and geochronology.

The seismometer innovations thereof: James David Forbes.

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.

Modern earthquake location still requires a minimum of three seismometers.

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

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.

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.

भूकम्पमापी हिंदी उपयोग और उदाहरण

""भूकंप का मापन भूकम्पमापी यंत्र से किया जाता है, जिसे सीस्मोग्राफ कहा जाता है।

यह आधार-दस का लघुगणक आधारित पैमाना होता है, जो वुड-एंडर्सन टॉर्ज़न भूकम्पमापी के आउटपुट के सर्वाधिक विस्थापन का संयुक्त क्षैतिज आयाम (एम्प्लिट्यूड) का लघुगणक निकालने पर मिलता है।

भूकम्पमापी (Seismometer)।