Gravimetric Point

a point on the earth’s surface where the acceleration of gravity has been measured and the geodetic coordinates, including elevation, have been determined. In conducting a gravimetric survey, a network of reference points of various categories, as well as of ordinary points, is created. Repeated measurements with highly accurate gravimetric instruments are made on the reference gravimetric points. The initial reference gravimetric point for all gravimetric surveys in the world is a point in Potsdam (German Democratic Republic).

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Gravimetric Survey

References in periodicals archive ?

For topographic correction, the methodology proposed by Kane [34] and Nagy [35] is considered, in order to obtain a grid of topographic correction, which through a sampling operation assigns the correction value to each gravimetric point. Finally, the Bouguer anomaly values are triangular interpolated.

Geomorphology Characterization of Ica Basin and Its Influence on the Dynamic Response of Soils for Urban Seismic Hazards in Ica, Peru

The gravimetric point in Lacko exhibits a drop in the value of acceleration resulting most likely from the expansion of the building in which the measurement station is located.

Geodynamic studies in the Pieniny Klippen belt in 2004-2015

The relative gravity surveys conducted in Tabasalu were connected to the Suurupi absolute gravimetric point (Oja et al.

Precise levelling data processing near terraced landforms

The gravimetric survey was connected to elative gravimetric point FGG2 included into the gravimetric network of the 1st order of 2006 campaign (Kuhar et al.

Analysis of different height systems along the Sava River/ Ivairiu auksciu sisteme prie sava upes analize

As data set for calculations, 1518 gravimetric points (3) were used, covering an area of approx.

Local modelling of quasigeoid heights with the use of the gravity inverse method--case study for the area of Poland

The network of gravimetric points in this region, which includes the Jelenia Gora valley area and the upper part of the Karkonosze, became the part of a research project in 2001.

Ten years of gravimetric monitoring on the points of geodynamic networks in the Sudety Mts