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EN
International concept of renovation of the old tumbledown astronomic observatory at the Mt. Pip-Ivan in Charnohora (Eastern Carpathians) and establishment in it the Ukrainian- Polish scientific station emerged seven years ago as a result of a bilateral initiative of the scientists-geodesists from the University "Lviv Polytechnic" and the Warsaw University of Technology. After that, during a whole series of Ukrainian-Polish discussions which included representatives of different scientific institutions, the project of creation of the Ukrainian-Polish geophysical observatory with the permanently working satellite. gravimetric tidal, seismic, magnetic, meteorologic al and eeologieal laboratories as well as with the recreation and tourist centre was developed. It is also envisaged to release in the future this rebuild observatory to the organisation of Central European Initiative (CEl) as the international training and educational centre. In January 2002 the Ukrainian-Polish Coordination Scientific Council was established under the chairmanship of a representative of the lvano-Frankivsk administration district. The deputy chairmen of this Council are: from the side of Ukraine - Dr. Kornelij Tretyak, and from Polish side - Prof. Dr. Janusz Śledziński. In summer 2002 the scientists from the Cracow Academy of Mining and Metallurgy and Lviv Polytechnic carried out successfully the GPS campaign that incorporated few the highest picks in Charnohora including the Mt. PipIvan to the geodynamic network of Eastern Carpathians. The creation of the Ukrainian-Polish geophysical observatory on the top of the highest part of the Eastern Carpathians is commonly recognised as a very nice example of the fruitful and effective cross-border cooperation between Ukraine and Poland. Lately this concept met with approval of the highest government authorities of both countries.
EN
The paper contains a report from studies concerning gravity and position data determination to obtain the plumb-line curvature in the Earth`s gravity field directly in terrain in real time. In the suggested approach quasi-synchronic satellite measurements and gravity determinations ought to be performed at some points not marked round the central station, where the horizontal gradient of anomalies and its azimuth have to be obtained.
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