Isostatic compensation of the Earth crust is discussed. Using the ETOPO1 digital elevation model and gravity data a Moho model and isostatic anomalies field was constructed for the area of Ukrainian Carpathians, bounded by: φ=47.30÷50,300 N, λ=22÷270 E. Technique for isostatic anomalies calculation is described. Relation between the isostatic anomalies and main tectonics units of region is defined.
Objective. The research objective is to determine relationship between crust tension forces and forces that operate in near-Earth space and earthquakes in entrails of the Earth, based on that was identifying opportunities for short-term earthquake prediction. Methods. Accumulation of earthquakes scores statistical information, their location and display time, as well as moon and sun (own observations, data from literature and Internet-resources) location information. Analysis of obtained data its comparison. Results.
The aim of this article is the role and place of geodesy and gravimetry in the complex Earth Sciences and making recommendations for their using in various fields of knowledge of science. Problem and its relation with important scientific and practical tasks. In the article we consider some issues of the current state and prospects of geodesy and gravimetry. So modern geodesy – natural branch, which includes several areas: geodesy and topography, applied engineering or surveying, marine surveying, space geodesy, higher geodesy and physical geodesy and others.