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Abstract
The principal task in studying recent crustal movements at the present stage, along with elaborating theoretical concepts, continues to be that of accumulating quantitative information about as many parameters as possible which characterize the spatial, temporal and energetic spectra of these movements. The author deals with some questions of improving the geodetic methods and instruments and makes an attempt to show the accuracy with which the speed of recent horizontal and vertical crustal movements can be measured today and in the future.
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