Geophysical and bathymetric results have been used for the study of the transitional zone between the Eurasian continent and the Arctic Ocean, which is being considered by the authors as a junction area of continental margins with the adjacent seaward structures, and is dependent of the actual type of the crust found beneath the ocean.The deep Arctic Ocean comprises different types of crust: basins have an oceanic crust with increased sedimentary thickness; the Lomonosov and Mendeleev Ridges have crusts close to subcontinental; and the crust of the Gakkel Ridge is typically mid-oceanic. At least four types of transition zones may be distinguished: (1) 'normal' transition zone, where the 'granitic' layer is wedging out and the crust consists of a thinned sedimentary layer and 'basalt'; this is the junction of the continent and the oceanic basin; (2) a zone where the continental crust thins to the oceanic crust, the 'granitic' layer is absent, and the 'basalt' layer is underlain by the 7.5 km/s layer, rather than the normal mantle; this is represented by the junction of the continent with the rift zone of the median ridge that juts out into the shelf and extends under the continent; (3) a zone where the continental crust thins, the 'granitic' layer is wedging out, but the crust does not thin to the oceanic crust, mainly because of an increase in thickness of sediments; this zone is a junction of the continent with a basin with subcontinental crust; (4) a zone where the continental crust thins, but does not reach oceanic thickness; this is a junction of the continent with the oceanic crust. In the transition zones of the first and third types structural downwarping compensated by the sediments has been developed.The development of the transition zone of the Arctic was intermittent in the geological past, which we see expressed by the asymmetric development of the Greenland–Canadian and Eurasian sectors. These examples of different structures of transition zones are not unique. The transition zone between the Asiatic continent and the Indian Ocean appears to be most similar in its complexity to the transition zone of the Arctic Ocean. However the 'normal' type of transition zone characteristic of much of the continents of Australia, South America, Africa, and parts of other continents frequently occurs here.

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Introduction. The regional geographic information system, being a tool for information and analytical support for making managerial decisions, has been widely used in almost all areas of the Federal Service in the field of consumer protection and human well-being, increasing their effectiveness and efficiency. Purpose. To analyze the effectiveness of the use of a regional geographic information system in solving the problems of the sanitary and epidemiological well-being of the region and to assess the prospects for the development of this system in the activities of the service. Material and methods. Retrospective analysis of the results of the adopted management decisions to improve the state of the environment and health of the population based on the implemented regional geographic information system. Results. The conducted retrospective analysis showed the high efficiency of using regional geoinformation systems when performing environmental and hygienic studies to assess the state of public health, environmental pollution, and in particular, to establish cause-and-effect relationships between the influence of environmental factors on public health and medical demographic indicators. Limitations. The limitation of the study is due to the inability to analyze the long-term experience of using geoinformation systems in solving the problems of sanitary and epidemiological well-being, as well as the lack of indicators of the effectiveness of their use on examples from other regions. Conclusion. The use of geoinformation technologies makes it possible for the authorities of the region to visually present information on priority hygienic and epidemiological problems in a particular administrative territory, and helps to determine the priorities for developing measures aimed at preserving the health of the population.

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