Атлас Антарктики

This article introduces the Soviet project to compile a comprehensive Atlas of Antarctica, initiated in the early 1960s. The project aimed to systematically organize the extensive yet scattered expedition data accumulated during the International Geophysical Year, presenting the latest scientific understanding of Antarctica through a comprehensive atlas. Approved by the USSR Academy of Sciences and involving about 20 institutions, the atlas covers multiple disciplines including geography, geophysics, geology, climate, glaciology, oceanography, and biology. It was planned for publication in loose-leaf format to facilitate updates. The project served both scientific research and education, reflecting Soviet organizational capacity and international perspective in polar science.

An Antarctic atlas in two volumes is being published in the U.S.S.R. The first volume contains about 200 pages of maps, the second about 1000 pages of text. The basic principle of the geographical division of the Antarctic is stated here, emphasizing both its geographical originality and the features of geographical similarity of the zones of the southern and northern hemispheres. The Antarctic and sub-antarctic circles are distinguished. The temperate zone of the southern hemisphere is discerned beyond the Antarctic boundaries, but still within the area of the South Ocean.

This article reviews the organizational, editorial, cartographic, and printing experience accumulated during the creation of the Atlas of Antarctica, a large-scale collaborative project involving research institutes, universities, government agencies, subject specialists, and a cartographic production factory. The broad participation of institutions enabled the project to mobilize extensive expeditionary and archival materials, but geographical and administrative fragmentation created major difficulties in coordination, standardization, and quality control. During editorial preparation, the team developed the atlas layout, general and thematic specifications, sample maps, principles for rendering geographical names, and a preliminary map list. Decisions concerning scale, sheet arrangement, format, projection, and orientation were guided by the need to represent available knowledge of the South Polar Region in maximum detail and to permit independent use and later replacement of individual sheets. Most small-scale maps adopted an azimuthal projection equidistant along meridians, with scale preserved at 70°S, while overview maps were oriented to the Greenwich meridian to facilitate comparison and international standardization. The map list evolved from an unsystematic set of institutional proposals into a structured production schedule and finally a thematic table of contents. This process demonstrated the necessity of preparing authorial sketches before final layout, especially for innovative maps based on incompletely processed sources. However, extensive late-stage revisions weakened the schedule’s coordinating function and caused avoidable corrections. Submitted authorial materials varied substantially in methodology, generalization, legends, graphical treatment, and consistency across adjacent or related maps. Editors therefore had to study Antarctic geography, consult subject experts, and establish a five-stage compilation sequence progressing from standard bases and large-scale materials to thematic syntheses and overview maps. Twenty standard bases were produced, and transparent plastic supports, photographic copying, and shared graphic and color scales were used to ensure spatial and visual consistency. The production process also introduced new photomechanical methods, including wash-off relief duplication, combined printing forms, contact-screen reproduction of halftone originals, masking, and coordinated printing of linework and background colors. These techniques reduced the number of printing runs while maintaining the quality of proofs in the full edition. The experience shows that a major scientific atlas requires early stabilization of its thematic structure, standardized authorial instructions, qualified cartographic editing, carefully planned production order, and close interaction between scientists and manufacturers. Modular sheet design and adaptable printing technology further enhance usability, revision, and long-term scientific value.

This article examines the cartographic design and prepress production of “Antarctica on the Map of the Southern Hemisphere,” the introductory plate of the Atlas of Antarctica. The map was intended to show Antarctica’s geographic relationship to other southern continents while combining spatial credibility with a vivid, three-dimensional representation of Earth. It employed an oblique azimuthal projection developed by the Central Research Institute of Geodesy, Aerial Survey and Cartography, which conveys terrestrial curvature while limiting peripheral distortion. The content includes continents, major inland waters, rivers, landforms, and Antarctic sea ice, with graphic distinctions among perennial ice, seasonal ice, fractures, leads, and current-driven ice transport. Relief, ice, and hemispheric curvature were modeled through colored chiaroscuro under simulated northwestern illumination. The principal technical innovation was a photographic method for producing smooth spherical shading: a matte-painted papier-mâché hemisphere was photographed under controlled lateral lighting, with shielding against stray light and a white reflector to enhance modeling in shadowed areas. The resulting halftone image, together with a continuous relief wash and line originals, was converted into screened transparencies of varying contrast. These were combined with hypsometric layers and multiple color plates; the final map used four line colors and ten background colors. The printed sheets achieved generally strong visual and technical quality, although brighter blue in illuminated ocean areas and richer, less luminous land colors would have improved land–sea contrast. The study demonstrates that photographic modeling can replace labor-intensive manual ink washes while producing more consistent tonal effects. It also argues that such relief-and-globe-style maps are valuable not only in scientific reference atlases but also in education, where they can provide an effective conceptual transition from the globe to the flat map.

The Antarctic Atlas, a product of extensive Soviet collective work, is a comprehensive scientific-reference atlas depicting the natural conditions and exploration history of the South Polar region in maximum detail. Containing around 500 maps, charts, and diagrams, it covers topics from topography and glaciology to climate, oceanography, biology, and geology. Its significance lies in systematizing previously scattered data, establishing new natural boundaries (including recognizing the Southern Ocean as a distinct basin), and refining geographical nomenclature. The atlas holds scientific, practical, and political value, showcasing international cooperation. Its creation also advanced cartographic methodology and provided a framework for future research.

This review examines the first volume of the Atlas of Antarctica, published in the Soviet Union in 1966 to mark the tenth anniversary of Soviet Antarctic expeditions. Drawing on Russian, Soviet, and international observations collected from the discovery of Antarctica through 1963, the work is presented as the first comprehensive atlas devoted to the region. Produced collaboratively by numerous Soviet research institutions, it contains 543 maps together with extensive diagrams, tables, aerial photographs, documentary reproductions, and a geographical index of 4,668 names. Although the Antarctic Convergence generally defines its spatial scope, several maps extend to the Subtropical Convergence or even 10° south latitude. The atlas synthesizes the history of exploration and cartography and organizes contemporary knowledge across aeronomy and geophysics, geology and relief, climatology, glaciology, oceanology, biology, and physical-geographical regionalization. The review concentrates on its climatological, glaciological, and oceanographic sections. It highlights the pioneering climatic regionalization of Antarctica, the representation of ice-sheet thickness, accumulation, snow and firn properties, and the mapping of relationships between atmospheric circulation and ocean dynamics. A specific methodological reservation concerns the use of January and July rather than December and June for solar-radiation maps, given the direct astronomical control of insolation in polar regions. The reviewer also notes that scarce, short, and asynchronous observations sometimes prevented reliance on long-term datasets, an understandable limitation of the relatively recent emergence of coordinated Antarctic research. Overall, the atlas is judged a major interdisciplinary synthesis with lasting importance for cartography, geography, polar science, and the history of Antarctic knowledge.

This review introduces the first volume of the Atlas of Antarctica, published in 1966. Containing approximately 500 maps, diagrams, and illustrations compiled from Soviet and international sources, the volume systematically represents Antarctica’s natural conditions and major scientific findings. Its three sections cover exploration history, general thematic mapping, and detailed regional maps. Topics include topography, geology, geophysics, climate, glaciology, oceanography, and biological distribution, with innovative treatments of the ionosphere, cosmic radiation, terrestrial currents, and subglacial bedrock relief. Large-scale maps, aerial photographs, self-contained legends, explanatory notes, and a bilingual-script place-name index enhance accessibility and practical use. Distinguished by its comprehensive scope and novel cartographic approach, the atlas provides a valuable foundation for Antarctic research, transportation planning, and engineering development.