Abstract

The authors describe the results of an experiment in compiling a data base for a global digital terrain model from information contained on a 1:15,000,000-scale hypsometric map. Particular emphasis is placed on strategies for digitizing terrain data from the original map. A key feature affecting the results of such modeling is the delineation of continental boundaries—whether at the ocean shoreline or the edge of the continental shelf. Translated by Edward Torrey, Alexandria, VA 22308 from: Geomorfologiya, 1991, No. 2, pp. 25–31.

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