КРУПНОМАСШТАБНОЕ КАРТОГРАФИРОВАНИЕ РЕЛЬЕФА ГОРНЫХ СТРАН (НА ПРИМЕРЕ АЛТАЯ)

Abstract

Relief of mountain areas has very complicated pattern due to interaction between active tectonics and wide range of exogenous processes. Large scale geomorphological mapping based on aerial pictures and satellite images is the most effective and cheap way to determine the sequence and conditions of landforms rise in these regions. The author considers operational principles of analytical geomorphological mapping and methodical approaches that had been developed in the process of some Mountain Altai regions mapping. They include the use of boundaries of new type (which are not similar to slopes' bend) and new designation for objects that unite characteristics of different genetic types.