In geoscience studies, one of the main problems facing geomorphologists is access to analysis outcomes that are interpretable within the framework of landforms and geomorphical processes. This problem is impossible to tackle without some previous fieldwork and direct observation, especially with regard to small-scale phenomena.
Although remote sensing and image processing can, to some extent, help toward solving this problem, these images are not as easy to access as topography maps.
This paper is based on the implementation of a research project, and sets out to explain a method by which geomorphic processes are interpreted by studying and analyzing the forms of contour lines in topographic maps.
To achieve our purpose, thirty areas were assessed during fieldwork, and then landforms, contour patterns and the nature of land and formative systems were classified within the framework of an empirical-deductive method to determine the relationship holding between them.
The most important conclusion from this investigation is that the form of contour lines in topographic maps displays spatial content, in the sense that, by relying on certain topical principles, and without having access to geological information, one can get to know with elatively high precision the form, process and the nature of the sediments characteristic of a particular area.