Abstract
In the literature devoted to geomorphology and glaciology not much has been written about wall-sided glaciers, thanks to which high mountains have their specific landscape character. It is also difficult to find in the literature of the subject a classification of the wallsided glacier forms which would take into account the richness and variety of this phenomenon. After many years of experience in almost all highest mountains of Asia, South America and Europe, the authors decided to fill this gap and therefore to provoke a discussion among the geomorphologists.