A periglaciális környezet felszínalakulása 1. rész

The intensive research of the periglacial features in Hungary took place in the 1960’s, but the main problem was that only fossil phenomena could be studied in Hungary. At that time the periglacial phenomena were classified on a purely descriptive basis, according to formal similarities. The following is not a description of the entire field of knowledge, but only a selection of some important and neglected or misunderstood phenomena and forms.