Geomorphologic regionalising of the Romanian territory in the space-chronologic system context

The geomorphologic regionalising of the area attached to our country have evolved in time in relation with the level of knowledge of its relief and substrate. There is regionalising at various levels (from the entire territory to morphosites), a different denomination of the units of relief, but there are also patterns which are considered acceptable. Currently, it is possible to build an improved objective pattern which may consider among others: The relatively recent changes of the research of the geologic substrate through the prism of the tectonics of the active (micro) plaques in the area of our country; The scalar size of the taxonomic organization of the relief; The relative primate of the chronologic/ temporal component; The option for a regionalizing pattern between: the typological model (the similitude of the forms of relief), the morpho-chronologic one (temporal synchronisation), the pattern of the foundation structure (the “tectonic” pattern), the model of the composition of relatively homogenous elementary surfaces (“morphographic” model) etc. Keywords— morpho-chronologic model; extra-Carpathian area; Carpathian area; the taxonomy of the relief