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HYPOTÉZA O METASTABILITE RELIÉFU

In: Geografický časopis, vol. 56, no. 2
Ján Urbánek
Detaily:
Rok, strany: 2004, 125 - 139
Kľúčové slová:
geomorphological catena, basin, gravitational processes, metastability, hypothesis, hierarchic organization
O článku:
The study is concerned with hierarchic organization of geomorphological processes. It describes three levels of organization, the level of gravitational processes, the level of geomorphological catenas and the level of basins. It is presumed that metastability is linked to the basin level, which remains metastable due to a certain organization of processes at the level of geomorphological catenas. The author presumes that the metastability of basins depends on a high rate of differentiation of catenas.
Ako citovať:
ISO 690:
Urbánek, J. 2004. HYPOTÉZA O METASTABILITE RELIÉFU. In Geografický časopis, vol. 56, no.2, pp. 125-139. ISSN 0016-7193.

APA:
Urbánek, J. (2004). HYPOTÉZA O METASTABILITE RELIÉFU. Geografický časopis, 56(2), 125-139. ISSN 0016-7193.