(Article of periodic en Russe - 1998)

Document title

Èvolûciâ rel'efoobrazuûŝih processov Zapadnogo Priohot'â v kajnozoe (Russe)
L'évolution des processus morphogéniques dans l'ouest de la région d'Okhotsk au Cénozoïqie

Authors(s) and Affiliation(s)



During Late Cenozoic the lead geomorphologic processes in the western Priokotie changed together with relief and climate evolution. Plains with areas of hummocky topography have been transformed into deeply dissected low and middle mountains. Climate has changed from humid subtropical (Oligocene) into frigid (subarctic) with tundra development (Late Pleistocene). All these conditions have formed recent surface pattern. Many processes are now very slow, but they changed many times in Late Cenozoic. Each time interval was characterised by specific set of lead geomorphologic processes and of extreme, catastrophic, ones, which were locally distributed. Analysis of relief evolution allows to date the formation of the ground features'main types


Article of periodic

published at : Geomorfologiâ / ISSN 0435-4281

Editor : Nauka, Moskva - RUSSIE, FEDERATION DE (1970)

Millesime : 1998, no2 [pp. 81-90]

Bibliographic references : 20 ref.

Collation : Illustration ;




Laboratoire INTERGEO - Paris

INIST-CNRS, Cote INIST : 14585

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2001.
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