Solr Search · GéoProdig, portail d'information géographique

The author shows the history of the Carpathian geological vertical zones during the Late Pleistocene and Early Holocene. The warming of climate, from a continental periglacial climate to a more oceanic one, and the rise in humidity were two engines

The monograph describes the late Quaternary history of Vistula river, based on the extended records gathered during last 20-30 years by the team of more than 20 scientists participating in two national projects, consists of 6 parts. The first part
of several tributaries, which were investigated in detail ; the four - summarises the history of Vistula valley during the Pleistocene. The first conclusions of monograph are presented in part five. More general conclusions are gathered in part six. - (BJ)

with other phenomena outside river valleys: Younger Dryas, 8700-7700, 6600-6000, 5200-4900, 4500-4350, 3300-2850, 2350-1650 BP, V-VIc AD, X-XIc AD and starting from XVIc AD. In last 2-3 millenia the anthropogenic factor starts to play more important role

of uplift cause accelerated incision of valleys and large slope failures, it may be more important than the secular processes acting in various climatic vertical zones. The mountain glaciers during advances separate valley sides into supraglacial

of the meandering toward braiding channels. Again the late XIXth century regulation is reflected in the turn from aggradation to erosion. The separation of the climatic factor from the anthropogenic one needs more extensive research. - (DG)

Résultats de la recherche (5 résultats)