The developmental stages of an accumulative cone of dry valley as an indication of change in natural environment conditions (Western Pomerania)

dc.contributor.authorPaluszkiewicz, Renata
dc.date.accessioned2016-11-22T12:59:34Z
dc.date.available2016-11-22T12:59:34Z
dc.date.issued2013
dc.description.abstractThe aim of this paper is to present the stages of development of an alluvial cone as an indication of change in natural environment conditions. a detailed research was conducted within the upland regions of Drawsko Lakeland. At the valley mouth of one of the erosional-denudational valleys an alluvial cone in question splays out. The imparity between the capacity of the erosional-denudational valley and the capacity of the alluvial cone indicates that the main stage of erosion had taken place before the cone’s deposition. During the beginning stage the material acquired from the dissection was most likely delivered directly to the channel of Dębnica river and was incorporated in the fluvial transport. The cone was formed during the later stage. The results of the radiocarbon analyses reveal that the formation of the alluvial cone and the valley associated with the cone took place during the Subatlantic. It was also estimated that the cone aggraded with the rate of approximately 3,9 mm per year.pl_PL
dc.identifier.citationQuaestiones Geographicae vol. 32 (1), 2013, pp. 16-20pl_PL
dc.identifier.issn0137-477X
dc.identifier.urihttp://hdl.handle.net/10593/15673
dc.language.isoengpl_PL
dc.publisherWydział Nauk Geograficznych i Geologicznych Uniwersytetu im. Adama Mickiewiczapl_PL
dc.rightsinfo:eu-repo/semantics/openAccesspl_PL
dc.subjecterosional-denudation valleypl_PL
dc.subjectalluvial conepl_PL
dc.subjectDrawsko Lakelandpl_PL
dc.subjectWest Pomeraniapl_PL
dc.titleThe developmental stages of an accumulative cone of dry valley as an indication of change in natural environment conditions (Western Pomerania)pl_PL
dc.typeArtykułpl_PL

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