Exploring landscape setting: First results of geomorphological and sedimentological investigations of the mammoth bone site Dolní Věstonice I (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68081758%3A_____%2F24%3A00601950" target="_blank" >RIV/68081758:_____/24:00601950 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Exploring landscape setting: First results of geomorphological and sedimentological investigations of the mammoth bone site Dolní Věstonice I (Czech Republic)

Popis výsledku v původním jazyce

The contribution presents a geoscientific research of the large accumulation of mammoth bones at the Gravettian site of Dolní Věstonice I, concentrated both on the site's geomorphological setting and the sedimentary record. Preliminary results show that several larger mass movements differentiate the slope and that the mammoth bone accumulation is located in a depression, postoccupationally impacted by short-distance slope transport, weathering and pedogenesis before being buried by loess sedimentation. The resulting loess sequence illustrates periods of landscape instability (indicated by undulations, cryoturbation and displacements) as well as landscape stability (indicated by weak soil horizons and ice-wedge pseudomorphs).

Název v anglickém jazyce

Exploring landscape setting: First results of geomorphological and sedimentological investigations of the mammoth bone site Dolní Věstonice I (Czech Republic)

Popis výsledku anglicky

The contribution presents a geoscientific research of the large accumulation of mammoth bones at the Gravettian site of Dolní Věstonice I, concentrated both on the site's geomorphological setting and the sedimentary record. Preliminary results show that several larger mass movements differentiate the slope and that the mammoth bone accumulation is located in a depression, postoccupationally impacted by short-distance slope transport, weathering and pedogenesis before being buried by loess sedimentation. The resulting loess sequence illustrates periods of landscape instability (indicated by undulations, cryoturbation and displacements) as well as landscape stability (indicated by weak soil horizons and ice-wedge pseudomorphs).

Druh

O - Ostatní výsledky

CEP obor

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OECD FORD obor

60102 - Archaeology

Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2024

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů