Sedimentological and geochemical research carried out in North- West Mazovia, central Poland, allowed the determination of landscape transformation in relation to the history of human settlement. The types of sediments subject to analysis included palaeochannel filling, accumulation on the river floodplain and colluvial deposits. The absolute ages of sediments and their sedimentological features allow the conclusion that the first response to human activity in the area is recorded in the overbank deposits in the Skrwa River valley as a result of the Wielbarska Culture in 200-300 AD. Subsequently, fan accumulation at the mouths of gullies started around the 12th-13th centuries AD. Frequent changes of sediment properties have been observed si...
Settlement archaeology is often supported by geoarchaeology in which human habitation is...
The research carried out in the Utrata valley focused on geochemical (such as heavy metals content) ...
While on the continental or global level and across the long time-scales, erosion and accumulation p...
Fluvial and slope deposits were investigated in the NW part of Masovia region. Their deposition was ...
ABSTRACT. The area of Chroberz (southern Poland) poses questions of an interdisciplinary character c...
In the study the authors analysed the diversity of the textural indices and selected geo-chemical fe...
During the last few decades, many case studies have focused on landscape transformations in response...
Based on palaeobotanical analyses of organic deposits, as well as geomorphological and geological st...
Textural and structural diversity of slope covers and alluvial deposits in the upper parts of mid-mo...
Paleogeography of the lower Przemsza River valley was studied in detail. By means of sedimentologica...
We present results from a palaeoecological analysis conducted on deposits accumulated in an oxbow la...
This paper presents the results of multidisciplinary research on Neo-Holocene slope deposits cover u...
the place where the Wisłok flows into the San, went through a 6-meter-thick series of de-posits of t...
Anthropogenic alterations of the recent millennia of our era, in the loess areas of the Lublin Uplan...
The present paper discusses the influence of geochemical properties on biogenic deposits in the Wilk...
Settlement archaeology is often supported by geoarchaeology in which human habitation is...
The research carried out in the Utrata valley focused on geochemical (such as heavy metals content) ...
While on the continental or global level and across the long time-scales, erosion and accumulation p...
Fluvial and slope deposits were investigated in the NW part of Masovia region. Their deposition was ...
ABSTRACT. The area of Chroberz (southern Poland) poses questions of an interdisciplinary character c...
In the study the authors analysed the diversity of the textural indices and selected geo-chemical fe...
During the last few decades, many case studies have focused on landscape transformations in response...
Based on palaeobotanical analyses of organic deposits, as well as geomorphological and geological st...
Textural and structural diversity of slope covers and alluvial deposits in the upper parts of mid-mo...
Paleogeography of the lower Przemsza River valley was studied in detail. By means of sedimentologica...
We present results from a palaeoecological analysis conducted on deposits accumulated in an oxbow la...
This paper presents the results of multidisciplinary research on Neo-Holocene slope deposits cover u...
the place where the Wisłok flows into the San, went through a 6-meter-thick series of de-posits of t...
Anthropogenic alterations of the recent millennia of our era, in the loess areas of the Lublin Uplan...
The present paper discusses the influence of geochemical properties on biogenic deposits in the Wilk...
Settlement archaeology is often supported by geoarchaeology in which human habitation is...
The research carried out in the Utrata valley focused on geochemical (such as heavy metals content) ...
While on the continental or global level and across the long time-scales, erosion and accumulation p...