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Niełatwa archeologia klifów – przypadek stanowisk w Bagiczu

100%
Chmiel-Chrzanowska M.
Folia Praehistorica Posnaniensia
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2018
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vol. 23
9-22
EN
The following paper presents the problem of archaeological sites located on cliffs on the Southern Baltic Sea shore. This article discusses issues related to a necessity of solving the problem of this kind of research, related to methodological, as well as documentation and preservation standards based on preliminary results of the project conducted in Bagicz area (Ustronie Morskie commune). In this region four new structures were noted on a cliff surface. The key to understand the situation of archaeological sites located on a cliff areas is the knowledge of the processes related to their formation and activity. All of them have a huge impact for the state of preservation of the cliff, however they have various intensity level depending on the part of the Baltic Coast.
2
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Biodiversity and Temporal Diversity in Archaeological Landscapes: Towards a New Perception

92%
Matteini T.
Loci Communes. International Journal of Studies on Spaces in Arts and Humanities, Anthropology and Architecture
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2021
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vol. 1
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issue 1
1-12
EN
Reflecting on several crucial issues regarding the protection, planning, and management of archaeological landscapes from the point of view of the Discipline of Landscape Architecture, the article focusses on the roles of the vegetal component and plant biodiversity in the landscaping of archaeological sites.After outlining a background framework of the theoretical, cultural, and ecological relationships between vegetation and ruins adopting a landscape architecture approach, the article proposes a set of conceptual and operational tools to deal with active and inventive1 conservation of archaeological landscapes, striving to adopt the “strong forward-looking” attitude recommended by the European Landscape Convention (Florence 2000).By re-reading the consolidated concept of biodiversity (CBD, 1992) according to a different research dimension, the concept of temporal diversity is explored and proposed as a key issue in the interpretation and planning of layered landscapes. Focusing in particular on design issues in the management of ruin and vegetation integration, an innovative approach is presented in regards to various greenery-related potentialities in the landscaping and management of archaeological sites.The article’s concluding remarks aim to open new trans-disciplinary windows of research on active and inventive conservation of archaeological landscapes to foster further exploration of this potentially broad ambit of investigation.
3
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New evidence for the Late Iron Age in the Posočje region, Slovenia

70%
Laharnar B.
Studia Hercynia
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2023
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vol. 27
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issue 2
77-97
EN
Several archaeological sites from the Late Iron Age have recently been discovered in Posočje, a region along the upper and middle reaches of the River Soča/Isonzo (NW Slovenija, NE fringes of Italy), which compel us to re -examine the Latenisation of the region. Supra -regional La Tène forms began to appear in the material culture at the end of the Early Iron Age, in the late 4th and early 3rd centuries BC. This was followed by a marked decrease in habitation remains, a ‘hundred -year crisis’ with very little archaeological evidence available for the time between the initial decades of the 3rd and the mid-2nd century BC. The picture then changed again with the rise of the Late Iron Age Idrija group, as most of the sites connected with this group date between 150/130 BC and the Augustan period. This is also the period of the first ancient literary sources mentioning the wider area, which inspire ever newer attempts at ethnic identifications of the population living there. The sources reveal that the Romans appear to have associated the area with the Carni.
4
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Litologia, geneza i wiek osadów w Kalnikowie i Chotyńcu na Płaskowyżu Tarnogrodzkim (Kotlina Sandomierska)

58%
Gębica P., Superson S., Trybała-Zawiślak, K., Woronko B.
Acta Geographica Lodziensia
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2017
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vol. 106
65-86
PL
Artykuł omawia wyniki analiz uziarnienia, obróbki ziarn kwarcu i datowań metodą OSL zróżnicowanych pod względem pochodzenia i wieku osadów czwartorzędowych (osady eoliczne, rzeczne, fluwioglacjalne) występujących na stanowiskach archeologicznych w południowej części Płaskowyżu Tarnogrodzkiego. Osady wydmowe w Kalnikowie-Zagrebli miąższości 1,2 m charakteryzują się dominacją ziarn drobnoziarnistych o średniej średnicy Mz=2,9 phi. Tak drobnoziarniste osady są rzadko spotykane w wydmach z późnego glacjału w Kotlinie Sandomierskiej. Depozycja piasków wydmowych na podstawie datowań OSL miała miejsce w młodszym dryasie. Osady budujące podłoże wydmy, to piaski drobnoziarniste z poziomami bruków żwirowych pochodzenia fluwioglacjalnego, które jak wykazała obróbka ziarn kwarcu, znajdują się na wtórnym złożu. Terasę nadzalewową Wiszni o wysokości 6–8 m n.p.rz. budują warstwowane horyzontalnie drobnoziarniste utwory piaszczyste, które na powierzchni terasy tworzą wał przykorytowy. Cechy strukturalne osadów oraz rozkład parametrów uziarnienia wskazują, że akumulowane były w strefie przykorytowej równi zalewowej. Analiza osadów pylastopiaszczystych pokrywających wierzchowinę płaskowyżu w otoczeniu wału grodziska z okresu celtyckiego w Chotyńcu wykazała, że nie są to utwory pochodzenia wietrzeniowego, ale prawdopodobnie osady genezy eolicznej.
EN
The article presents the results of grain size, quartz grain roundness analysis and OSL datings, differing in origin and age of the Quaternary deposits (aeolian, fluvial, fluvioglacial) occurring in the archaeological sites in the southern part of the Tarnogród Plateau. The dune sediments in the Kalników-Zagrebla site of a thickness of 1.2 m are characterized by the domination of fine grains with the mean diameter Mz=2.9 phi. Such fine sediments are unusual in the Late Glacial dunes in the Sandomierz Basin. The deposition of the dune was dated by the OSL to the Younger Dryas. The dunes are underlain by fine sands with thin gravel horizons of fluvioglacial origin, which represent the redeposited sediments according to quartz grain roundness analysis. The terrace of the Wisznia River 6–8 m above the river channel is built of horizontally bedded fine sands, which form the natural levees on the terrace surface. Structural features and the distribution of grain size parametres indicate, that sands were accumulated in the proximal part of the floodplain. An analysis of the silty-sandy sediments covering the plateau around the hill-fort rampart from the Celtic Period in Chotyniec site, excluded their weathering origin and proved their aeolian genesis.
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