Defining Issues

Author(s):  
Dennis Harding

‘Hillfort’ is a term of convenience. It is widely recognized that the monuments in question are not restricted topographically to hills, and that their role may not have been primarily, and certainly not exclusively, for military defence. Nor are they restricted chronologically to the Iron Age, though during that period they are particularly prominent. The term came into general currency following the publication in 1931 of Christopher Hawkes’ paper, simply entitled ‘Hillforts’, in Antiquity, which also established their predominantly Iron Age date in Britain. Prior to that, Christison (1898) in Scotland had discussed ‘fortifications’, and Hadrian Allcroft (1908) for England had classified ‘earthwork’, both extending their studies into the Medieval period. But ‘hillfort’ for all its limitations has remained in general usage in Britain. Chronologically, this study is concerned with the ‘long Iron Age’; that is, including the post-Roman Iron Age in northern Britain especially, and with later Bronze Age antecedents. Geographically it is concerned with regional groups throughout Britain, but with further reference to Ireland, and in the wider context of relevant sites and developments in continental Europe. The key element of the sites under consideration is enclosure, physically or conceptually demarcating an area to which access is restricted or controlled. This may be achieved by rampart and ditch, stockade or fence, or by the incorporation of topographical and natural features such as cliff-edge or marsh. The scale of enclosing works may range from a relatively modest barrier to massive earthworks that reshape the landscape, and in structural morphology, from single palisade or bank to multiple lines, variously disposed. Topographically they may be located around hilltop contours, on cliffedge, ridge, or promontory, on spurs or hill slopes, in wetlands or spanning river bends, or across variable terrain. In area enclosed they may range from well under a hectare to 20 ha and more, with the territorial or terrain oppida of the late pre-Roman Iron Age attaining 300 ha or more. From size alone, therefore, we may infer a great diversity in the practical, social, and symbolic purposes that they may have served. At the smaller end of the scale, the distinction between hillforts and other enclosed settlements is sometimes a matter of subjective assessment, but otherwise their size and scale suggests that they were community sites, serving a social unit larger than a single family or household.

2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Valero-Garcé

Abstract The varved sediments of Lake Montcortès (central Pyrenees) have provided a continuous and well-dated high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, and the vegetation and the landscape around the lake had already been transformed by humans by this time. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age (ca. 1100 BCE) and the Early Medieval period (820 CE), aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture, hemp retting and other human activities. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing catchment vegetation and landscape changes from the Iron Age onwards. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level (central Pyrenees). The intensification of human pressure in Early Medieval times (580 CE onwards) has also been observed in Lake Montcortès, but the overall anthropization of its watershed had already commenced a couple of millennia before, at the beginning of the Iron Age. It could be interesting to verify whether the same pattern – i.e., Late Bronze “pristinity”, Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line. This pattern complicates the definition of the “Anthropocene”, as it adds a new dimension, i.e., elevational diachronism, to the anthropization of mountain ranges, in general.


AmS-Varia ◽  
2020 ◽  
pp. 77-86
Author(s):  
Marianne Lönn

This article discusses the meaning of stones and the practice of gathering stones, in graves, clearance cairns and stone-covered hillocks. The emphases are on stone-covered hillocks and their long-term usage (up to 1500 years), analyzed using the concept of longue durée. In this paper I propose that the stones in themselves have a cultic meaning as well as the actions, i.e. the remodeling of hillocks and the placing of clearance cairns among graves. In this, I see a connection between stone-covered hillocks, graves and clearance cairns. The underlying concept is a stable, but slowly changing, prehistoric religious tradition that lasted from the Bronze Age to the Migration Period and possibly also through the Late Iron Age. A basic change in this does not take place until the coming of Christianity in the Medieval Period. The reason that Medieval and later clearance cairns were placed together with graves is probably due to their similar appearance.


1999 ◽  
Vol 49 ◽  
pp. 153-158
Author(s):  
Antonio Sagona

The ancient settlement of Sos Höyük, situated east of Erzurum, is providing a significant stratigraphic sequence of human occupation from the Late Chalcolithic to the Medieval period. This sequence includes the transition from the end of the Bronze Age into the first centuries of the Iron Age, a period which is surrounded by difficult but intriguing historical questions. At the mound of Sos Höyük evidence for this transition is starting to emerge from a relatively small operation on the northern slope, midway down the mound, in trenches M15 and L16.The stratigraphic record at Sos Höyük together with a large range of radiocarbon readings taken from samples collected over four seasons of excavation indicate that the site was occupied throughout the late fourth/third millennium BC and intermittently in the second millennium. The earliest centuries of the second millennium BC are best defined by storage pits, wattle and daub dwellings and burials that conform generally to a tradition initially documented by Kuftin in his excavations of the Trialeti kurgan burials near Tbilisi, Georgia (Kuftin 1941; Miron, Orthmann 1995: 79–94).


2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Lorenzo Valero-Garcés

The varved sediments of Lake Montcortès (central Pre-Pyrenees) have provided a continuous high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, when the landscape around the lake had already been transformed by humans. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age and the Early Medieval period, aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture and hemp retting. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing vegetation and landscape changes. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level. It could be interesting to verify whether the same pattern – i.e., Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line.


2021 ◽  
Author(s):  
Valentí Rull ◽  
Teresa Vegas-Vilarrúbia ◽  
Juan Pablo Corella ◽  
Blas Valero-Garcé

Abstract The varved sediments of Lake Montcortès (central Pre-Pyrenees) have provided a continuous high-resolution record of the last ca. 3000 years. Previous chronological and sedimentological studies of this record have furnished detailed paleoenvironmental reconstructions. However, palynological studies are only available for the last millennium, when the landscape around the lake had already been transformed by humans. Therefore, the primeval vegetation of Montcortès and the history of its anthropogenic transformations remains unknown. This paper presents a palynological analysis of the interval between the Late Bronze Age and the Early Medieval period, aimed at recording the preanthropic conditions, the anthropization onset and the further landscape transformations. During the Late Bronze Age (ca. 1100 BCE to 770 BCE), the vegetation did not show any evidence of human impact. The decisive anthropogenic transformation of the Montcortès catchment vegetation and landscape started at the beginning of the Iron Age (770 BCE) and continued during Roman and Medieval times in the form of recurrent burning, grazing, cultivation, silviculture and hemp retting. Some intervals of lower human pressure were recorded, but the original vegetation never returned. The anthropization that took place during the Iron Age did not cause relevant changes in the sediment yield to the lake, but a significant limnological shift occurred, as manifested in the initiation of varve formation, a process that has been continuous until today. Climatic shifts seem to have played a secondary role in influencing vegetation and landscape changes. These results contrast with previous inferences of low anthropogenic impact until the Medieval Period, at a regional level. It could be interesting to verify whether the same pattern – i.e., Iron Age anthropization and Early Medieval intensification of human pressure – may be a recurrent pattern for mid-elevation Pyrenean landscapes below the tree line.


2021 ◽  
Vol 13 (12) ◽  
Author(s):  
Knut Kaiser ◽  
Johann Friedrich Tolksdorf ◽  
Anna Maartje de Boer ◽  
Christoph Herbig ◽  
Falk Hieke ◽  
...  

AbstractColluvial sediments originating from soil erosion on slopes have proven to constitute significant evidence for tracing past human impact on mountain landscapes. In the Central European Erzgebirge (Ore) Mountains, colluvial sediments are associated with specific landforms (footslopes, slope flattenings, dells) and cover a share of 11% (11,905 ha) of the regional soil landscape. Thirteen pedosedimentary sections with colluvial layers were investigated at five forested sites (520–730 m a.s.l.) within a context of mining archaeology, integrating data from pedology, archaeology, palaeobotany, and geochronology. The thickness of the gravel-bearing loamy, silty, and sandy colluvial layers is up to 70 cm, which are mostly located on top of the sections. The geochronological ages and archaeological data reveal a high to late medieval to post-medieval age of the colluvial sediments. Pollen data show a drastic decline of the mountain forests in the late twelfth to fifteenth centuries AD accompanied by an increase of pioneer trees and spruce at the expense of fir and beech. The primary cause of soil erosion and subsequent colluvial deposition at the sites investigated is medieval to post-medieval mining and other early industrial activities. A compilation of 395 radiocarbon and OSL ages, obtained from colluvial sediments at 197 upland sites in Central Europe, shows that anthropogenically initiated colluvial dynamics go as far back as the late Bronze Age to the early Iron Age. Most ages derive from the medieval to post-medieval period, corresponding to the general intensification of settlement and land-use activities including deforestation and widespread ore mining.


2012 ◽  
Vol 78 ◽  
pp. 173-206 ◽  
Author(s):  
Susan Ripper ◽  
Matthew Beamish ◽  
A. Bayliss ◽  
C. Bronk Ramsey ◽  
A. Brown ◽  
...  

The recording and analysis of a burnt mound and adjacent palaeochannel deposits on the floodplain of the River Soar in Leicestershire revealed that the burnt mound was in use, possibly for a number of different purposes, at the transition from the Neolithic to the Bronze Age. An extensive radiocarbon dating programme indicated that the site was revisited. Human remains from the palaeochannel comprised the remains of three individuals, two of whom pre-dated the burnt mound by several centuries while the partial remains of a third, dating from the Late Bronze Age, provided evidence that this individual had met a violent death. These finds, along with animal bones dating to the Iron Age, and the remains of a bridge from the early medieval period, suggest that people were drawn to this location over a long period of time.


Viking ◽  
2021 ◽  
Vol 85 (1) ◽  
Author(s):  
Søren Diinhoff

In the summer months of 2013, the University Museum of Bergen conducted an archeological excavation of a large prehistoric settlement area at Etnesjøen in Etne parish, Western Norway. By use of mechanized top soil stripping numerous buildings, inhumation burials, cooking pits and kilns were uncovered. The site dates from the Late Bronze Age to Early Medieval Period. The focus of the article is the discovery of a Pre-Roman Iron Age village, formed of up to six farms chronologically spanning up to five generations of continuous occupation. At the time of the excavation, this was only the second pre-historic village of its kind found in Norway, indicating a significant and important discovery. 


2006 ◽  
Vol 72 ◽  
pp. 341-365 ◽  
Author(s):  
Andy M. Jones

Three seasons of archaeological fieldwork were carried out in 1998–2000 by Cornwall Archaeological Un within the Imerys Stannon China Clay Works, Bodmin Moor. The first two seasons involved the excavation of an Early Bronze Age cairn group and Middle Bronze Age and Middle Iron Age settlement activity. The third season on the Northern Downs involved the evaluation a number of cairns, field systems, and palaeoenvironmental sites.The cairn group consisted of three earlier Bronze Age ring-cairns and two ‘tailed’ cairns. One ring-cairn continued to be used as a ceremonial monument in the Middle Bronze Age and was reused during the Iron Age as a dwelling. An artefact assemblage including Bronze and Iron Age pottery and stonework was recovered. Two prehistoric beads one of faience, the other of amber, were also found.Ten Bronze Age radiocarbon determinations spanning 2490–1120 cal BC and two Iron Age determinations (370–40 cal BC) were obtained from three of the cairns. Two pollen columns on the Northern Downs were also dated. Significantly, a series of eight determinations was obtained from a single column, which provided environmental information from the Mesolithic through to the early medieval period. The radiocarbon dating showed that impact on the vegetation of the Down commenced during the Neolithic, with larger-scale clearance during the Bronze Age. Widespread open grassland was established by the Middle Bronze Age.It is suggested here that use of space within the cairn group was structured and that the cairns formed a monument complex which was part of a wider landscape cosmology, involving groupings of particular monument types and the referencing of rocky outcrops and tors.The investigations on Stannon Down were important as an opportunity to study an Early Bronze Age ceremonial landscape and reconsider how later Middle Bronze Age and Iron Age peoples on Bodmin Moor might have engaged with and interpreted the materiality of earlier prehistoric monuments.


1983 ◽  
Vol 10 (1) ◽  
pp. 41-71 ◽  
Author(s):  
G J Barclay

SUMMARY Myrehead has revealed the eroded remnants of activity from the Beaker period (Period A) onwards, with actual settlement evinced only from about the early first millennium be. The three houses and the cooking pits of Period B may have been constructed and used sequentially. This open settlement was probably replaced during the mid first millennium bc, possibly without a break, by a palisaded enclosure (Period C), which may have contained a ring-groove house and a four-post structure. Continued domestic activity (Period D) was suggested by a single pit outside the enclosure, dated to the late first millennium bc/early first millennium ad. The limited evidence of the economy of the settlements suggests a mixed farming system.


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