Chapter Four. An Arena For Higher Powers. Cult Buildings And Rulers In The Late Iron Age And The Early Medieval Period In The Mälar Region

2021 ◽  
Vol 26 (1) ◽  
pp. 137-162
Author(s):  
Fredrik Fahlander

This text discusses reuse and modifications of older graves in southern Sweden during the Late Iron Age and early medieval period (c. 9th to 12th centu- ries AD). Post-burial practices in the Late Iron Age have in general been interpreted as means to nego- tiate status, identity and rights to land, while in the later part of the period they are comprehended as expressions of religious insecurity and syncretism. In this text, the continuity of post-burial practices during the whole period is stressed and instead of general top-down interpretative models, the onto- logical status and material aspects of death, dead bodies and their graves is emphasized. It is argued that the post-burial actions generally constituted ways of relating to a specific type of materiality, the bones of the ancient dead, which transgress binary categorizations such as living–dead, past–present, heathen–Christian, and human–nonhuman. The argument builds on five recently excavated sites in southern Sweden: Bogla, Broby Bro, Lilla Ullevi, Valsta and Vittene.


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.


Author(s):  
Rebecca C. Redfern

The feeding and rearing of infants are sociocultural and developmental processes, each with their own timetables that can either unite or diverge, depending on the wellbeing and physiological growth of the infant, and the needs of the mother or carer and the society in which they live. They are highly emotive and complex topics, which go to the heart of human relationships and behaviours, because they are regarded as important steps to achieving personhood and a social identity. Furthermore, because these processes begin during pregnancy, they rely on the intimate connections between a mother and foetus, and carer and baby. This chapter will examine these processes from pregnancy through to childhood, providing a framework to understand the practices and choices made by the Iron Age, Roman and Saxon communities in Britain and Europe.


Author(s):  
Alastair MacLaren ◽  
Ewan Campbell ◽  
Gordon Cook ◽  
Janet Hooper ◽  
L Wells ◽  
...  

Two rescue excavations at the northern edge of a rather sparsely occupied part of the interior of Caithness are reported here, lying near to one of the largest clusters of archaeological sites in the modern county. In the event, the monuments were not threatened, and survive.Because of the limited nature of the excavation at Loch Shurrery (NGR ND 043568),the main value of the evidence about the hut circle relates to its structure and dating. The excavated remains represented a medium-sized oval house with a west-facing entrance. It had an off-centre hearth of rectangular construction. It was rather different in structure to the majority of the small group of such sites which have been excavated in the northern part of the Scottish mainland, as it did not appear to have an internal ring of post holes. In addition, its western entrance is not matched at the other sites, where entrance orientations are to the south, east or south-east. The wall of the Loch Shurrery house was fairly thick and the excavation suggested that it was complex, while the entrance passageway was quite long. The existence of door checks is also an unusual feature and may relate to the entrance structures of brochs and other substantial roundhouses. Two samples of charcoal from the hearth inside the hut circle were submitted for radiocarbon dating: the determinations produce calibrated ranges (at 2-sigma) of 346-4 cal BC and 341 cal BC-1 cal AD. It is likely that most of the excavated, undecorated pottery is also Iron Age, part of a broad tradition of very coarsely tempered pottery. Not-withstanding evidence of extended occupation, the whole period of construction and occupation may have occurred within the Iron Age.The mound of Lambsdale Leans (NGR ND 051548)lies in Reay parish, situated on low-lying ground at the head of Loch Shurrery and close to where its main tributary (the Torran Water) enters the loch from the south. The main characteristics of the this partially-excavated site are the presence of what appeared to be two extended inhumations and the remnants of possible structures associated with several layers of burnt material. Lambsdale Leans itself was a natural mound, of elongated shape and composed largely of sand, into which were set the burials and structural remains. The burials (one certainly female, the other probably so) were not in cists. The structural remains, while not fully excavated, accord well with the general tenor of the available evidence of later first millennium AD buildings in the north of Scotland. Both structures at Lambsdale Leans had floors comprising roughly laid paving, edged with upright slabs, and with an outer kerb of stones. The earliest-dated pottery sherds, unstratified, are from a single grass- tempered handmade vessel whose form cannot be determined. Overall,on one interpretation the Lambsdale Leans evidence favours a context within the Early Medieval period in Caithness. The pottery however, being mostly C12-C13 oxidised wheel-thrown vessels, can be seen to support the suggestion that occupation on the site may have begun in the Medieval period.


2021 ◽  
Vol 3 ◽  
pp. 129
Author(s):  
Nicky Garland ◽  
Barney Harris ◽  
Tom Moore ◽  
Andrew Reynolds

Linear earthworks of a monumental character are an enigmatic part of the British landscape. Research in Britain suggests that such features range in date from the early 1st millennium BC to the Early Middle Ages. While the  roles of these monuments in past societies cannot be understated, they remain a relatively under-researched phenomenon. This article introduces the Leverhulme Trust-funded ‘Monumentality and Landscape: Linear Earthworks in Britain’ project, which aims to provide a comparative study of linear earthworks focusing on those dating to the Iron Age and early medieval period. This contribution reviews our approach and shares preliminary results from the project’s first year, identifying wider implications for the study of linear earthworks.


2021 ◽  
Vol 150 ◽  
pp. 247-278
Author(s):  
Ronan Toolis

Underlying much research on Iron Age Scotland is a pervasive regionalism. This has led to the underplaying of cultural traits that are evident across the country. The examination of south-west Scotland, a region that does not have a distinctive later prehistoric character and which is often viewed as somewhat peripheral to understanding Iron Age Scotland, however, reveals underlying patterns of settlement and culture that are embedded across Scotland but markedly different to Iron Age societies to the south. Moreover, cultural traits apparent across Scotland but absent south of the border continued into the early medieval period, suggesting significant cultural divergences between 400 BC and AD 650.


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.


2020 ◽  
Vol 12 (14) ◽  
pp. 5794
Author(s):  
Edward Pollard ◽  
Anthony Corns ◽  
Sandra Henry ◽  
Robert Shaw

Promontory forts are an understudied but distinctive maritime archaeological feature from the Iron Age to the early medieval period from northern Spain to Scotland. Their coastal location renders them susceptible to erosion and loss to history, a situation exacerbated by increased storm frequency and sea level rise. Reconstruction of their original form is important to determine their role in the society of the time. This paper concentrates on a particularly notable group of promontory forts along the Copper Coast of Co. Waterford, where traces of up to 32 remain today within a 24 km stretch of coastline. The methodology has involved using oral tradition, historical records and field survey. This has been enhanced by aerial survey using drones and light aircraft. This paper models the data to estimate areas eroded and show how forts were once significantly larger and dominated coastal resources with an economy of farming, fishing, mining and trading. This paper calculates a likely erosion rate of 4–5 cm/yr and anticipates the last remains to be lost in 350 years, perhaps sooner with climate change.


2011 ◽  
Vol 14 (1-2) ◽  
pp. 190-209 ◽  
Author(s):  
Pamela J. Cross

Burial of horses and horse-elements occurred throughout Europe during the first millennium AD. These burials are prevalent in northwest Europe and are perhaps more significant in Britain than previously realised. This article explores the position and value of the horse within Britain during this period and why the burials are likely to represent ritual deposition. Both horse and human-horse burials, are linked to non-Christian burial and sacrificial practices of the Iron Age and Early Medieval period and are particularly associated with Anglo- Saxon and Viking Britain. Some of the traditions appear to reflect the culture described in the Icelandic Sagas, Beowulf, and other legends and chronicles. Archaeologically, the human-horse burials are also linked with high status individuals and ‘warrior graves’, while complete-horse and horse-element burials may represent ritual feasting and/or sacrificial rites which are probably linked with fertility, luck, and the ancestors.


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