Le Yaudet, Ploulec'h, Côtes d'Armor, Brittany. An Interim Report on the Excavations of 1991–4

1995 ◽  
Vol 75 ◽  
pp. 43-70 ◽  
Author(s):  
Barry Cunliffe ◽  
Patrick Galliou
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Eleventh Century ◽  
Third Century ◽  
North Coast ◽  
Agricultural Activity ◽  
Early Medieval Period ◽  
The North ◽  
Late Iron Age ◽  
Two Phases

The promontory site of Le Yaudet, on the north coast of Brittany, was occupied from the Bronze Age to the present day, at various stages during this period sharing in maritime exchange systems linking Brittany to Britain. In the Late Iron Age the site, of some 6ha, was surrounded by stone and rubble defences the main cross-promontory defence being of murus gallicus type. The defences are of at least two phases, the later probably dating to the time of Caesar. Occupation continued and in the late third century AD a new wall was built around the defensive circuit at a time when similar coastal sites on both sides of the Channel were being defended. On one site, agricultural activity of the early medieval period was followed by village development in the eleventh century. The present village is a shrunken remnant of the earlier, more extensive settlement.

scholarly journals Isolated and backward Westerwolde (Groningen, the Netherlands)? A confrontation of archaeological and historical data from the Middle Ages in a wider geographical context

2021 ◽  
pp. 273-344
Author(s):  
Henny A. Groenendijk ◽  
Remi Van Schaïk
Keyword(s):  
The Netherlands ◽  
Bronze Age ◽  
19Th Century ◽  
Middle Ages ◽  
Iron Age ◽  
Critical Study ◽  
Ecological Data ◽  
The North ◽  
Late Iron Age ◽  
The 19Th Century

The aim of this paper is to question the supposed isolated and backward position of the region of Westerwolde, in the north-eastern part of the Netherlands. Westerwolde’s geographically rather isolated position has traditionally been brought forward to explain its backward image. Progressive peat growth ever since the Bronze Age occupation had transformed Westerwolde into an island. It was abandoned in the Late Iron Age, only to be recolonized in the early Middle Ages. During the 19th century, romantics were still admiring Westerwolde’s arcadian scenery and cultural traditions. In contrast, from the mid-19th century until well into the 20th century, protagonists of modern agriculture criticized its backward farming methods and standard of living, as well as its poor infrastructure. The central issues we address here is whether critics were justified in describing it as backward in the 19th century and whether concrete indications for this assumed backwardness are to be found in previous centuries. To jump from early medieval times to the 19th century is too big a leap, but combining archaeological and ecological data with a renewed and more critical study of written sources against the background of huge landscape transformations has brought a nuanced understanding of how Westerwolde evolved. We present new insights for the period starting with the conquest of Frisia and Saxony by the Carolingians and the introduction of Christianity, when missionaries and newly founded monasteries acquired agricultural assets and rights in the conquered region, up to the late Middle Ages. We therefore analyze church foundations, livelihoods or economic conditions of existence in connection with occupation structures, infrastructure and exchange of consumer goods interdisciplinarily. Conservatism appears easily confused with backwardness, and an aversion to innovation, with indifference, as underlying external factors often forced the inhabitants to adopt a wait-and-see attitude. Westerwolde is viewed continuously in connection with the adjacent regions of Drenthe and Lower Saxon Emsland.

A Preliminary Investigation of Two Prehistoric Cave Sites in Southern Albania

2009 ◽  
Vol 104 ◽  
pp. 9-26 ◽  
Author(s):  
K.D. Francis ◽  
D.J. Bescoby ◽  
I. Gjipali
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Preliminary Investigation ◽  
Radiocarbon Dates ◽  
Lithic Assemblage ◽  
The North ◽  
Late Iron Age ◽  
Middle Bronze Age ◽  
Trading Networks ◽  
The Town

In this article we describe the evaluation of two prehistoric sites situated within the coastal zone of south-western Albania, originally investigated by the Italian prehistorian Luigi Cardini in 1939. The first is a cave site in the town of Himara; the second a rock-shelter at Kanalit in the Acroceraunian Mountains to the north. Investigations at both locations revealed stratified evidence of prehistoric activity dating from the mid-Holocene. At Kanalit, an extensive lithic assemblage provided evidence for the exploitation of the adjoining coastal lowlands during the Mesolithic, while at Himara, a largely unbroken sequence of deposits records often intensive human activity at the cave from the Early Bronze Age. Radiocarbon dates have provided a significant independent chronological marker for Early/Middle Bronze Age horizons. The ceramic evidence indicates a predominance of local influences, the site not becoming part of wider trading networks until the late Iron Age, c. seventh to sixth centuries BC.Σε αυτό το άρθρο πραγματευόμαστε τη σημασία δύο προϊστορικών θέσεων, οι οποίες βρίσκονται στην παράκτια ζώνη της ΝΔ Αλβανίας. Οι θέσεις αυτές είχαν αρχικά ερευνητεί από τον Ιταλό προϊστορικό αρχαιολόγο Luigi Cardini το 1939. Η πρώτη θέση αφορά ένα σπήλαιο στην πόλη της Χειμάρρας και η δεύτερη μία βραχοσκεπή, στη θέση Kanalit, στα Ακροκεραύνια όρη προς βορρά. Έρευνες στις δύο θέσενς αποκάλυψαν στρωματογραφημένες ενδείξεις προϊστορικής δραστηριότητας, που χρονολογούνται από το μέσο Ολόκαινο. Στη θέση Kanalit ένα ευρύ σύνολο λίθινων αντικειμένων παρέχει στοιχεία για την εκμετάλλευση των γειτονικών παράκτιων πεδινών περιοχών κατά τη Μεσολιτική περίοδο. Στο σπήλαιο της Χειμάρρας μία σειρά από αδιάσπαστες, στο μεγαλύτερο μέρος τους, αποθέσεις μαρτυρεί συχνά έντονη ανθρώπινη δραστηριότητα από την Πρώιμη Εποχή του Χαλκού. Οι ραδιοχρονολογήσεις παρέχουν ένα σημαντικό ανεξάρτητο χρονολογικό δείκτη για τους ορίζοντες της Πρώιμης/Μέσης Εποχής του Χαλκού. Η κεραμική φανερώνει την επικράτηση τοπικών επιρροών, με τη θέση αυτή να μην λαμβάνεν μέρος στα ευρύτερα εμπορικά δίκτυα πριν από την όψιμη Εποχή του Σιδήρου, περίπου τον 70 – 60 αιώνα π.Χ.

Excavation of a prehistoric enclosure at Mar Hall, Bishopton, Renfrewshire

2012 ◽  
Vol 34-35 (1) ◽  
pp. 117-135 ◽  
Author(s):  
Graeme Cavers ◽  
Victoria Clements ◽  
Sarah Lynchehaun
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Early Iron Age ◽  
Late Bronze Age ◽  
Archaeological Excavation ◽  
Late Iron Age ◽  
Two Phases

Remains of a multi-palisaded and ditched enclosure were identified during an archaeological watching brief and evaluation carried out in July 2007. In accordance with planning conditions an archaeological excavation was subsequently undertaken between August and December 2007, on behalf of Mar Estates Ltd. The excavation identified two phases of construction at the enclosure, the multiple palisades and entrance dating to the Late Bronze Age/Early Iron Age and a large ditch dating to the Middle-Late Iron Age. A Bronze Age burnt mound was found nearby.

The Carpathian and Danubian area

2018 ◽  
Author(s):  
Aurel Rustoiu
Keyword(s):  
Bronze Age ◽  
Black Sea ◽  
Iron Age ◽  
Carpathian Basin ◽  
The Black Sea ◽  
The North ◽  
Late Iron Age ◽  
First Millennium ◽  
Danube Region ◽  
Greek World

This chapter provides an overview of Iron Age societies in the eastern Carpathian basin and lower Danube region, from the Great Hungarian Plain to the Black Sea, drawing on funerary and settlement data from the different regions. The first iron objects occur in Transylvania in the late Bronze Age, but ironworking only developed fully in the early first millennium BC. Throughout the period, the area was open to contacts with central Europe, as well as the Mediterranean and Black Sea regions. The so-called Scythian and Celtic horizons in the Carpathian basin were both associated with newcomers, although the nature and extent of population movement remains open to discussion. In the north Balkans, a series of opulent graves and fortified settlements attests to the development of an aristocracy with strong ties to the Greek world, followed in the late Iron Age by the rise of the impressive but short-lived Dacian kingdom.

scholarly journals A multi-proxy Holocene palaeoenvironmental record of climate change and prehistoric human activity from Lough Cullin, southeast Ireland

The Holocene ◽  
2022 ◽  
pp. 095968362110665
Author(s):  
Kevin Kearney ◽  
Benjamin Gearey ◽  
Susan Hegarty ◽  
Suzi Richer ◽  
Carla Ferreira ◽  
...  
Keyword(s):  
Bronze Age ◽  
Human Activity ◽  
Iron Age ◽  
Vegetation Change ◽  
Late Neolithic ◽  
Early Medieval Period ◽  
Late Iron Age ◽  
Subsequent Step ◽  
Woodland Regeneration ◽  
Radiocarbon Chronology

A multiproxy (pollen, microcharcoal, loss-on-ignition, magnetic susceptibility and geochemistry) sequence from Lough Cullin, southeast Ireland, supported by a high-resolution radiocarbon chronology, modelled using Bayesian approaches, provides a record of environmental change for much of the Holocene. Following the establishment of mixed deciduous woodland, climatic deterioration was likely responsible for pronounced vegetation change and erosion, 7615–6500 cal. BC to 6245–5575 cal. BC, evidence for the ‘8.2 Kyr’ BP climate event. The so-called ‘elm decline’ is dated to 4220–3980 cal. BC and whilst there are possible indications of an anthropogenic cause, clear evidence of woodland clearance with cereal pollen is recorded at 3900–3700 cal. BC, 3790–3580 cal. BC and 3760–3650 cal. BC, during a period of clearance and farming of 320–450 years duration. A reduction in farming/settlement and woodland regeneration during the Middle Neolithic parallels the archaeological record, with low levels of activity during the Late Neolithic/Chalcolithic after 2960–2525 cal. BC, prior to increases during the Bronze Age then woodland clearance and agriculture between 1500–1410 and 1275–1000 cal. BC, corresponding with the archaeological evidence. A subsequent ‘step-wise’ reduction in human activity follows, from the latter date to 815–685 cal. BC, and a brief but pronounced cessation at 690–535 cal. BC. Renewed woodland clearance and agriculture commenced until 415–250 cal. BC. From the latter date until cal. AD 390–540, the Late Iron Age/Early Medieval period, a phase of woodland recovery is attested, followed by renewed landscape disturbance and arable agriculture in particular, continuing to the close of the record at cal. AD 780–1035.

The Swedish Jordan Expedition 2013 at Tall Abu al-Kharaz. Preliminary results from Areas 9, 10 and 11

2014 ◽  
Vol 7 ◽  
pp. 129-148 ◽  
Author(s):  
Peter M. Fischer ◽  
Teresa Bürge
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Early Bronze Age ◽  
Jordan Valley ◽  
North East ◽  
The North ◽  
Late Iron Age ◽  
12Th Century ◽  
Iron Age I ◽  
The City

The Swedish excavations at Tall Abu al-Kharaz, a twelve-hectare tell in the central Jordan Valley, continued in 2013 in order to shed further light on the Iron Age occupation of this city that was first settled around 3200 BC, corresponding to the conventional Early Bronze Age IB. The Iron Age occupation lasted from the 12th century BC until 732 BC, when the city was conquered by the Neo-Assyrians. From 2009 to 2012, excavations in Area 9 revealed an exceptionally well-preserved two-storey compound dating from Iron Age I (local Phase IX), i.e. around 1100 BC. The stone compound was exposed for a length of 46 m. It consists of 21 rooms, with walls still standing to a height of more than 2 m. Several hundred complete vessels and other objects point to the extensive contacts of a fairly rich society. Contacts with the Aegean and Cyprus, through offshoots of the Sea Peoples/Philistines, and with Egypt and Phoenicia, were ascertained. At the end of the 2012 season, the eastern limit of the compound was reached. In 2013, complementary excavations were carried out to the north and east of the compound. The eastern extension revealed a defence system which had originally been built in the Early Bronze Age IB/II around 3100 BC but had been reused as a part of the Iron Age I defence structures. Test trenches in the north-eastern part of Area 10 and in Area 11 north-east of Area 10, i.e. a hitherto unexplored area of the city, revealed remains from the Late Bronze Age and the Early and Late Iron Age.

The Long and Winding Road that Leads to Angkor

2012 ◽  
Vol 22 (2) ◽  
pp. 265-289 ◽  
Author(s):  
Charles Higham
Keyword(s):  
Southeast Asia ◽  
Bronze Age ◽  
Iron Age ◽  
Eleventh Century ◽  
Southern China ◽  
Hunter Gatherers ◽  
Rice Farmers ◽  
Late Iron Age ◽  
Colonial Empire ◽  
French Colonial

In the late sixteenth century, Portuguese missionaries encountered a vast city at Angkor. Abandoned for 150 years, it had been partially restored as a Buddhist piligrimage centre but many of the monuments had been given over to the forest. They wondered about its origins. Some suggested that it was the work of Trajan, others of Alexander the Great. Following the establishment of the French colonial empire in Southeast Asia three centuries later, and in the absence of any information on prehistoric societies, the civilization of Angkor was seen as the result of Indianization, whereby Indian religions, architecture, writing and language were adopted by the indigenous inhabitants. This article presents the results of twenty years of research in the upper Mun Valley of northeast Thailand, an area that was part of the Kingdom of Angkor and seat of the dynasty of two of its greatest kings, Suryavarman II and Jayavarman VII. For the first time, the entire prehistoric cultural sequence from late hunter-gatherers to the end of the Iron Age has been documented and dated. We find that after the ingress of rice farmers from southern China in the mid second millennium BC, there were two surges in social complexity. Both were coincidental with the availability of new exotic goods through exchange. The first took place in the initial Bronze Age, in the eleventh century BC, and was followed by several centuries of relative poverty in mortuary practices. The second took place in the late Iron Age and led directly to the foundation of powerful chiefdoms from which can be traced the genesis of early civilizations in Southeast Asia, including that of Angkor.

The Romano-British Shrines at Brigstock, Northants

1963 ◽  
Vol 43 (2) ◽  
pp. 228-263 ◽  
Author(s):  
Ernest Greenfield
Keyword(s):  
Iron Age ◽  
Fourth Century ◽  
Third Century ◽  
The Third ◽  
Late Iron Age ◽  
Polygonal Shape

SummaryTwo shrines of circular and polygonal shape, probably part of a larger group, were erected early in the second half of the third century A.D., and occupied until late in the fourth century. The shrines occur in an area of widespread settlement dating from the late Iron Age until the end of the fourth century. Many objects of bronze and iron of ritual significance, together with a large number of votive deposits and coins, were recovered from the circular shrine. Miss M. V. Taylor's discussion of the principal objects appears on pp. 264–8.

The Britons in Southern Scotland

Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 77-88 ◽  
Author(s):  
Kenneth Jackson
Keyword(s):  
Iron Age ◽  
Roman Period ◽  
Anglo Saxon ◽  
Medieval Period ◽  
The West ◽  
Early Medieval Period ◽  
The North ◽  
Dark Ages ◽  
The People ◽  
Northern Portion

The archaeological background of the people of what is now Scotland south of the Forth and Clyde in the Roman period was a La Téne one, and specifically chiefly Iron Age B. This links them intimately with the Britons of southern Britain in the conglomeration of Celtic tribes who called themselves Brittones and spoke what we call the Brittonic or Ancient British form of Celtic, from which are descended the three modern languages of Welsh, Cornish and Breton. To the north of the Forth was a different people, the Picts. They too were Celts or partly Celts; probably not Brittones however, but a different branch of the Celtic race, though more closely related to the Brittones than to the Goidels of Ireland and (in later times) of the west of Scotland. Not being Brittonic, the Picts may be ignored here. Our southern Scottish Brittones are nothing but the northern portion of a common Brittonic population, from the southern portion of which come the people of Wales and Cornwall. Some historians speak of the northern Brittones as Welsh, following good Anglo-Saxon precedent, but this is apt to lead to confusion. The best term for them, in the Dark Ages and early Medieval period, as long as they survived, is ‘Cumbrians’, and for their language, ‘Cumbric’. They called themselves in Latin Cumbri and Cumbrenses, which is a Latinization of the native word Cymry, meaning ‘fellow-countrymen’, which both they and the Welsh used of themselves in common, and is still the Welsh name for the Welsh to the present day. The centre of their power was Strathclyde, the Clyde valley, with their capital at Dumbarton.

Bronze Age Barrows on Charmy Down and Lansdown, Somerset

1950 ◽  
Vol 30 (1-2) ◽  
pp. 34-46 ◽  
Author(s):  
Audrey Williams
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
The South ◽  
Stream Flows ◽  
North East ◽  
The North

Charmy Down is a plateau three miles north-east of Bath (fig. 1, 1), east of the Bath-Tetbury road. About a square mile in extent it has a general height of well over 600 ft. To the north the scarp falls swiftly, on the east more gently, to the wooded valley of St. Catherine's Brook, a tributary of the Bristol Avon and the modern Somerset–Gloucester boundary. At the foot of the steep western scarp a second stream flows south to the Avon. On the south Chilcombe Bottom separates Charmy Down from Solsbury Hill, distinguished by its Iron Age earthwork. The underlying rock is oolite, a southward continuation of the Cotswold formation.

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