Daggers in the West: Early Bronze Age Daggers and Knives in the South-west Peninsula

2013 ◽  
Vol 79 ◽  
pp. 165-191 ◽  
Author(s):  
Andy M. Jones ◽  
Henrietta Quinnell
Keyword(s):  
Bronze Age ◽  
Copper Alloy ◽  
Radiocarbon Dating ◽  
Human Remains ◽  
Early Bronze Age ◽  
The South ◽  
The West ◽  
South West ◽  
South West England

This paper describes the results from a project to date Early Bronze Age daggers and knives from barrows in south-west England. Copper alloy daggers are found in the earliest Beaker associated graves and continue to accompany human remains until the end of the Early Bronze Age. They have been identified as key markers of Early Bronze Age graves since the earliest antiquarian excavations and typological sequences have been suggested to provide dating for the graves in which they are found. However, comparatively few southern British daggers are associated with radiocarbon determinations. To help address this problem, five sites in south-west England sites were identified which had daggers and knives, four of copper alloy and one of flint, and associated cremated bone for radiocarbon dating. Three sites were identified in Cornwall (Fore Down, Rosecliston, Pelynt) and two in Devon (Upton Pyne and Huntshaw). Ten samples from these sites were submitted for radiocarbon dating. All but one (Upton Pyne) are associated with two or more dates. The resulting radiocarbon determinations revealed that daggers/knives were occasionally deposited in barrow-associated contexts in the south-west from c. 1900 to 1500 calbc.The dagger at Huntshaw, Devon, was of Camerton-Snowshill type and the dates were earlier than those generally proposed but similar to that obtained from cremated bone found with another dagger of this type from Cowleaze in Dorset: these dates may necessitate reconsideration of the chronology of these daggers

Excavation of Four Barrows, and a Middle Bronze Age Cremation Cemetery, at Heatherstone Grange, Bransgore, Hampshire

2018 ◽  
Vol 73 (1) ◽  
pp. 11-89
Author(s):  
Richard Massey ◽  
Elaine L. Morris
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Early Bronze Age ◽  
The South ◽  
The West ◽  
Radiocarbon Dates ◽  
North West ◽  
The North ◽  
South West ◽  
Middle Bronze Age

Excavation at Heatherstone Grange, Bransgore, Hampshire, investigated features identified in a previous evaluation. Area A included ring ditches representing two barrows. Barrow 1.1 held 40 secondary pits, including 34 cremation-related deposits of Middle Bronze Age date, and Barrow 1.2 had five inserted pits, including three cremation graves, one of which dated to the earlier Bronze Age, and was found with an accessory cup. A number of pits, not all associated with cremation burials, contained well-preserved urns of the regional Deverel-Rimbury tradition and occasional sherds from similar vessels, which produced a closely-clustered range of eight radiocarbon dates centred around 1300 BC. Of ten pits in Area C, three were cremation graves, of which one was radiocarbon-dated to the Early Bronze Age and associated with a collared urn, while four contained only pyre debris. Barrow 1.3, in Area E, to the south, enclosed five pits, including one associated with a beaker vessel, and was surrounded by a timber circle. Area F, further to the south-west, included two pits of domestic character with charcoal-rich fills and the remains of pottery vessels, together with the probable remains of a ditched enclosure and two sets of paired postholes. Area H, located to the north-west of Area E, partly revealed a ring ditch (Barrow 1.4), which enclosed two pits with charcoal-rich fills, one with a single Late Bronze Age/Early Iron Age potsherd, and the other burnt and worked flint. A further undated pit was situated to the east of Barrow 1.4. The cremation cemetery inserted into Barrow 1.1 represents a substantial addition to the regional record of Middle Bronze Age cremation burials, and demonstrates important affinities with the contemporary cemeteries of the Stour Valley to the west, and sites on Cranborne Chase, to the north-west.

Prehistoric Roads and Tracks in Somerset, England: 2. Neolithic

1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
Extensive Region ◽  
Peat Deposits ◽  
Third Millennium ◽  
South West England

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).

On the number of Patella species in south-west England

1980 ◽  
Vol 60 (3) ◽  
pp. 565-574 ◽  
Author(s):  
Patrick M. Gaffney
Keyword(s):  
Morphological Variation ◽  
West Coast ◽  
Gel Electrophoresis ◽  
The South ◽  
The West ◽  
Enzyme Systems ◽  
South West ◽  
South West Coast ◽  
East West ◽  
South West England

Limpet populations of the genus Patella from the south-west coast of England were examined by means of gel electrophoresis in order to settle debate on the specific status of the three Patella forms. Populations varied morphologically along an east-west gradient, from three distinct forms in the west to continuous intergradation in the east, in accord with earlier studies. Patella collected were divided into three groups on the basis of a complex of external features described by earlier workers, corresponding to the morphologically defined taxa P. vulgata Linn., 1758, P. aspera Röding, 1798, and P. depressa Pennant, 1777. These groups were electrophoretically distinct in five of seven enzyme systems examined, with no hybrids or intermediates. Incomplete speciation and hybridization can be ruled out as possible causes of the observed morphological variation.

Tarkasnawa King of Mira ‘Tarkondemos’, Boǧazköy sealings and Karabel

1998 ◽  
Vol 48 ◽  
pp. 1-32 ◽  
Author(s):  
J. D. Hawkins
Keyword(s):  
Bronze Age ◽  
Historical Geography ◽  
Western Anatolia ◽  
Late Bronze Age ◽  
Major Advance ◽  
The South ◽  
The West ◽  
South West ◽  
Historical Figure ◽  
Western Border

The historical geography of Anatolia in the period sourced by the Boǧazköy texts (Middle-Late Bronze Age) has proved an on-going problem since they first became available, and nowhere was this more acutely felt than in southern and western Anatolia, generally acknowledged as the site of the Arzawa lands, also probably the Lukka lands. A major advance has been registered since the mid-1980s, with the publication and interpretation of the Hieroglyphic inscription of Tudhaliya IV from Yalburt, and the Cuneiform treaty on the Bronze Tablet of the same king. These two documents have established that the later territory of Rough Cilicia constituted the Late Bronze Age kingdom of Tarhuntassa with its western border at Perge in Pamphylia, and that the Lukka lands did indeed occupy all of (or more than) classical Lycia in the south-west. These recognitions, by establishing the geography of the south and south-west, correspondingly reduced the areas of uncertainty in the west.In 1997 I was fortunately able to establish the reading of the Hieroglyphic inscription attached to the long-known Karabel relief, which lies inland from Izmir in a pass across the Tmolos range between Ephesos and Sardis. This can be shown to give the name of Tarkasnawa, King of Mira, and those of his father and grandfather, also kings of Mira but with names of uncertain reading. This is the same king known from his silver seal (referred to as ‘Tarkondemos' from an early and incorrect identification), and impressions of other seals of his have more recently been found at Boǧazköy. Clearly he was an important historical figure.

Excavations at Hacılar, First Preliminary Report

1958 ◽  
Vol 8 ◽  
pp. 127-156 ◽  
Author(s):  
James Mellaart
Keyword(s):  
Bronze Age ◽  
Preliminary Report ◽  
River Valley ◽  
Early Bronze Age ◽  
The South ◽  
Entire Surface ◽  
Main Road ◽  
South West ◽  
Antique Dealer ◽  
The Village

The village of Hacilar is situated in the Vilayet of Burdur in South-west Anatolia, about 25 km. west of Burdur itself on the main road to Yeşilova and Denizli. The chalcolithic site lies about 1·5 km. west of the village and just beyond the orchards, which are irrigated by a plentiful spring at the foot of a great limestone crag which overlooks the village. It is this spring which since neolithic times has been the main reason for more or less continuous occupation in this region. Apart from the neolithic and early chalcolithic site at Hacılar there is a large Early Bronze Age mound on the northern outskirts and a classical site to the south-west of the village.The prehistoric site is an inconspicuous mound, about 150 metres in diameter, rising to a height of not more than 1·50 m. above the level of the surrounding fields (Fig. 1 and Pl. XXIXa). The entire surface of the mound is under cultivation and a series of depressions show the holes made by a local antique-dealer in search of painted pots and small objects. About 1 km. west of the site runs the Koca Çay, the ancient Lysis, and on the eastern scarp of this river valley lies the cemetery of the Early Bronze Age settlement. Not a single burial has yet been found in the chalcolithic or neolithic levels of our site and it is therefore not unreasonable to suggest that its cemetery also may eventually be located there.

Maiden Castle: excavation, education, entertainment?

Antiquity ◽  
1985 ◽  
Vol 59 (226) ◽  
pp. 97-100 ◽  
Author(s):  
G. J. Wainwright ◽  
B. W. Cunliffe
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
The South ◽  
The West ◽  
South Side ◽  
South West ◽  
The One ◽  
Great Complexity

In its developed or final form Maiden Castle, some two miles (3.2 km) south-west of Dorchester in Dorset, is an iron age hillfort, of great complexity, which takes in two knolls of a saddle-backed spur of Upper Chalk, the highest point of which is about 440 ft (c.134 m) above OD. The defences enclose47 acres (c.18 ha) and consist of three banks and two ditches with an additional bank inserted along most of the south side. There are two entrances, at the east and at the west, each with double openings elaborately defended by outworks. The outstandingly imposing character of Maiden Castle is derived from the size and complexity of these earthwork defences rather than from its altitude or the natural defensive advantages of its position. Ptolemy has been thought to supply a hint as to the ancient name of Maiden Castle. The conventional identification of Roman Dnrchester is with theDurnovaniaof the Antonine Itinerary. Ptolemy omits that placename, but mentionsDuniumin the same region as the one city apparently worthy of mention in the territory of the Durotriges (GeographiaI, 103, ed. C Müller (1883)).Duniumwas long ago identified with Maiden Castle. This may well be so, although recently Hod Hill and Hengistbury have also been put forward as possibilities. Part of the hillfort lies on the site of a neolithic causewayed enclosure and it also surrounds a unique ‘long-mound’ of the same period, a bronze age round barrow and the foundations of a Romano-British temple and accompanying buildings.

scholarly journals Fugitive Monuments and Animal Pathways: Explaining the Stone Settings of Exmoor

2015 ◽  
Vol 81 ◽  
pp. 87-106 ◽  
Author(s):  
Mark Gillings
Keyword(s):  
Bronze Age ◽  
Critical Comment ◽  
Early Bronze Age ◽  
South West ◽  
Widespread Phenomenon ◽  
Human Animal ◽  
South West England

As a result of the exclusive use of extremely small megaliths (miniliths), the prehistoric stone settings of Exmoor, south-west England, challenge current approaches to the interpretation of monumental stone architecture during the later Neolithic and Early Bronze Age. Whilst the broader context of the practice of erecting tiny upright stones (a seemingly diverse and widespread phenomenon) and the reasons why this diminutive architecture has tended to escape sustained critical comment have been explored (smaller stone elements being relegated to a generalised background or subsidiary role such as ‘packing’), attempts to explain the settings have been remarkably few. Drawing upon the results of ten years of piecemeal fieldwork on the moor the present paper seeks to rectify this, arguing that far from being generalised ritual structures or metaphorical expressions of hunting groups, the tiny stones were, instead, an integral part of a dynamic human–animal landscape of movement and pause.

Excavations at Stavros, Ithaca, in 1937

1952 ◽  
Vol 47 ◽  
pp. 227-242 ◽  
Author(s):  
Helen Waterhouse
Keyword(s):  
Water Supply ◽  
Bronze Age ◽  
Small Area ◽  
Limited Extent ◽  
The South ◽  
The West ◽  
Main Site ◽  
South West ◽  
Narrow Ridge ◽  
The Village

For three weeks of May–June 1937 excavations of limited extent were conducted at Stavros in northern Ithaca. The main site was a small area immediately below the village square to the south-west, where chance finds by the proprietor of the land, followed in 1936 by a trial excavation, had revealed the presence of Greek graves and a Bronze Age deposit.Stavros lies on a narrow ridge commanding the bays of Phrikes to the east and Polis to the west. Along this ridge must at all times have run the route from the south of the island to Pelikata and the fertile valley of Kalamos. Below the ridge, to the south west, there is a good water-supply at Asprosykia, where late Helladic sherds are recorded. The existence of large dressed blocks lower down the slope at the head of the valley, and of other blocks and rock-cuttings farther westwards, towards Polis Bay, suggests that a not inconsiderable town stood here in classical times.

scholarly journals Neolithic Complex of the Settlement of Barsova Gora II/9

2020 ◽  
Vol 19 (7) ◽  
pp. 191-202
Author(s):  
Yury P. Chemyakin
Keyword(s):  
Bronze Age ◽  
Radiocarbon Dating ◽  
Stone Tools ◽  
Early Bronze Age ◽  
Functional Identification ◽  
Early Neolithic ◽  
The West ◽  
Settlement Type ◽  
Time Periods ◽  
The Right

Purpose. Materials published here describe findings on the ancient settlement Barsova Gora II/9b (located 7 km to the west of Surgut city on the right bank of the Ob river). Over the 5 years of excavations, the remains of structures from different time periods were uncovered and studied, among which 5 seated below grade square and rectangular dwellings stand out. Results. Original flat-bottomed pottery, clay ornamented bars and a spherical pommel have been found inside these dwellings. Clay bars were probably used as spatulas for smoothing dishes, skin scrapers. Among stone tools, polished ones predominate: chopping tools (axes, adzes, chisels, including grooved ones), lancet-shaped arrowheads and knives, as well as abrasives. Flint tool findings were less common: a few leaf-shaped arrowheads, scrapers and one lithic core. A fragment of a quartz lithic core and about ten quartz flakes were found as well. Among the pottery next to flat-bottomed vessels, there are round-bottomed vessels. Generally pottery is decorated in a variety of ways – drawn, impaled, using a walking comb stamp, with pits. Among the patterns there appears straight, broken or wavy lines, areas of a walking stamp. Clear geometric shapes are rare. On some pots horizontal compositions are replaced by vertical ones in the lower half of the vessels. Flat bottoms are ornamented with crossed, wavy and other patterns. Conclusion. Incorrect functional identification of the clay bars during first excavations led to initial incorrect dating of the settlement as belonging to the Early Bronze Age. The stratigraphy and radiocarbon dating during the new excavations revealed earlier settlement dates going back to early Neolithic. Some similarities to these structures and settlement type can be found in the ancient settlements of Boborykino and Bystrinsky cultures, Petrovoborsky and Kayukovsky types, settlements of Amnya I and others within the Eneolithic Period as well. However, the settlement of Barsova Gora II/9b is a unique cultural type dating from 6th – early 5th millennium BC.

Celtic fields and farms on Dartmoor, in the light of recent excavations at Kestor

1955 ◽  
Vol 20 (1) ◽  
pp. 87-102 ◽  
Author(s):  
Aileen Fox
Keyword(s):  
Bronze Age ◽  
Early Bronze Age ◽  
The South ◽  
Steep Ascent ◽  
South West ◽  
Rock Formations ◽  
Coastal Belt ◽  
Open Country ◽  
Pastoral Economy ◽  
Light Shading

The granite upland of Dartmoor has attracted settlers coming into the south-west of Britain from the early Bronze Age (Beaker phase) onwards. The long outline of the moor is visible from the South Devon coast, which with its series of good harbours invites intrusion. The navigable lower reaches of the south-flowing rivers—the Plym, Yealm, Erme, Avon, Dart and Teign—and the ridgeways along their watersheds provide convenient thoroughfares across the intervening coastal belt, the South Hams and the hinterland of Torbay, as far as the foot of the main escarpment. Above this steep ascent, where the granite overlies the Devonian rock formations, and where the rivers run in deep wooded gorges, the moorland mass forms a rolling tableland (1000-1400 feet high), broken only by the profile of the numerous upland valleys or by the fantastic eroded outlines of the tors. It is in this zone (light shading, fig. 1) that the evidence for most of the prehistoric settlement and early cultivation is to be found. Between 1400 and 1500 feet, the ground rises markedly again to the uninhabited northern heights (Yestor 2039 feet) and the southern heights (Ryder's Hill 1692 feet), in which the rivers have their sources and which are now blanketed in peat bog (dark shading, fig. 1). The heights apart, Dartmoor contains a broad tract of elevated open country, well-watered grass and heather moor, ideally suited to sustain a primitive pastoral economy. In many places on the marginal slopes and in the upland valleys a sufficient depth of sandy soil has accumulated on top of the rock to make arable cultivation possible; at present, cultivation ceases at about 1000 feet, which is the normal tres line.

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