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.

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

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.

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.

The Late Bronze Age in the West and the Aegean

2012 ◽  
Author(s):  
Trevor Bryce
Keyword(s):  
Bronze Age ◽  
Western Anatolia ◽  
Late Bronze Age ◽  
The West ◽  
Population Groups ◽  
Wide Range ◽  
First Millennium ◽  
Second Millennium Bce

This article presents data on western Anatolia during the Late Bronze Age, wherein it was the homeland of a wide range of states and population groups. The most important and most powerful of these was a group of kingdoms that are attested in Hittite texts as the Arzawa Lands. Most scholars associate the development of these kingdoms with Luwian-speaking populations who had occupied large parts of Anatolia from (at least) the early second millennium BCE. The most enduring link between Anatolia's Late Bronze Age civilizations and their first-millennium-BCE successors is provided by the Lukka people, one of the Luwian-speaking population groups of southwestern Anatolia. They were almost certainly among the most important agents for the continuity and spread of Luwian culture in southern Anatolia throughout the first millennium BCE.

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.

Troy in recent perspective

2002 ◽  
Vol 52 ◽  
pp. 75-109 ◽  
Author(s):  
D.F. Easton ◽  
J.D. Hawkins ◽  
A.G. Sherratt ◽  
E.S. Sherratt
Keyword(s):  
Bronze Age ◽  
Recent Progress ◽  
Historical Geography ◽  
Political Capital ◽  
Western Anatolia ◽  
Late Bronze Age ◽  
Detailed Consideration ◽  
The Press ◽  
Sharp Criticism ◽  
The University

AbstractThe historic series of excavations of Hisarlik-Troy have been continued over the last 15 years by a collaboration between teams from the universities of Tübingen and Cincinnati with fruitful results. Over the year 2001 however the director, Manfred Korfmann, attracted sharp criticism from colleagues, largely through the medium of the press, for his methods and publications. He was accused of exaggerating the importance of the site in the Late Bronze Age, particularly as a political capital and trading centre of Anatolia, and more specifically of unduly inflating the results of his investigations of the lower city. A symposium was convened by the University of Tübingen in February 2002 with a view to discussing these criticisms and the defence in an academic atmosphere. The four authors of this article attended the Tübingen symposium. After listening to the contributions it seemed to us that an assessment of the issues from our respective view-points would be timely: thus a detailed consideration of the archaeological questions, a review of the notable recent progress in Hittite sources firming up the historical geography of western Anatolia, and an evaluation of Troy's position in Late Bronze Age trade. In all these areas we conclude that the criticisms of Korfmann are themselves considerably exaggerated.

Late Bronze Age Lynchet-Settlements on Plumpton Plain, Sussex

1935 ◽  
Vol 1 ◽  
pp. 16-38 ◽  
Author(s):  
G. A. Holleyman ◽  
E. Cecil Curwen
Keyword(s):  
Bronze Age ◽  
Late Bronze Age ◽  
The South ◽  
The West ◽  
North West ◽  
North East ◽  
The North ◽  
Primary Object ◽  
North Edge ◽  
North And South

Plumpton plain is situated on the top of the South Downs, roughly 600 feet above sea level, six miles north-east of Brighton and four miles north-west of Lewes (fig. 1). From its western end a broad spur slopes gently southwards from the northern escarpment of the Downs, lying between Moustone Valley on the south-east and Faulkners Bottom on the west. Most of this Downland is covered with a dense scrub of gorse, thorn and bramble, and with large patches of bracken and heather. A series of broad paths running roughly at right angles with one another has been cut through this vegetation to facilitate the preservation of game. Along the main ridge of the spur running north and south is a broad gallop which, at a height of 600 feet O.D., passes through a group of earthworks situated 1500 feet from the north edge of the Downs and 2300 feet east of Streathill Farm. This group was the primary object of bur investigations and will be referred to as Site A (fig. 2).Site B (fig. 3) lies a quarter of a mile to the south-east of Site A on a small lateral spur jutting between the twin heads of Moustone Bottom. The only visible evidence of prehistoric occupation was a quantity of coarse gritty sherds and calcined flints on the surface to the south-east of a low bank and ditch which runs across the spur.Several groups of lynchets enclosing square Celtic fields are to be seen in the neighbourhood of these two sites. They lie principally to the south-east of Site A and to the south of Site B.

The Base and Top of the Coral-rock in Barbados

1937 ◽  
Vol 74 (8) ◽  
pp. 337-359 ◽  
Author(s):  
C. T. Trechmann
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
East Part ◽  
Varying Thickness ◽  
South West ◽  
New Information ◽  
Main Portion ◽  
Coral Rock

1. The coral-rock commences nearly everywhere with a basal bed of varying thickness containing a fauna of pre-Pleistocene aspect among which the genus Haliotis (absent from these coasts at the present day), Pleurotomaria, Meiocardia, etc., are noticeable. This faunule may have lived at a depth of 700–1,000 feet.2. The supposition that the southerly anticlines are a later uplift than the main portion of Barbados is supported by the absence of ravines, and the presence of post-coral-rock beds which occur as coastal veneers at low altitudes, and in greater thickness in the south-east corner near Whitehaven.3. The south-east part of the island from Consett Point to Ragged Point has probably extended further seawards in comparatively recent times ; the series of converging faults and dislocations in the cliff sections suggest that the thrusts from the west or south-west may have been resisted by this part of the island.4. The relative claims of fault-scarping or marine erosion in production of the rising terraces is discussed ; and new information regarding the thickness of the coral-rock at sea-level from a boring is detailed.5. The finding of a faunule with Pliocene or possibly Miocene affinities at the base of the coral-rock puts the Oceanic series further back, into the Miocene.

scholarly journals The Results of a Chemical, Microscopical and Bacteriological Examination of Samples of London Milks

1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton
Keyword(s):  
Bacteriological Examination ◽  
Milk Supply ◽  
The South ◽  
The West ◽  
The North ◽  
South West ◽  
Pure Milk

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.

The End of the Bronze Age in the South West Copaïc

Euphrosyne ◽  
1973 ◽  
Vol 6 ◽  
pp. 7-21
Author(s):  
John M. Fossey
Keyword(s):  
Bronze Age ◽  
The South ◽  
South West ◽  
The Bronze Age
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