An Iron-Age Site near Radley, Berks.

1931 ◽  
Vol 11 (4) ◽  
pp. 399-404
Author(s):  
E. Thurlow Leeds

In 1928 by courteous permission of Mr. Badcock, the owner, the Oxford University Archaeological Society, under the supervision of Mr. R. T. Lattey, was able to examine a site in a field bounded on the west by the road leading from Radley village to Abingdon and on the south by a second road leading eastwards towards Radley station. There, on the wall of a disused gravelpit, holes filled with earth had produced evidence of human occupation. Exploration of some of these resulted in the discovery of a series of trenches, the relation of which to one another could not be exactly determined owing to the limited area available for investigation. One piece of trench ran with a somewhat north-easterly trend up to the northern edge of the field, with a recessed pit about 4½ ft. across at one point, while a second longer stretch, after running in a north-westerly direction for a few yards, turned almost at right angles towards the south-west, and some distance farther on, at the point where the excavations had to cease, appeared to be bending southwards.

2018 ◽  
Vol 73 (1) ◽  
pp. 110-136
Author(s):  
Oliver Good ◽  
Richard Massey

Three individual areas, totalling 0.55ha, were excavated at the Cadnam Farm site, following evaluation. Area 1 contained a D-shaped enclosure of Middle Iron Age date, associated with the remains of a roundhouse, and a ditched drove-way. Other features included refuse pits, a four-post structure and a small post-built structure of circular plan. Area 2 contained the superimposed foundation gullies of two Middle Iron Age roundhouses, adjacent to a probable third example. Area 3 contained a small number of Middle Iron Age pits, together with undated, post-built structures of probable Middle Iron Age date, including a roundhouse and four and six-post structures. Two large boundary ditches extended from the south-west corner of Area 3, and were interpreted as the funnelled entrance of a drove-way. These contained both domestic and industrial refuse of the late Iron Age date in their fills.


Mnemosyne ◽  
2016 ◽  
Vol 69 (2) ◽  
pp. 202-225
Author(s):  
Sarah Pothecary

A number of places that feature in Strabo’s description of the Asian peninsula were situated on the ancient road that ran between the Euphrates river and the city of Ephesus. It is likely that Strabo journeyed along the entire thousand-kilometre length of the road, even though he makes explicit reference to his presence in only a few locations. He most probably made the journey as a youth on his way to Roman Asia, in the south west of the peninsula, from Pontus in the north. Decades pass before Strabo, as an old man, writes the Geography and includes in it the memories of places he had visited. The outdated tone of some of his descriptions reflects this passage of time.


A number of samples of subfossil Cepaea nemoralis and hortensis from sites in southern Britain of archaeological interest, ranging in date from about 4500 b .c . to Romano-British and Anglo-Saxon, have been scored for frequency of the major banding morphs, and compared with present-day samples taken on each site or as near to it as these species could be found. In C. nemoralis there is a significant decrease of unbandeds from pre-iron Age samples to the corresponding ones for the present day, but no indication of systematic change from Iron Age samples to the present day. Spread banded also shows changes from pre-iron Age samples to present-day ones, but very little change from the early Iron Age to the present day. The smaller samples of C. hortensis available give no sign of a trend although there is much change from pre-iron Age times to the present; Iron Age samples and the corresponding present-day ones do not show the relative constancy of composition seen in C. nemoralis —as usual these two very closely related species are behaving differently. At the present day there is evidence (experimental and distributional) that the frequencies of banding morphs of C. nemoralis are affected by climate, unbandeds and mid-bandeds being favoured by better summers than those normal in Britain at present. The available evidence, from pollen analysis and other sources, of changes in the climate of southern Britain in the last 6500 years suggests that the observed differences in morph frequencies can be related to known climatic changes, in agreement with present-day evidence. One area effect (south-west M arlborough Downs) has contracted and become less intense since pre-iron Age times, as perhaps have others; in some cases a site has remained in an area effect, but the effect itself has changed. Two pairs of samples from lowland sites appear to have changed from frequencies indicating area effects in pre-iron Age times to others consistent with visual selection at the present day. Area effects seem to have been rather constant from the Iron Age to the present day.


2013 ◽  
Vol 17 (2) ◽  
pp. 115-151
Author(s):  
Christian Konrad Piller

According to some classical authors, the region south-west of the Caspian Sea was inhabited by the large tribe of the Cadusians (Greek Καδουσιοι, Latin Cadusii). During the Achaemenid Period, several armed conflicts between the Imperial Persian forces and the warlike Cadusians occurred. Of particular importance is the disastrous defeat of Artaxerxes II in 380 B.C. From the archaeological point of view, little has been known about the material culture of the Achaemenid Period (Iron Age IV) in Talesh and Gilan. Until recently, only a few burial contexts from the South of Gilan could be dated to the period between the 6th and 4th centuries B.C. However, during the last two decades, Iranian archaeologists excavated numerous Bronze and Iron Age graveyards in the Talesh Region. A number of burial contexts at sites, such as Maryan, Mianroud or Vaske can securely be dated to the Achaemenid Period. With this new material basis, it was possible to subdivide the Iron Age IV into different subsequent phases. Furthermore, it is likely that the material culture described in this article could be at least partially attributed to the Cadusians.


2000 ◽  
Vol 95 ◽  
pp. 259-299 ◽  
Author(s):  
J. N. Coldstream

Among over 1800 boxes of Sir Arthur Evans's finds now stored in the Stratigraphical Museum at Knossos, at least 150 contain Greek pottery from Subminoan to Classical. A systematic study of this material, in relation to its recorded find spots, throws new light on the eastern part of the early Greek town, bordering the site of the Minoan Palace. Above the Palace itself, fresh evidence is produced, and fresh interpretation offered, for the Greek sanctuary described by Evans. In its immediate surroundings, there are signs of busy domestic and industrial life in the early Greek town above the South-West Houses, the West Court, the Theatral Area, and the Pillared Hall outside the North Entrance to the Palace. Greek occupation is also noted above the House of Frescoes, the Little Palace and the Royal Villa. A wider aim of this article is to trace the limits of the early Greek town of Knossos, both of its original Early Iron Age nucleus surviving from Late Minoan times, and of its spacious extension towards the north in the late eighth and seventh centuries BC.


Author(s):  
Valter Lang

This chapter examines Iron Age funerary and domestic archaeological sites, and economic and cultural developments from c.500 BC–AD 550/600, in the east Baltic region (present day Estonia, Latvia, and Lithuania). While the early pre-Roman Iron Age was to some extent a continuation of the late Bronze Age in material culture terms, many changes took place in the late pre-Roman Iron Age. At the change of era, new cultural trends spread over the east Baltic region, from the south-eastern shore of the Baltic to south-west Finland, which produced a remarkable unification of material culture over this entire region up to the Migration period. Differences in burial practices and ceramics, however, indicate the existence of two distinct ethnic groups, Proto-Finnic in the northern part of the region and Proto-Baltic to the south. Subsistence was based principally on agriculture and stock rearing, with minor variations in the economic orientation of different areas.


1969 ◽  
Vol 34 ◽  
pp. 148-190 ◽  
Author(s):  
I. M. Stead ◽  
M. Jarman ◽  
Angela Fagg ◽  
E. S. Higgs ◽  
C. B. Denston

The Iron Age hill-fort at Grimthorpe (Grid reference SE.816535) in the parish of Millington, East Riding of Yorkshire, is on the western edge of the Yorkshire Wolds, with a commanding position over the Vale of York. There is an uninterrupted view to the White Horse on the Hambleton Hills, 25 miles to the north-west; beyond York, 13 miles to the west, to the Pennines; and to the south 25 miles to the chimneys of Keadby and Scunthorpe. To the west and south the land slopes away to the Vale of York, and to the north and east there is a sharper fall to Given Dale and Whitekeld Dale. The hill-fort defences follow the 520 feet contour, and enclose an approximately circular area of eight acres (fig. 1).A traditional reference may be preserved in the field-name—Bruffs—perhaps a variation of ‘Brough’, which ‘refers in all cases to ancient camps, usually Roman ones’. But all surface indications have now been obliterated by ploughing, and even a century ago there was little more to be seen. John Phillips in 1853 noticed ‘unmistakable traces of ancient but unascertainable occupation’, and in 1871 an excavation by J. R. Mortimer located ‘the filled up inner ditch of a supposed camp’. But Mortimer was not concerned with the settlement; his interest had been aroused by the discovery, in 1868, of a burial with rich grave-goods, including metalwork with La Tène ornament, in a chalk-pit within the south-west sector of the hill-fort.


1998 ◽  
Vol 64 ◽  
pp. 331-342 ◽  
Author(s):  
Michael Fulford ◽  
John Creighton
Keyword(s):  
Iron Age ◽  

The discovery by Mr David Walsh, a local metal detectorist, of what proved to be a Late Iron Age, decorated bronze mirror was reported to us on its discovery in the autumn of 1994 and led to a small excavation of the context and immediate environs of the find (Figs 1–2). It was made on the south-facing slope of a low hill, at about the 75 m contour, at SU 632 603 in LP 3516 which lies just within the parish of Bramley and at the southern extremities of a Roman settlement that developed around the junction of the Roman roads leading from Silchester to Winchester and Chichester. The findspot is thus some 2 km south-south-west of the walled area of the Roman town which overlies the heart of the Late Iron AgeoppidumofCalleva. The overall extent of the site as revealed by the distribution of artefacts in the ploughsoil has been plotted by Corney over an area in excess of 6 ha (1984, 283–5, figs 81–3). Although some Silchester Ware of latest Iron Age and earliest Roman date had been recovered from around the centre of the settlement, the bulk of the pottery suggested occupation lay principally between the late 1st/early 2nd century AD and the late 4th century AD.


Sign in / Sign up

Export Citation Format

Share Document