Bronze Age Barrows on Charmy Down and Lansdown, Somerset

1950 ◽  
Vol 30 (1-2) ◽  
pp. 34-46 ◽  
Author(s):  
Audrey Williams

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.

Starinar ◽  
2009 ◽  
pp. 89-108 ◽  
Author(s):  
Aleksandar Bulatovic

Slightly biconical shaped bowls, the upper cone (rim and shoulder) of which is decorated with horizontal and slanted facets or slanted channels, as well as semi-globular bowls of inverted rim decorated with horizontal facets or slanted channels are characteristic of the end of Bronze Age and mark the beginning of Iron Age in many cultural groups within the Balkan Peninsula. Problem of their origin, chronology and distribution is present in archaeological literature for a long time. Many authors perceived the significance of this ceramic shape for the chronological, ethnic and cultural interpretation of the Late Bronze, that is, of the Early Iron Ages within the territory of the Balkans. Pottery from the burned layers in Vardina and Vardaroftsa sites in the north of Greece, among which there were bowls with inverted, slanted channeled rim, was designated way back by W. Heurtley as Danubian pottery or Lausitz ware, connecting its origin with the Danube Basin. Anumber of conclusions have been reached upon the study of finds of slightly biconical bowls and bowls of inverted rim, decorated with channels or facets, from several indicative sites from Late Bronze and Early Iron Ages within the Balkan Peninsula and south part of the Middle Europe. It has been stated that the bowls appear first within the southwest Slovakia and northwest Hungary in the Br D period, to spread very fast, already in the Br D/Ha A1 period, from its home territory to the east, to the northeast Hungary and northwest Romania. Namely, this first spreading wave into these territories brought along only variety Ia bowls, which were further distributed to the south, during the Ha A1 period, to the central parts of the Balkan Peninsula and consequently it can be concluded that these bowls are somewhat older than other varieties. In the period Br D - Ha A1, in north Hungary, under the influence of Gava Culture, on one hand, and Caka Culture, on the other, appear also variety IIa bowls (turban dish), distributed to the east with a new migration wave, in the same manner as was the case with the first migration wave, but also to the south, along the Bakonjska Range, to the present day Croatia and Slovenia, where, in the Ha A1/A2 periods, were stated exclusively variety IIa bowls. Representatives of the variety Ia bowls remained in the Pomoravlje region and Juzna Morava Basin, as confirmed by a large number of these bowls and also by other ceramic shapes of that stylistic and typological pattern, prevailing within this region in the Ha A1/A2 periods. First variety IIa bowls (Mediana, Krzince) appear only during the second migration wave coming from the north of the Balkans to the central part of the Balkan Peninsula (Ha A2 period). These bowls, however, are particularly characteristic of Macedonia and lower Povardarje, where variety Ia bowls were not stated at all. The second migration wave representatives, with turban dish bowls (variety IIa), were much more aggressive as witnessed by many burned settlements from that period in the Vranjska-Bujanovacka Valleys and Povardarje. During Ha B-C periods, bowls of both types (particularly variety IIa) became inevitable part of ceramic inventory of nearly all cultural groups in the Balkan Peninsula, which could be explained by the spread of cultural influence of the new stylistic trend, though, however, it could be possible that migrations, which at the time were numerous and of greater or lesser intensity, were one of the spreading causes of this ceramic shape into the east, south and west parts of the Balkan Peninsula in the Ha B period. Representatives of the mentioned migrations, which were carried out in at least two larger migration waves, bringing along bowls to the Balkan Peninsula, are protagonists of historically known migrations from that period, known under names of Doric and Aegean migrations. The assumed direction of these migrations coincides mainly with the distribution direction of bowl types I and II. Migrations spreading the bowl types I and II started in the south part of the Middle Europe, but were initiated by the representatives of the Urnenfelder cultural complex from the Middle Europe, as observed in certain ceramic shapes, stated together with type I bowls and originating from cultures of the Urnenfelder complex, and in numerous metal finds, which were produced in Middle European workshops. It is of interest to point out that bowl movements could be followed up to the northwest shores of the Aegean Sea, but they are not stated in the south Trace and in Troy, thus imposing conclusion that their representatives did not reach Troy. Consequently, their possible participation in destruction of VIIb2 layer settlements is utterly uncertain. The migrations, however, started chain reaction of ethnic movements in the Balkans, causing many ethnic and cultural changes within this territory which will lead to creation of new cultural groups to mark the developed Iron Age. To what extent bowls of this type, particularly variety IIa, left deep trace in the Iron Age Cultures in the central Balkans, is shown in the fact that survivals of this variety remained within these regions even several centuries later, in late phases of the Ha C period (VI/V century BC).


Author(s):  
Viacheslav Zabavin ◽  
◽  
Serhij Nebrat ◽  

The article presents the results of new research of the archeological expedition conducted by Mariupol State University in the North-East Azov Area. Archaeological research was carried out in the South of Donetsk region near the village of Yalta in 2016. In the mound 9 graves of the Bronze Age and 1 burial of the early Iron Age were investigated. The primary embankment was built during the Early Bronze Age by the tribes of the Pit Grave culture. The oldest burials in the mound are 4, 5 and 7. The most interesting was the children's burial 7. The buried child was accompanied by four ceramic vessels. Subsequently, another grave of the Pit Grave culture was built in the mound – burial 8. During the Late Bronze Age the population of the Zrubna / Timber-grave culture continues to use the necropolis. Researched at least three burials of the Zrubna / Timber-grave culture – 1, 2 and 10. Based on the typological analysis of the ritual-inventory complex, they can be attributed to the second (developed) horizon of the Zrubna / Timber-grave culture burial grounds of the North Azov Sea Area. As regards burial 3, presented by the authors, date back to the early Iron Age and precede the sites of the Scythian time. The burial 3 from Yalta are determined as complex of Chernohorivka type / Chernohorivka group of Cimmerian Culture or as late Chernohorivka complex. The authors consider peculiarities of the rite and inventory complex as well as some aspects of cultural and chronological character, spiritual and material culture of the tribes which, in the researchers’ view, are conflated with the historical Cimmerians. The burial in the mound placed near the villag of Yalta demonstrate some certain features of ingenuity. The man buried in the mound was most likely to have something to do with the religious or the hieratic sphere of life. The materials of the investigated burial mound enrich our knowledge about the ancient past of the population of the Azov steppes.


2018 ◽  
Vol 73 (1) ◽  
pp. 11-89
Author(s):  
Richard Massey ◽  
Elaine L. Morris

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.


1977 ◽  
Vol 43 ◽  
pp. 31-129 ◽  
Author(s):  
Ken Smith

Winklebury Camp (SU61355290), an Iron Age 'plateau fort’, now of some 7.6 hectares (19 acres), is situated in the parish of Basingstoke, approximately 1 mile north-west of the town centre of Basingstoke, (fig. 1), though it is now surrounded by housing estates. It occupies a hill of Upper Chalk which has been isolated from the main mass of the North Hampshire Downs by two dry river valleys, one trending south-east, the other north-east. Both are tributary to the R. Loddon. The hill rises to a maximum height of 126 m a.s.l., near the projected line of the western rampart and slopes off gradually to north and south, and more steeply to the south-east. About half a mile to the south of the fort, a tributary of the R. Loddon, now culverted, would have provided the nearest source of water.Winklebury Camp has suffered from gradual encroachment by the surrounding housing estates, losing the ditch and rampart face to the north and east, and ditch, rampart and a small part of the interior, to the west. Only to the south does any of the bank and ditch survive. In the south-west corner of the fort, in an area protected by the remains of a small copse, a 90 m length of eroded rampart remains to an approximate height of 2 m. There is no ditch fronting this rampart now, but immediately east of the end of the stretch of rampart is the only remaining length of ditch. This extends for some 200 m along the remainder of the south side of the fort, averaging 2 m deep and 5 m wide. It rises in the south-east corner at a causeway, beyond which is another short stretch of ditch which is rapidly lost in house gardens. This causeway is faced by rampart, but there are indications, for example a slight change in the direction of the rampart at this point, that this is in fact a blocked entrance.


Starinar ◽  
2010 ◽  
pp. 19-36
Author(s):  
Aleksandar Kapuran ◽  
Aleksandar Bulatovic ◽  
Igor Jovanovic

For many years, the territory along the course of the Crni Timok river in northeast Serbia was not presented as an interesting area for early Neolithic excavation. However, recent inspection of older unpublished data, with newer reconnaissance, has shed new light on this period of prehistory. A larger number of sites have been discovered with similar topographical positions on the edges/rims of large areas or on ridges above river courses. Thanks to cooperation between the geographical project TOPOI from Berlin and the Archaeological Institute in Belgrade, work has begun on the production of a digital ?archaeological model of probability? (ARM), which will improve reconnaissance of this region. Alongside the only systematic excavation/investigation of settlements in Kucajna, 16 more localities have been confirmed, situated in the area between the Roman imperial palace of Felix Romuiana in the south and Bor in the north. They are located at the following sites: Cerova Faca and Dubrava in Brestovac; Kot 1 and 2, Pundjilov potok (Pundjil?s stream) in Metovnica; La Bunar in Sarbanovac; Smolnica, Abri above Lazareve pecine (Lazarus? cave), Donja Stopanja (Lower Stopanja) Kobila in Zlot. In the area around Felix Romuliana several settlements have been discovered: in sectors Intra and Extra muros, Kravarnik, Varzari, Petronj 2, sites between Magura and Rimski majdan (Roman mine) and Visicina Basta. From the examination of finds discovered at these sites it can be concluded that on the territory along the course of the River Timok the population of the Starcevo-Keres-Kris cultural complex was relatively well established during the early Neolithic period. The Neolithic occupation of the region had proceeded from the Djerdap gorge in the north and Sicevacka, Svrljiska and Trgoviska gorges in the south, towards the course of the River Timok i.e. the central part of north-east Serbia. The Mesolithic populations had gradually accepted the production of food. Utilizing the optimal climate and fertile soil, they improved their husbandry through new agricultural methods and the better domestication of animals. This experimental process demanded successive migrations, which impoverished the quality of soil and the seasonal movements of animals that needed to be tamed. By analysis of the topographical and geomorphologic character of this terrain, early Neolithic settlements can be described as being agricultural-livestock husbandry and livestock husbandry-hunting based. The first settlements were located on gently inclined terrains relatively close to water sources, at altitudes of 180 to 300 m. The second category of settlements were formed on uplands, offering a better view of the terrain, 230 to over 450 metres above sea level. These were probably short-term or seasonal settlements since such territories were usually unsuitable for habitation during the winter months. The poor geomorphology of the land, the magma-rock substratum and ill-drained soil, in combination with primitive agriculture, guaranteed greater soil erosion, which would destroy the economic worth of the soil. With the disappearance of the early- Neolithic population from this region, human habitation did not reoccur until several millennia later, during the middle Bronze age.


1925 ◽  
Vol 5 (1) ◽  
pp. 80-82
Author(s):  
Prescott Row

The old manor of Waddon is part of the Parish of Croydon and lies to the south west of the Parish Church of that town. Here at the head of the Wandle River there are many evidences of a wide spread population in prehistoric times and the fields on the lower slopes of the North Downs which steadily rise from Waddon Station towards Purley are littered with flakes and have yielded many implements.The particular site to which I draw the attention of the Society, and indicate as the Cedars Estate, is easily reached by the bridle path running westward by Waddon Mill on the banks of the river, and the section under discussion, is the north east corner of the plot marked as Brandy Bottle Hill on the six inch Ordnance Survey. A hillock of Thanet sand here rises and extends eastward over the next field, the top of which is some 140 feet above sea level and makes a vantage spot with a good look out, over the wide stretches of the level plain running north from the present course of the Wandle river, in early times no doubt a stretch of marshland. It is still called Waddon Marsh.


1935 ◽  
Vol 1 ◽  
pp. 16-38 ◽  
Author(s):  
G. A. Holleyman ◽  
E. Cecil Curwen

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.


Author(s):  
Peter M. Fischer ◽  
Teresa Bürge

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.


2021 ◽  
Vol 43 (2) ◽  
pp. 116-130
Author(s):  
V.V. Noskevich ◽  
N.V. Fedorova ◽  
A.M. Yuminov

Kagarlinsk copper deposits have been worked out since IV millennium BC and till the end of II millennium BC in the steppes of the South Urals and a huge amount of copper have been recovered from their ores in the Bronze Age. Geophysical studies have been conducted in the south periphery of the Kagarlinsk ore field not far from Belousovka village at the mining-processing complex with the length of 900—1000 m and 30—70 m size across. Something like a hundred of small open-cut mines from 3 to 12 m in diameter are fixed in this area with near side mine dumps, sites for assortment of extracted ore adjoined at stove pits 3—5 m in diameter for burning up lump ores. Thorough topographic, gradient magnetic and geo-radar surveys have been fulfilled in areas where typical objects: open-cut mine, a pit for pilot burning up ores, slime sites and ore store are situated. As a result new data have been obtained on the structure of ancient outputs and associated technological facilities. Numerous magnetic anomalies revealed near the open-cut mine and a pit testify that copper ore encloses sufficient amount of iron and pilot assortment of the burned up ore took place near the pits. According to the results of geo-radar survey special features of pit-stove have been reconstructed and 3D model of the ancient open-cut mine built. A pit for burning up ore was cone-shaped with steps for comfort of loading and unloading ore. Its bottom diameter was 5m, the principal mine was 1—1.5 m in diameter and depth rough 3 m, the volume of the pit did not exceed 13—15 m3. Transversal size of a mine was 7—9 m and the depth was up to 4 m. The open-cut mine had steep sides from the north, east and south and in the west the relief was mildly sloping. The entrance to the open-cut mine was from the west. Initial depth of the open-cut mine differed from the present day surface by 2—3 m. According to our appraisal the amount of extracted ore in this mine was 25—30 tons. Taking into account the overall number of mines some 2—2.5 thousand tons of bulk ore were extracted during operation of Belousovka mining-metallurgical complex.


Author(s):  
Erika Weiberg

The point of departure for this paper is the publication of two Early Helladic sealing fragments from the coastal settlement of Asine on the north-east Peloponnese in Greece. After an initial description and discussion they are set in the context of sealing custom established on the Greek mainland around 2500 BCE. In the first part of the paper focus is on the apparent qualitative differences between the available seals and the contemporary seal impressions, as well as between different sealing assemblages on northeastern Peloponnese. This geographical emphasis is carried into the second part of the paper which is a review and contextualisation of the representational art of the Aegean Early Bronze Age in general, and northeastern Peloponnese in particular. Seal motifs and figurines are the main media for Early Helladic representational art preserved until today, yet in many ways very dissimilar. These opposites are explored in order to begin to build a better understanding of Peloponnesian representational art, the choices of motifs, and their roles in the lives of the Early Helladic people.


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