The Garamantes of Fezzan: Excavations on Zinchecra 1965–7

1970 ◽  
Vol 50 (1) ◽  
pp. 37-66 ◽  
Author(s):  
Charles Daniels

SummaryThe Garamantes inhabited Fezzan, now the Saharan province of the Libyan Arab Republic, their capital, Garama, lying c. 105 miles west of Sebha in the wadi el Agial. After an unruly early history they appear to have become pacified and open to Roman influence. Before Garama was founded the tribe inhabited the promontory fortress of Zinchecra c. 2½ miles to the south-west, where excavation has revealed three main periods of occupation. The earliest consists of rock-scooped hearths, the second of rough dry-stone and frond shelters with stone-lined hearths. The third is more complex with buildings ranging from rough shelters to well-built mud-brick ‘houses’, the latest of which date to the first century B.C. and employed dressed stone in their basal courses. At the start of this period a complex of enclosure banks and walls was thrown around the base of the spur. Finally the site was abandoned to cemeteries.

1919 ◽  
Vol 23 ◽  
pp. 64-66
Author(s):  
F. B. Welch
Keyword(s):  

I Here describe a few sites on the south side of the valley of the Strymon, which I noticed while stationed there in 1916–1918. All except No. 5 belong to the third type described by Wace and Thompson and consist of large, low flat-topped mounds covered with Hellenistic sherds. This part of the country was anciently inhabited by the Bisaltai.1. At kilometre 70 on the Salonika-Serres road, about three kilometres south-west of Sakavcha, and two-and-a-half kilometres west of Makesh. Round the edges the remains of ancient walls can be easily traced; in places they are still three feet high and the same thickness with small towers at irregular intervals. Remains of house walls can be found everywhere a few feet down.


1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements

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).


1989 ◽  
Vol 84 ◽  
pp. 177-185
Author(s):  
R.W.V. Catling ◽  
R.E. Jones

Two vases, a cup and an oinochoe, from Arkesine in south-west Amorgos are published for the first time. It is argued that both are probably Middle Protogeometric, one an import from Euboia, the other from the south-east Aegean; chemical analysis supports both attributions. Their implications for the early history of Amorgos are discussed.


Britannia ◽  
2018 ◽  
Vol 49 ◽  
pp. 53-77
Author(s):  
Matthew Symonds

AbstractExceptional aspects of the design and location of a pair of first-century fortlets on the Exmoor coast are explicable as a product of local influence. Previous explanations for the remote setting of these small posts and the distinctive defences securing them have focused on a signalling role, with the fortlets serving as a means to transmit messages to naval vessels patrolling the Bristol Channel. Instead, both the landscape setting and articulation with local settlement patterns imply that these installations strengthened pre-existing measures to counter coastal raiding. Parallels between this variant fortlet design and settlement morphology in the South-West peninsula suggest that the army co-opted an indigenous architectural style. The two fortlets could act as components of what was effectively a composite coastal cordon, built on collaboration between the Roman military and the local population.


1900 ◽  
Vol 32 (4) ◽  
pp. 763-768
Author(s):  
T. K. Krishṇa Menon

Malayalam is the language of the south-west of the Madras Presidency. It is the third most important language of the Presidency, the first and the second being Tamil and Telugu respectively. It is spoken in Malabar, Cochin, and Travancore. Out of a total of 5,932,207 inhabitants of these parts, 5,409,350 persons are those who speak Malayalam. These countries, taken as a whole, are bounded on the north, by South Canara, on the east by the far-famed Malaya range of mountains, on the south by the Indian Ocean, and on the west by the Arabian Sea.


2015 ◽  
Vol 8 ◽  
Author(s):  
Guilherme Frainer ◽  
Nicholas W. Daudt ◽  
Caio J. Carlos

We report on three aberrantly plumaged White-chinned PetrelsProcellaria aequinoctialisfrom the Brazilian Economic Exclusive Zone in the south-west Atlantic Ocean – the first reports based upon tangible evidence for the region. Two of them showed a low degree of colour aberration (some white around the eyes and on the upper-wing coverts), whereas the third exhibited the highest degree of plumage aberration so far reported for the species: a plumage mostly white with brown freckles on the upper- and under-parts, head and nape. We also commented on problems related to at-sea identification of aberrantly plumaged seabirds.


Archaeologia ◽  
1921 ◽  
Vol 71 ◽  
pp. 141-198 ◽  
Author(s):  
Alfred Heneage Cocks

The subject of this Report is one of several Romano-British sites in the Hambleden valley, about a mile south of the village of that name, not far from the south-west corner of the county of Buckingham. The finds lead to the inference that the homestead was built before the middle of the first century A. D., and occupied until the end of the fourth, the latest coins being dated 392-5. The southernmost extremity of the enclosure is barely 300 yards from the Thames at Hambleden Lock. The Oxford-London road, at a point a mile nearer Henley than Great Marlow, runs east and west, close to the Bucks, bank of the river, and a branch road turns off almost opposite the lock, and runs north to Hambleden Skirmett, Turville, Watlington, etc. The homestead is in the western angle formed by these two roads, and is on the Greenlands estate of Viscount Ham-bleden, to whom not only I personally, but I think all antiquaries, owe much for his liberality in financing the protracted excavations, and in building the Museum to house the results.


1916 ◽  
Vol 21 ◽  
pp. 84-124
Author(s):  
F. W. Hasluck

In the following paper an attempt has been made to bring together scattered notices from printed sources regarding the geographical distribution of the Bektashi sect, as indicated by the position of existing or formerly existing convents of the order. I have further included such information on this subject as I have been able to obtain from my own journeys and enquiries (1913–15) among the Bektashi: nearly all this information is gathered from Bektashi sources, and much from more than one such source. I hope to have made a fairly complete record of Bektashi establishments in Albania, now the most important sphere of their activities, and a substantial basis for further enquiry in the other countries where the sect is to be found, with the exception of Asia Minor, for which my sources are at present inadequate.From the evidence at our disposal the Bektashi establishments in Asia Minor would seem to be grouped most thickly in the ‘Kyzylbash’ or Shia Mahommedan districts, especially in (1) the vilayets of Angora and Sivas, and (2) in the south-west corner (Lycia) of that of Konia, where the Shia tribes are known from their occupation as Tachtadji (‘wood-cutters’). For the third great stronghold of Anatolian Shias, the Kurdish vilayets of Kharput and Erzeroum, no information as to Bektashi tekkes is available.


1986 ◽  
Vol 52 ◽  
pp. 31-51 ◽  
Author(s):  
Peter Drewett ◽  
C. Cartwright ◽  
S. Browne ◽  
K. D. Thomas ◽  
A. Thompson ◽  
...  

An extensively plough-damaged oval barrow of the third millennium bc was excavated. The entire mound had been removed by ploughing. No burials were found under the site of the mound but disarticulated human skeletal material was found in the ditches. The main flanking ditches appear to have silted in naturally with evidence of Beaker activity and Romano-British agriculture in the higher levels. Some evidence of deliberate back-filling, including the burial of carved chalk objects, was found in the ditches at the east end. A single Saxon hut was excavated in the north-east corner of the barrow and a rubbish deposit containing Middle Saxon pottery was found in the upper levels of the ditch in the south-west corner of the barrow.


1970 ◽  
Vol 28 ◽  
pp. 42-43
Author(s):  
K Perch-Nielsen

In this second year of the five year project of mapping the Scoresby Sund region three field parties spent the six-week season mapping in the northern part ofthe area. One party mapped the flat land south-west of Olympen, one party completed the map of the south-western part of Scoresby Land while the third party spent three weeksin the Werner Bjerge and the rest of the season in north-western Jameson Land.


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