scholarly journals Karian Sites and Inscriptions

1896 ◽  
Vol 16 ◽  
pp. 188-236 ◽  
Author(s):  
W. R. Paton ◽  
J. L. Myres
Keyword(s):  
The South ◽  
Hellenic Journal ◽  
The West ◽  
Short Account ◽  
The North ◽  
Made In

The sites and inscriptions which follow were noted during a series of short journeys made in 1893 and 1894 with the help of grants from the Hellenic and Royal Geographical Societies. The geographical and descriptive results are published in Journ. Roy. Geog. Soc. viii, (shortly to appear), and a short account of the geology in Journal Oxf. Junior Scientific Club, ii. 33 (Jan. 1896): cf. Proc. Brit. Ass. 1893 (Nottingham), p. 746. An account of Telmessos, Karyanda and Taramptos has already appeared in the Hellenic Journal, xiv. 373 ff.These researches are confined to the area included between Latmos (Besh-parmak) and the Latmian Gulf (Denizli Liman) on the north, the Marsyas valley (China Chai) on the east, the Gulf of Keramos on the south, and the sea on the west. Though sites already identified were in nearly all cases visited, they are not discussed here, unless there is fresh evidence to bring forward.

scholarly journals The Works of Pergamon and their Influence

1886 ◽  
Vol 7 ◽  
pp. 251-274
Author(s):  
L. R. Farnell
Keyword(s):  
Good Reason ◽  
Right Wing ◽  
Left Wing ◽  
The South ◽  
Hellenic Journal ◽  
The West ◽  
West Side ◽  
South West ◽  
The Right ◽  
Made In

The questions concerning the art of Pergamon, its characteristics and later influence, depend partly for their solution on the reconstruction and explanation of the fragments in Berlin. Much progress has been made in the work during the last year. The discovery which decided what was the breadth of the staircase, and what were the figures which adorned the left wing and the left staircase wall, has been already mentioned in the Hellenic Journal. It is now officially stated that the staircase was on the west side of the altar, although Bohn, in his survey of the site, at first conceived that this was impossible. Assuming that this point is now settled, we may note what is certain, or probable, or what is merely conjectural, in the placing of the groups. We know that the wing on the left of the staircase, and the left staircase-wall, were occupied by the deities of the sea and their antagonists: by Triton, Amphitrite, Nereus, and others which we cannot name. Among them, also, we may perhaps discern the figure of Hephaestos, and in their vicinity we must suppose Poseidon. On the right wing of the staircase, and around the south-west corner, we have good reason for placing Dionysos, with Cybele and her attendant goddesses, although the order of the slabs on which these latter are found is not the same as was formerly supposed.

Part II. The Grave Circle

1954 ◽  
Vol 49 ◽  
pp. 244-247
Author(s):  
A. J. B. Wace ◽  
F. H. Stubbings
Keyword(s):  
First Year ◽  
East Side ◽  
The South ◽  
The West ◽  
South Side ◽  
Double Ring ◽  
North East ◽  
The North ◽  
Western Half ◽  
Made In

In 1950 and 1952, in view of recent discussions about the date of the Grave Circle, we decided to make some fresh soundings in its supporting wall to see if any fresh evidence could be obtained. In the first year the work was confined to soundings in the battered supporting wall on the south side opposite the north-east corner of the House of the Warrior Vase, and was undertaken by Mr. Kenneth Rowe. In 1952 further soundings were made in the battered supporting wall, the wall at its base on the west was further examined, and a sectional cut was made across the double ring of standing slabs on the north-east side about midway between the entrance and the then surviving cover slabs. The work was then directed by Dr. F. H. Stubbings.At the time of Schliemann's excavations the western part of the double ring of vertical poros slabs of the Grave Circle, which rests on the battered supporting wall, was in a very ruinous condition. This can be seen clearly in Schliemann's illustration and in the photographs published later. After the close of Schliemann's and Stamatakes' excavations the supporting wall was restored both on the west and on the south, and the western half of the double ring of standing slabs was reconstructed. When Keramopoullos excavated the fallen rock in the centre of the circle the Greek Archaeological Service undertook some further work of conservation.

scholarly journals BRONZE CROSS-SHAPED PLAQUES AS A CHRONOLOGY INDICATOR OF SKYTHIAN KURGANS OF THE NORTH PONTIC REGION OF THE SECOND — THIRD QUARTER OF THE 4th CENTURY BC

2019 ◽  
Vol 31 (2) ◽  
pp. 157-170
Author(s):  
S. V. Polin ◽  
М. N. Daragan
Keyword(s):  
Black Sea ◽  
Forest Steppe ◽  
Left Bank ◽  
Main Zone ◽  
The South ◽  
The West ◽  
Black Sea Region ◽  
The North ◽  
Made In

In the Scythian kurgans of the IVth century BC in the Northern Black Sea region, 31 bronze cruciform plaques were found. Such plaques are found mainly in male graves and much less often in female ones. These plaques were used as quiver buckles and for attaching the quiver to the belt. The main zone of concentration of cross-shaped plaques finds covers is the territory of the Lower Dnieper region, directly to the Dnieper. Apparently, this indicates that they were made in this region, where their place of manufacture could be only Kamenskoe hillfort, which was the center of metallurgy and metalworking in Steppe Scythia. From here they diverged south-east to Sivash within the present-day Kherson region, and much further north to the forest-steppe within the present-day right-bank Cherkasy and left-bank Kiev regions. Cross-shaped plaques are indicators of the advance of the steppe Scythians from the Lower Dnieper region to the north in the Ukrainian forest-steppe, to the west as far as the Lower Danube and very close to the south-east to Sivash. The latter direction, apparently, corresponds to migrations to winter pastures. More than half of all finds of cross-shaped plaques reliably date from within the second to third quarters of the IVth century BC, which gives every reason to assume the same dating for the complexes, where there are no own dating materials. In general, such bronze cross-shaped plaques are a reliable chronological indicator Scythian burials of the Northern Black Sea region of the second — third quarter of the IVth century BC, and also partly ethnic.

2. The Surface Geology of Mid-Lochaber

1882 ◽  
Vol 11 ◽  
pp. 483-487
Author(s):  
Duns
Keyword(s):  
Point Of View ◽  
The Body ◽  
The South ◽  
The West ◽  
North East ◽  
The North ◽  
South West ◽  
Surface Geology ◽  
Made In

An attempt is made in this paper, mainly from the point of view of the Society's “Boulder Committee,” to examine and classify the surface-deposits of a comparatively small compact area, which is bounded on the north and north-east by the river Spean, on the south and south-west by the river Nevis, on the west and northwest by the Lochy and the Caledonian Canal, and on the east and south-east by the Nevis range of Mountains. Reference is also made to the district between the Nevis and Loch Linnhe, including Auchintore and part of Glen Nevis. The body of the paper is limited to the statement of phenomena. It is felt, however, that the chief value of a record of facts is to lead to a definite knowledge of the forces which underlie them, and of the laws of which they are the expression.

Blechkanne. Copper Hammered Pitchers of the First Centuries AD from the North Pontic Area and Sarmatia

2018 ◽  
Author(s):  
М.Ю. Трейстер
Keyword(s):  
Black Sea ◽  
The South ◽  
The West ◽  
North East ◽  
The North ◽  
Black Sea Coast ◽  
The Crimea ◽  
Sea Area ◽  
North Western ◽  
Made In

The article is devoted to the finds of jugs hammered out of sheet of the Straldzha type in the North Pontic region, which were first investigated by B.A. Raev in the 1970s and 1980s, who assumed that they were made in the workshops of Thrace. An analysis of the chronology of the vessels shows that in Sarmatia, with rare exception, predominate finds in the funeral contexts of the late 1st and the first half of the 2nd century AD., while in the Bosporus and partly in the South-Western Crimea, the finds of such pitchers predominate in the complexes and layers of the mid-3rd – early 4th century AD. Taking into account the finds of recent decades in the territory of the Western and North-Western Pontic area, in the Crimea, as well as in the burials of the nomads of Asian Sarmatia and the mapping of finds, it becomes evident that the center of the conglomeration of finds in the Northern Black Sea Coast is located in the Bosporan Kingdom with the “splashes” on adjacent territories: to the west – to the region of the South-Western Crimea and to the north-east – to the nomads of the Lower Don region. The doubts expressed by J. Kunow and D.B. Shelov over 30 years ago that pitchers of the Straldzha type were manufactured only in Thrace and Shelov’s assumption, that they may have been produced in the northern Black Sea area, become especially relevant now. To consider, as before, that all these pitchers, which were simple, easy in production and used most probably to boil water, found in the Northern Black Sea area (where the number of finds exceeds the Thracian ones by a factor of two) were made in Thrace, becomes more and more complicated and, in my opinion, contradicts logic. I am not going to postulate that the finds from Thrace were made in the Bosporan Kingdom, they could have been made in the local workshops or in Pannonia.

Excavations at Fishbourne, 1964: Fourth Interim Report

1965 ◽  
Vol 45 (1) ◽  
pp. 1-11
Author(s):  
Barry Cunliffe
Keyword(s):  
Interim Report ◽  
The South ◽  
The West ◽  
Main Road ◽  
Main Site ◽  
Main Building ◽  
The North ◽  
Southern Half ◽  
Eastern Half ◽  
Made In

During the fourth season of excavation at Fishbourne work was spread over an area of about ten acres, most of it being concentrated on three main sites: the west wing of the main building, the eastern half of the north wing, and the southern half of the east wing. In addition, exploratory trenches were dug through the area to the north of the north wing and several trial excavations were made in gardens to the south of the modern main road. Previously, in December 1963 and January 1964, limited excavations had been undertaken in the garden of no. 65 Fishbourne Road, in the area of the greenhouses to the west of the main site, and in other gardens further west.

US and Russian policies and strategies in the Middle East: Iraq and Syria as a model

2019 ◽  
pp. 220
Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed
Keyword(s):  
Middle East ◽  
East Asia ◽  
Balance Of Power ◽  
Western World ◽  
International Conflicts ◽  
The South ◽  
The West ◽  
The North ◽  
East Region ◽  
Middle East Region

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.

scholarly journals Gitksan

2016 ◽  
Vol 46 (3) ◽  
pp. 367-378 ◽  
Author(s):  
Jason Brown ◽  
Henry Davis ◽  
Michael Schwan ◽  
Barbara Sennott
Keyword(s):  
British Columbia ◽  
The South ◽  
The West ◽  
The North

Gitksan (git) is an Interior Tsimshianic language spoken in northwestern British Columbia, Canada. It is closely related to Nisga'a, and more distantly related to Coast Tsimshian and Southern Tsimshian. The specific dialect of Gitksan presented here is what can be called Eastern Gitksan, spoken in the villages of Kispiox (Ansbayaxw), Glen Vowell (Sigit'ox), and Hazelton (Git-an'maaxs), which contrasts with the Western dialects, spoken in the villages of Kitwanga (Gitwingax), Gitanyow (Git-anyaaw), and Kitseguecla (Gijigyukwhla). The primary phonological differences between the dialects are a lexical shift in vowels and the presence of stop lenition in the Eastern dialects. While there exists a dialect continuum, the primary cultural and political distinction drawn is between Eastern and Western Gitksan. For reference, Gitksan is bordered on the west by Nisga'a, in the south by Coast Tsimshian and Witsuwit'en, in the east by Dakelh and Sekani, and in the north by Tahltan (the latter four of these being Athabaskan languages).

The Origin of Neolithic Culture in Northern Europe

Antiquity ◽  
1949 ◽  
Vol 23 (91) ◽  
pp. 129-135 ◽  
Author(s):  
V. G. Childe
Keyword(s):  
Northern Europe ◽  
Southern Sweden ◽  
The South ◽  
The West ◽  
The North ◽  
Neolithic Culture ◽  
Northwest Germany ◽  
Shell Mounds ◽  
Expansive Group ◽  
Megalithic Tombs

Till 1948 the coherent record of farming in Northern Europe began with the neolithic culture represented in the Danish dysser (‘dolmens’) and most readily defined by the funnel-necked beakers, collared flasks and ‘amphorae’ found therein. As early as 1910 Gustav Kossinna had remarked that these distinctive ceramic types, and accordingly the culture they defined, were not confined to the West Baltic coastlands, but recurred in the valleys of the Upper Vistula and Oder to the east, to the south as far as the Upper Elbe and in northwest Germany and Holland too. He saw in this distribution evidence for the first expansion of Urindogermanen from their cradle in the Cimbrian peninsula. In the sequel Åberg filled in the documentation of this expansion with fresh spots on the distribution map and Kossinna himself distinguished typologically four main provinces or geographical groups—the Northern, Eastern, Southern and Western. Finally Jazdrzewski gave a standard account of the whole content of what had come to be called Kultura puharów lejkowatych, Trichterbecherkultur, or Tragtbaegerkulturen. As ‘Funnel-necked-beaker culture’ is a clumsy expression and English terminology is already overloaded with ‘beakers’, I shall use the term ‘First Northern’.The orgin of this vigorous and expansive group of cultivators and herdsmen has always been an enigma. Not even Kossinna imagined that the savages of the Ertebølle shell-mounds spontaneously began cultivating cereals and breeding sheep in Denmark. As dysser were regarded as megalithic tombs and as megaliths are Atlantic phenomena, he supposed that the bases of the neolithic economy were introduced from the West together with the ‘megalithic idea’. But the First Northern Farmers of the South and East groups did not build megalithic tombs. Moreover, in the last ten years an extension of the North group across southern Sweden as far as Södermannland has come to light, and these farmers too, though they used collared flasks and funnel-necked beakers, built no dolmens either. In any case there was nothing Western about the pottery from the Danish dysser, and Western types of arrow-head are conspicuously rare in Denmark.

A Reinterpretation of the Microlithic Industries of Wales

1963 ◽  
Vol 29 ◽  
pp. 99-132 ◽  
Author(s):  
G. J. Wainwright
Keyword(s):  
Short Distance ◽  
The South ◽  
The West ◽  
The North ◽  
South Wales ◽  
North Wales ◽  
River Valleys

The distribution of Mesolithic sites in Wales is controlled to a great extent by the terrain, for physiographically, Wales is a highland block defined on three sides by the sea and for the greater part of the fourth side by a sharp break of slope. Geologically the Principality is composed almost entirely of Palaeozoic rocks, of which the 600-foot contour encloses more than three quarters of the total area. There are extensive regions above 1,500 feet and 2,000 feet and in the north the peaks of Snowdonia and Cader Idris rise to 3,560 feet and 2,929 feet respectively. Indeed North Wales consists of an inhospitable highland massif, skirted by a lowland plateau and cut deeply by river valleys, providing only limited areas for settlement. The hills and mountains of Snowdonia with their extension at lower altitudes into the Lleyn Peninsula, and the ranges of Moelwyn, Manod Mawr, Arenig Fach and Cader Idris, are discouraging obstacles to penetration, save for a short distance along the river valleys. To the east of these peaks are extensive tracts of upland plateau dissected by rivers, bounded on the west by the vale of the river Conway and cleft by the Vale of Clwyd. To the east of this valley lies the Clwydian Range and further again to the east these uplands descend with milder contours to the Cheshire and Shropshire plains.To the south the district merges into the uplands of Central Wales, which are continuous until they are replaced by the lowland belt of South Wales.

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