Seuthopolis

Antiquity ◽  
1961 ◽  
Vol 35 (138) ◽  
pp. 91-102 ◽  
Author(s):  
Dimiter P. Dimitrov
Keyword(s):  
Left Bank ◽  
The South ◽  
The West ◽  
The North ◽  
Steep Slopes ◽  
The Village ◽  
River Banks ◽  
Natural Barriers

The site of the Thracian city of Seuthopolis lies about 8 km. to the west of Kazanluk, in the famous Valley of Roses, between the Balkan Range and the Sredna Gora Mountains. A spacious terraced area was formed by the erosion of the River Toundja (the ancient Thracian Tonsus); this is bounded to the north and east by a sloping plateau, on the site of the villages of Koprinka and Dounavtsi; and to the south, the steep slopes of the heights (site of the village of Morozovo (formerly Gorno Cherkovishté), the last of the Sredna Gora foothills, dropped down to the river banks. The last and lowest step of this terraced area projects deep into the bends of the Toundja to the south, forming a peninsula, or tongue of land, the banks of which are 4 to 5 m. in height; to the west and south it is bounded by the River Toundja, and to the east the Golyama Varovitsa or Chiflikchiiska River, a small, but always swiftly flowing tributary of the Toundja, guards its approaches. The Thracian city of Seuthopolis was situated precisely on this spot, called ‘Chiflika’ (The Farm), on the left bank of the River Toundja, defended from the west, south and east by natural barriers of water (PLATE IX).

scholarly journals The Tsakonian Dialect.—I

1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt
Keyword(s):  
East Coast ◽  
Mountain Range ◽  
The South ◽  
The West ◽  
Northern Boundary ◽  
Grazing Land ◽  
Bare Rock ◽  
The North ◽  
Cultivable Land ◽  
The Village

The area over which the Tsakonian dialect is spoken lies on the east coast of the Peloponnese between the Parnon range and the sea. Its northern boundary is roughly the torrent which, rising on Parnon above Kastánitsa, flows into the sea near Ayios Andréas, its southern the torrent which, also rising on Parnon, passes through Lenídhi to the sea. A mountain range stretches along the coast from end to end of the district, reaching its highest point (1114 metres) in Mt. Sevetíla above the village of Korakovúni. Between Tyrós and Pramateftí, the seaward slopes of this range are gentle and well covered with soil. Behind these coast hills there stretches a long highland plain, known as the Palaiókhora, which, in the north, is fairly well covered with soil, but gradually rises towards the south into a region of stony grazing land, and terminates abruptly in the heights above Lenídhi. The high hill of Oríonda rises out of the Palaiókhora to the west and forms a natural centre-point of the whole district. Behind it stretching up to the bare rock of Parnon, is rough hilly country, cut here and there by ravines and offering but rare patches of cultivable land.

Laconia

1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls
Keyword(s):  
Sea Level ◽  
The Other ◽  
The South ◽  
The West ◽  
Urban Settlement ◽  
West Side ◽  
The North ◽  
The Village

The village of Kalývia Sokhás lies against the base of one of the massive foothills in which Taygetus falls to the plain three or four miles to the south of Sparta (Plate 26, 1). It is bounded by two rivers which flow down in deep clefts from the mountain shelf. The hillside above rises steeply to a summit which is girt with cliffs on all but the west side and cannot be much less than four thousand feet above sea level; this von Prott believed to be the peak of Taleton. Its summit is crowned by the ruins of a mediaeval castle which was undoubtedly built as a stronghold to overlook the Spartan plain; the only dateable object found there, a sherd of elaborate incised ware, indicates occupation at the time when the Byzantines were in possession of Mystra. The location of the other sites mentioned by Pausanias in this region remains obscure, but fortunately that of the Spartan Eleusinion has not been in doubt since von Prott discovered a cache of inscriptions at the ruined church of H. Sophia in the village of Kalývia Sokhás. In 1910 Dawkins dug trenches at the foot of the slope immediately above the village and recovered a fragment of a stele relating to the cult of the goddesses and pieces of inscribed tiles from the sanctuary. The abundance of water in the southern ravine led von Prott to conclude that the old town of Bryseai with its cult of Dionysus also lay at Kalývia Sokhás; but no traces of urban settlement have come to light at the village, and the name rather suggests copious springs such as issue from the mountain foot at Kefalári a mile to the north where ancient blocks are to be seen in the fields.

Halmyris, a settlement and fort near the mouth of the Danube: interim report

2002 ◽  
Vol 15 ◽  
pp. 230-245 ◽  
Author(s):  
Mihail Zahariade ◽  
Myrna K. Phelps
Keyword(s):  
Local Environment ◽  
Danube Delta ◽  
Interim Report ◽  
The South ◽  
The West ◽  
The North ◽  
First Millennium ◽  
The Village

Ancient Halmyris lies in the NW corner of the Dobrudja region in SE Romania. It liesc.2.5 km east of the village of Murighiol on a rocky promontory which is slightly higher than the surrounding marshes. This is at the E end of the Dunavat peninsula (known in antiquity asExtrema Scythiae Minoris: Jord., Get.266) and it is bordered by the Danube delta on the north and east, Razelm lake on the south, and the Tulcea hills on the west (fig. 1). The site was occupied continuously from at least the mid-first millennium B.C. up to the 7th c. A.D. The local environment, flora and fauna were favourable to settlement until as a result of natural causes the Danube became almost inaccessible; from that point on, the settlement became vulnerable to human and other natural events and eventually it became deserted.The site is known today as Bataraia or Cetatea. In the early 20th c. the locals still called it the Genoese stronghold (Geneviz-Kaleh). In antiquity it lay on the bank of the southern arm of the Danube called Peuce (now known as Sfantu Gheorghe). Today the southern arm of the Danube runs 2 km north of the site and it is connected to Lake Murighiol by the Periboina canal. Until 1983 there were two lakes,c.100 andc.200 m from the site, modern relics of the ancient course of the river. To the east lie the Dunavat hills and to the south is Dealul Cetatea (“fort hill”) (fig. 2).

scholarly journals The Topography of the Scamander Valley.—I

1911 ◽  
Vol 17 ◽  
pp. 266-283 ◽  
Author(s):  
Walter Leaf
Keyword(s):  
The South ◽  
The North ◽  
Steep Slopes ◽  
High Road ◽  
River Banks

The course of the Scamander is divided into three well marked sections—valley basins divided by defiles. Beginning from the mouth we have first the Plain of Troy, of which nothing need be said here; enough has been written about it already. It is bounded on the south by the Bally Dagh and south of this again by the Kara Dagh. Into the bay between these two runs on the east a spur of the Kayaly Dagh. These hills descend in steep slopes to the river banks, and form a gorge of limestone cliffs some four miles long, nearly as far as Sarimsak Köprü (Garlic Bridge). The path from the north mounts the slopes of the Bally Dagh to a height of over 500 feet, then descends to the river where in the middle of the gorge there lies a small secluded plain—a spot of idyllic charm—and again rises to a height of over 600 feet in order to cross the southern barrier of the Kara Dagh and reach the high road from the Dardanelles to Ezine close to Sarimsak Köprü.

scholarly journals Notes and Inscriptions from Pamphylia

1911 ◽  
Vol 17 ◽  
pp. 215-249
Author(s):  
H. A. Ormerod ◽  
E. S. G. Robinson
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The North ◽  
Great Rivers ◽  
Short Time ◽  
The Village ◽  
The Town

The following notes were made by us on a short journey in Pamphylia during March 1911.It had been our intention on reaching Adalia about the middle of the month to go at once into Lycia, but the lateness of the season made the higher ground impossible, and it seemed better to spend a short time in examining the country in the immediate neighbourhood of Adalia, much of which was still imperfectly known (Fig. 1).The best description of the Pamphylian plain is that given by Lanckoronski. From the Kestros to the Melas stretches a low-lying, swampy plain, traversed by three great rivers which come down from the Pisidian highlands, feverish in summer, and during the winter months impossible for wheeled traffic. To the west of the Kestros rises a rocky plateau of travertine some hundred feet above sea-level, on which stands the town of Adalia (Attaleia) on cliffs above the sea, which diminish towards the west. To the north of Adalia rises a third level, which viewed from the south, resembles a high raised beach, running roughly parallel with the present coast as far as the village of Barsak. To the east of that point the hills turn in a north-easterly direction and sink gradually down towards the Kestros. The western part of the plateau is crossed by two main roads, leading respectively to Istanoz and Buldur.

scholarly journals XXIII.—On the Position of the Portus Lemanis of the Romans

Archaeologia ◽  
1867 ◽  
Vol 40 (2) ◽  
pp. 361-374
Author(s):  
Thomas Lewin
Keyword(s):  
The South ◽  
The West ◽  
Historic Period ◽  
South Side ◽  
North East ◽  
The North ◽  
The Common ◽  
East And West ◽  
The Hill ◽  
The Village

The Portus Lemanis must clearly have been one of the great thoroughfares between Britain and the Continent, and it is not a little singular that the position of a port once so famous should never have been satisfactorily settled. The common impression is that it lay at the foot of Lymne Hill. For the benefit of those who are not familiar with this neighbourhood, I should mention, in limine, that the village of Lymne or Lympne stands about 2½ miles to the west of Hythe, on the highest part of the cliff which girds in the eastern portion of Romney Marsh. On the declivity of the hill, about half-way down, is seen the old Roman castrum, called Stuttfall, occupying 10 or 12 acres. There are walls on the north, east, and west, and the east and west walls run down to the marsh itself; but, what is remarkable, the south side towards the marsh had never any wall,” and hence the erroneous notion so generally prevalent that at the foot of the castrum was once the Portus Lemanis, and that in the course of ages the sea retired from Lymne, when the port shifted to West Hythe, and that the sea again retired, when the port was transferred to Hythe. I shall endeavour to show that these changes, if they ever occurred, must have preceded the historic period, and that in the time of the Romans, as for many centuries afterwards, the only port was Hythe. In fact Portus and Hythe are the same thing, Portus in Latin being Hyð in Saxon.

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.

scholarly journals XXXIX. The lignites and clays of Bovey Tracey, Devonshire

1862 ◽  
Vol 152 ◽  
pp. 1019-1038 ◽  
Keyword(s):  
Far East ◽  
Left Bank ◽  
The South ◽  
North East ◽  
The North ◽  
South West ◽  
North Eastern ◽  
The Village ◽  
Western Portion ◽  
North Western

The little town or village of Bovey Tracey, in Devonshire, nestles at the foot of Dartmoor, very near its north-eastern extremity; it is situated on the left bank of the river Bovey, about two miles and a half above the point at which it falls into the Teign, and is about eleven miles from each of the towns Exeter, Torquay, and Totnes*,—bearing south-westerly from the first, north-westerly from the second, and northerly from the last. A considerable plain stretches away from it in a south-easterly direction, having a length of six miles from a point about a mile west of Bovey to another nearly as far east of Newton; its greatest breadth, from Chudleigh Bridge on the north-east to Blackpool on the south-west, is four miles. It forms a lake-like expansion of the valleys of the Teign and Bovey rivers, especially the latter, whose course it may be said to follow in the higher part, where it is most fully developed; whilst the Teign constitutes its axis below the junction of the two streams. Its upper, or north-western portion, immediately adjacent to the village, is known as “Bovey Heathfield,” and measures about 700 acres.

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.

Matronianus, Comes Isauriae: an Inscription from an Early Byzantine Basilica at Yanıkhan, Rough Cilicia

1985 ◽  
Vol 35 ◽  
pp. 93-97 ◽  
Author(s):  
Stephen Hill
Keyword(s):  
The South ◽  
Late Professor ◽  
The Road ◽  
Scrub Oak ◽  
The North ◽  
Wild Olive ◽  
On The Road ◽  
Olive Trees ◽  
The Village ◽  
Early Byzantine

The ruins at Yanıkhan form the remains of a Late Roman village in the interior of Rough Cilicia some 8 kilometres inland from the village of Limonlu on the road to Canbazlı (see Fig. 1). The site has not been frequently visited by scholars, and the first certain reference to its existence was made by the late Professor Michael Gough after his visit on 2 September 1959. Yanıkhan is now occupied only by the Yürüks who for years have wintered on the southern slopes of Sandal Dağ. The ancient settlement at Yanıkhan consisted of a village covering several acres. The remains are still extensive, and some, especially the North Basilica, are very well preserved, but there has been considerable disturbance in recent years as stone and rubble have been removed in order to create small arable clearings. The visible remains include many domestic buildings constructed both from polygonal masonry without mortar and from mortar and rubble with coursed smallstone facing. There are several underground cisterns and a range of olive presses. The countryside around the settlement has been terraced for agricultural purposes in antiquity, and is, like the settlement itself, densely covered with scrub oak and wild olive trees. The most impressive remains are those of the two basilical churches which are of little artistic pretension, but considerable architectural interest. The inscription which forms the substance of this article was found on the lintel block of the main west entrance of the South Basilica.

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