Notes and Inscriptions from Pisidia. Part II

1960 ◽  
Vol 10 ◽  
pp. 43-82 ◽  
Author(s):  
G. E. Bean
Keyword(s):  
The Other ◽  
Rock Surface ◽  
Mountain Range ◽  
The South ◽  
The West ◽  
Main Road ◽  
Rock Face ◽  
Eastern Side ◽  
East And West ◽  
The Hill

I pass now to the eastern side of the central mountain range, to the ancient sites lying east and west of the main Burdur–Antalya road.In the little plain of Çineovası, 13 km. from Burdur, about 300 yards east of the main road, just opposite the 110th kilometre-stone from Antalya, is a rocky hill some 40 m. high carrying a small fortified site that seems hitherto to have escaped observation. The top of the hill has been levelled to form an area some 25 by 15 m., surrounded on all four sides by a wall of excellent coursed polygonal masonry 1·20 m. thick (Pl. Va). On the west this wall merely supplements the precipitous rock-face; on the other sides it still stands to a height of some 5 m., and was originally much higher, as beds for polygonal blocks can be seen in several places in the rock-surface on the summit, and great quantities of these blocks are lying on the slopes below. In the interior are traces of four or five walls up to 1 m. thick, now flush with the ground, and a large rock-cut cistern some 5 by 4 m. and over 2 m. deep. At the south-east corner are the collapsed ruins of an ornamented building, the blocks carefully cut, with mouldings and clamp-holes; one of these blocks forms a shallow anta. Two architectural blocks apparently belonging to this building are lying in the cistern.

The West Court at Perachora

1967 ◽  
Vol 62 ◽  
pp. 353-371
Author(s):  
J. J. Coulton
Keyword(s):  
Short Distance ◽  
Sixth Century ◽  
East Side ◽  
The South ◽  
The West ◽  
Rock Face ◽  
North East ◽  
The North ◽  
South West ◽  
East And West

About 10 metres south-west of the sixth-century temple of Hera Akraia at Perachora, and nearly due west of the little harbour lies the small courtyard previously known as the ‘Agora’. Since its purpose is not known, it will here be non-committally referred to as the West Court. It was first excavated in 1932, and more fully, under the supervision of J. K. Brock, in 1933, but it was not entirely cleared until 1939, and it was at that time that the Roman house which stood in the middle of the court was demolished. The West Court is discussed briefly (under the name of ‘Agora’) in Perachora 1 and in the preliminary reports of the Perachora excavations. Short supplementary excavations were carried out in 1964 and 1966 to examine certain points of the structure.In shape the West Court is an irregular pentagon, about 24 metres from north to south and the same from east to west (Fig. 1; Plate 91 a, b). It is enclosed on the west, north, and on part, at least, of the east side by a wall of orthostates on an ashlar foundation. For a short distance on either side of the south corner, the court is bounded by a vertically dressed rock face which is extended to the north-east and west by walls of polygonal masonry. At the south-west corner the west orthostate wall butts against the polygonal wall, which continues for about 0·80 m. beyond it and then returns north for about 8 metres behind it.

Excavations at Fishbourne, 1965. Fifth Interim Report

1966 ◽  
Vol 46 (1) ◽  
pp. 26-38
Author(s):  
Barry Cunliffe
Keyword(s):  
Detailed Examination ◽  
Masonry Buildings ◽  
Interim Report ◽  
The South ◽  
The West ◽  
Main Road ◽  
Main Site ◽  
The North ◽  
East And West

The excavations of 1965 were largely concerned with the examination of the field containing the east and west wings of the palace and the Great Court which lies between them. As last year's work had almost completed the outline plan of the palace, the 1965 season was concentrated upon the detailed examination of the audience chamber and the entrance hall, the sample excavation of the garden about which practically nothing was known, and the area excavation of those parts of the timber and early masonry buildings belonging to the first-period settlement which had not previously been examined. In addition to this, trial trenches were cut through the newly acquired market-garden to the west of the main site, and further trenching was carried out in the fields to the north of the north wing and the field to the south of the modern main road. The final excavation of the north wing of the palace has been postponed until next season, after the construction of the modern cover-building has been completed.

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.

Art. VII.—Notes on Persian Belúchistán. From the Persian of Mirza Mehdy Khán. Published Teheran, July, 1875

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler
Keyword(s):  
Indian Ocean ◽  
Temperate Climate ◽  
The South ◽  
The West ◽  
The North ◽  
The People ◽  
The Indian Ocean ◽  
The Hill ◽  
Cool Climate

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.

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.

Ancient Cultivations at Housesteads, Northumberland

Antiquity ◽  
1931 ◽  
Vol 5 (19) ◽  
pp. 351-354
Author(s):  
W. Percy Hedley
Keyword(s):  
The South ◽  
The West ◽  
South Side ◽  
Close Proximity ◽  
Hadrian's Wall ◽  
The Military ◽  
The Hill ◽  
North And South

The Roman Fort of Borcovicium at Housesteads in Northumberland should need no introduction to anyone interested in archaeology. During the last year it has been brought into great prominence by being presented to the Nation by Mr John Maurice Clayton, and through its close proximity to the portion of Hadrian’s Wall recently threatened by quarrying operations.The fort at Housesteads was one of the earliest to be examined by British antiquaries, but although it has received so much attention its environs have been almost entirely disregarded. On both sides of the Military Way leading out of the west gateway was an extensive civil settlement, and traces of buildings can be seen on the south side of the fort. The hillside sloping to the southward is covered with the remains of early cultivations. These have generally been accepted as of Romano-British age. There are, however, two distinct systems of early cultivation. To the southwest of the fort there is a series of terraces running along the hillside, but on the southeast of the fort there are lynchets running north and south at regular interva up and down the hillside. From the hill to the south of Housesteads it can be clearly seen that where there is terrace cultivation it has been superimposed on the earlier system of lynchets, and this is also shown in air photographs.

III.—Picrite from the Ampwihi River, Mozambique

1917 ◽  
Vol 4 (4) ◽  
pp. 150-157 ◽  
Author(s):  
Arthur Holmes ◽  
H. F. Harwood
Keyword(s):  
Narrow Channel ◽  
Dry Season ◽  
The Other ◽  
The South ◽  
Eastern Side ◽  
South West ◽  
Western Side ◽  
The Right ◽  
Sand And Gravel ◽  
The Military

Almost due west of Mozambique Island, at a distance of about forty-two miles from the sea, the military road from Mosuril to Nampula crosses the Ampwihi River, an important tributary of the Monapo. During the dry season the stream is reduced to a string of stagnant pools, separated by long reaches of sand and gravel that here and there are interrupted by outcrops of the underlying formations. Throughout the greater part of its course the Ampwihi flows through a region in which gneisses persist with monotonous regularity, the only variation being that due to occasional intrusions of granite and of still later pegmatite dykes. At the point where the military road crosses the narrow channel a welcome diversion is introduced by the presence of a dark compact dyke about 10 feet in thickness. The dyke appears on the right-hand bank and crosses obliquely to the other side, taking a N.N.W.–S.S.E. course across the strike of the older rocks. Upstream, about seventy yards to the south-east, the Ampwihi bends to the south-west, so that it returns towards the dyke, which is again exposed across its sandy floor. The dyke was traced by Mr. E. J. Wayland in July, 1911, for a distance of altogether 200 yards, and was examined by Mr. D. Alex. Wray and later by myself during the same year. It is clearly the latest rock of the district, and is intruded along a line of fault, for in two cases pegmatite dykes seen on the eastern side are broken across and reappear on the western side with a well-marked northerly displacement.

Report on Excavations at Verulamium in 1934

1937 ◽  
Vol 17 (1) ◽  
pp. 28-55 ◽  
Author(s):  
A. W. G. Lowther
Keyword(s):  
The South ◽  
The West ◽  
Eastern Side ◽  
The North

During the time that the excavation of the theatre was being carried out, the investigation of insula XVI, immediately west of it, was begun, and was completed after some three months' work.The insula, a rectangle measuring 300 ft. by 160 ft. (with its greater length stretching from east to west) is bounded by roads on three sides, and by the metalled space surrounding the theatre on its fourth, or eastern, side. Cross-trenches showed the south road to be 29 ft., and the north road 18 ft., in width; the west road had been at least 29 ft. wide, but, owing to soil having been denuded from this higher part of the site, the exact width of this road was not determined by either of the two trenches dug across it (plan, pl. xxv).

Notes on the Types of English Villages and their Distribution

Antiquity ◽  
1927 ◽  
Vol 1 (4) ◽  
pp. 447-468 ◽  
Author(s):  
William Page
Keyword(s):  
Small Groups ◽  
Local Knowledge ◽  
The Other ◽  
Division I ◽  
The West ◽  
Main Road ◽  
The Subject ◽  
The Church ◽  
Mountainous Country

Little has been done towards solving the problem of the Saxon settlement of England by studying the types of villages and their distribution. Professor Maitland saw the importance of the subject and pointed out how valuable in this respect was the ordnance map ‘that marvellous palimpsest which under Dr Meitzen's guidance we are beginning to decipher’. Helpful, however, as the ordnance maps are, they cannot be read alone, a knowledge of the archaeology, history and topography of the district under review is a necessary equipment for such an investigation. The remarks here made are tentative and are offered in the hope they may be an incentive to others with local knowledge to examine the evidence of their districts.Professor Maitland, following Dr. Meitzen and others, has adopted two main types of settlements, namely, the scattered or dispersed, and the nucleated or clustered. These two types probably comprehend all forms of settlements, but certainly the nucleated type and possibly the scattered type, show many variants which it may be well to indicate before a methodical study of the subject can be made. I have elsewhere suggested the following classification of English towns and villages which will no doubt require modification and amplification but may meet a want for a preliminary inquiry; (I) scattered or dispersed settlements, (2) nucleated or clustered settlements off lines of communication, (3) nucleated settlements on lines of communication, (4) ring-fence settlements, (5) towns with bridge heads and double towns, (6) towns of gridiron plan, (7) towns of spider's web plan, (8) Bastide towns. Except for the first of these classes all of them are nucleated or clustered, and to this wider division I propose to devote my attention. It may perhaps be pointed out, however, that the scattered or dispersed settlements occur chiefly in Wales and in the west and north of England. They are found throughout Cornwall, in Devon, Somerset and the open parts of the Welsh border counties, in Yorkshire and Derbyshire, and probably they are the origin of the great parishes with their numerous townships of the other northern counties. They were adapted for a pastoral people and are generally to be found in moorland or mountainous country which has become divided into large parishes. They consist of hamlets and single houses or small groups of houses scattered somewhat promiscuously throughout a district. The principal hamlet from which the settlement or parish takes its name-which was probably the meeting place of the district and where the church was eventually placed-was generally on high land or a main road and frequently at cross roads, bridges, or such like places of nodality.

The inscriptions of south-east Chios, I

1963 ◽  
Vol 58 ◽  
pp. 53-67
Author(s):  
W. G. Forrest
Keyword(s):  
The Other ◽  
The South ◽  
The West ◽  
The North ◽  
British School ◽  
Comparative Safety

The plains of Pyrgi, Kalamoti, and Dotia, in the south-east corner of Chios, form a single geographic unit, bounded in the east by the hills which run inland from the promontory of Agridia, in the west by the low range of Kampia, Aradhopetra, and Kakopetria, and in the north by the more formidable barrier of the central mountains of the island. In them there are traces of several ancient sites, at Pindakas, Dotia, and elsewhere, but these appear to have been little more than isolated farmhouses or small sanctuaries and it is almost certain that most of the inscriptions from the area came originally from the major sites at Emporio and Phanai. From these they have been transported, some as far as Chios town, most to other local sites, to country churches or to the medieval towns of Pyrgi and Kalamoti. In many cases it is now impossible to trace their origin (even those which have reached the comparative safety of the Museum are often without record of their provenance), and it would therefore be pointless to try to isolate the inscriptions of any one ancient centre. For this reason I have collected here, in addition to the few inscriptions discovered in the British School excavations at Emporio, all the other material known to have been found in the area. For convenience I reproduce all but the most accessible texts in full. Generally it has been possible to check earlier readings on the stone (in which case the text is my own without any note of alterations unless they are significant); those which I have not seen are marked with an asterisk.

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