scholarly journals Art. XII.—An Ancient Hindu Temple in the Punjāb

1903 ◽  
Vol 35 (2) ◽  
pp. 335-338
Author(s):  
W. S. Talbot

Some twelve miles east of the junction of the Sawān with the Indus, between Makhad and Kālābāgh, and about three miles due south of the village of Shāh Muhammad Wālī in the north-west corner of the Jhelum (Jehlam) district, is an old temple called Kālar or Sassī dā Kallara, which has hitherto escaped notice. It is situated at a height of about 1,100 feet above sea-level, on the edge of a hillock rising steeply from the bank of the Kas Letī, one of the torrents, tributary to the Sawān stream, which descend from the northern face of the Salt Range; it here passes through a rough tract of hillocks and ravines. The temple is in a ruinous condition, due largely to the gradual wearing away of the soft sandstone hillside on the edge of which it stands, and its further decay will probably be rapid.

1963 ◽  
Vol 9 ◽  
pp. 10-21
Author(s):  
W. H. Plommer

The following article forms the conclusion to my chapter in a projected work on the Temple of Hemithea at Kastabos. The sanctuary is described by Diodorus in Book v, 62—3, and lies about a thousand feet above sea-level on the north-west slopes of the Carian Chersonese, overlooking from the south-east the more easterly isthmus on the long Cnidian Peninsula. It is the first Greek sanctuary of any importance and the first peripteral temple to be explored in the Rhodian Incorporated Peraea (see Fraser and Bean, The Rhodian Peraea and Islands, pp. 123 ff.), of which the whole Chersonese formed part.Our excavation, primarily salvage-work in remote country after a forest-fire had uncovered the remains, formed one stage in the mapping of ancient cities and demes of this neighbourhood by Professor John Cook and Professor George Bean. It established, from a stamped vase-handle and an inscription on a subsidiary building, that this was indeed, as surmised by Cook, the shrine of Hemithea, a local healing-goddess evidently, as Diodorus shows, of considerable local repute. We found that its greatness virtually began in the late fourth century, and was perhaps of fairly short duration.


Archaeologia ◽  
1817 ◽  
Vol 18 ◽  
pp. 340-343
Author(s):  
Edward Daniel Clarke

It is not attaching too high a degree of importance to the study of Celtic antiquities, to maintain, that, owing to the attention now paid to it in this country, a light begins to break in upon that part of ancient history, which, beyond every other, seemed to present a forlorn investigation. All that relates to the aboriginal inhabitants of the north of Europe, would be involved in darkness but for the enquiries now instituted respecting Celtic sepulchres. From the information already received, concerning these sepulchres, it may be assumed, as a fact almost capable of actual demonstration, that the mounds, or barrows, common to all Great Britain, and to the neighbouring continent, together with all the tumuli fabled by Grecian and by Roman historians as the tombs of Giants, are so many several vestiges of that mighty family of Titan-Celts who gradually possessed all the eastern shores of the Mediterranean, and who extended their colonies over all the countries where Cyclopéan structures may be recognized; whether in the walls of Crotona, or the temple at Stonehénge; in the Cromlechs of Wales, or the trilithal monuments of Cimbrica Chersonesus; in Greece, or in Asia-Minor; in Syria, or in Egypt. It is with respect to Egypt alone, that an exception might perhaps be required; but history, while it deduces the origin of the worship of Minerva, at Sais, from the Phrygians, also relates of this people, that they were the oldest of mankind. The Cyclopéan architecture of Egypt may therefore be referred originally to the same source; but, as in making the following Observations brevity must be a principal object, it will be necessary to divest them of every thing that may seem like a Dissertation; and confine the statement, here offered, to the simple narrative of those facts, which have led to its introduction.


1954 ◽  
Vol 49 ◽  
pp. 248-253 ◽  
Author(s):  
K. R. Rowe

Schliemann on his plan of the acropolis of Mycenae marks a terrace wall on the north-west corner of the ‘summit’. Steffen on his plan of the acropolis marks the same wall as one of his ‘kyklopische Stutz- u. Abschnittsmauern’. Dr. Leicester Holland included the wall in his plan of the palace made during our excavations there in 1920–23. Then we thought that this wall was a terrace wall which supported the end of the inclined roadway which climbed the Citadel from the Ramp to the north-west Propylon (9) of the Palace with its paved forecourt (7).In 1939 in excavating the rock shelf to the east of the Guardroom (3, 4) and below the terrace wall which supports the temple foundations on the north, we found a much ruined wall (Fig. 7, Z) on the very edge of the rock shelf, which here drops abruptly to the north. This wall was associated with a Middle Helladic deposit. Above this lay a somewhat disturbed Late Helladic stratum where the splendid ivory group of two women and a boy was discovered. The wall is a packed construction of largish stones about 1·25 m. thick, and the deposit behind it rests in a hollow in the rock and was at most 1·25 m. deep.


Ocean Science ◽  
2019 ◽  
Vol 15 (1) ◽  
pp. 147-159 ◽  
Author(s):  
Alexander Harker ◽  
J. A. Mattias Green ◽  
Michael Schindelegger ◽  
Sophie-Berenice Wilmes

Abstract. An established tidal model, validated for present-day conditions, is used to investigate the effect of large levels of sea-level rise (SLR) on tidal characteristics around Australasia. SLR is implemented through a uniform depth increase across the model domain, with a comparison between the implementation of coastal defences or allowing low-lying land to flood. The complex spatial response of the semi-diurnal M2 constituent does not appear to be linear with the imposed SLR. The most predominant features of this response are the generation of new amphidromic systems within the Gulf of Carpentaria and large-amplitude changes in the Arafura Sea, to the north of Australia, and within embayments along Australia's north-west coast. Dissipation from M2 notably decreases along north-west Australia but is enhanced around New Zealand and the island chains to the north. The diurnal constituent, K1, is found to decrease in amplitude in the Gulf of Carpentaria when flooding is allowed. Coastal flooding has a profound impact on the response of tidal amplitudes to SLR by creating local regions of increased tidal dissipation and altering the coastal topography. Our results also highlight the necessity for regional models to use correct open boundary conditions reflecting the global tidal changes in response to SLR.


1978 ◽  
Vol 44 ◽  
pp. 309-433 ◽  
Author(s):  
Patricia M. L. Christie ◽  
S. M. Elsdon ◽  
G. W. Dimbleby ◽  
A. Saville ◽  
S. Rees ◽  
...  

The ancient village of Carn Euny, formerly known as Chapel Euny, lies on a south-west slope just above the 500 foot contour in the parish of Sancreed in West Cornwall (fig. 1). The granite uplands of the region are rich in antiquities, as a glance at a recent survey shows (Russell 1971), not least those of the prehistoric period. The hill on which the site is situated is crowned by the circular Iron Age Fort of Caer Brane (pl. 27). Across the dry valley to the north-west rises the mass of Bartinny Down, with its barrows, while in the valley below the site near the hamlet of Brane is a small, well preserved entrance grave and other evidence of prehistoric activity. To the south-east about one mile away is the recently excavated village of Goldherring dating from the first few centuries of our era (Guthrie 1969). From later times, the holy well of St Uny and the former chapel which gave its name to the site, lie nearby to the west. The village contains a fine souterrain, locally known as a fogou, after a Cornish word meaning a cave (Thomas 1966, 79).Nothing appears to have been known of the settlement or Fogou before the first half of the 19th century when the existence of an unexplored fogou at Chapel Uny is first mentioned by the Reverend John Buller (1842), shortly followed by Edmonds (1849) who described to the Penzance Natural History and Antiquarian Society an ‘Ancient Cave’ which had been discovered by miners prospecting for tin.


1917 ◽  
Vol 7 ◽  
pp. 98-119 ◽  
Author(s):  
M. V. Taylor

Woodeaton is a small Oxfordshire parish, four miles north-east of the centre of Oxford city and a little west of the wide marshy level of the ‘Plain of Otmoor.’ It stands on a low, detached and rounded hill, 315 feet above sea level, and 120 feet above Otmoor. In old days it must have been difficult of access, for Otmoor spreads away to the east of it; low pastures along the river Cherwell close it in on the north and west, while south-westwards, too, the land is low-lying and marshy. Even to the south-east a marshy hollow separates it from the wooded slopes of Beckley and Elsfield, once part of Shotover Forest. However, the well-known Roman road which connects Dorchester (Oxon.) with Alchester, and which passes along the foot of Shotover, and traverses the village of Beckley and the plain of Otmoor, runs within two miles of Woodeaton; in dry seasons it may have helped those who wished to get to the spot.


1948 ◽  
Vol 68 ◽  
pp. 152-155
Author(s):  
R. E. Wycherley

The stoa investigated by the Americans in the N.W. corner of the agora of Athens has won with good reason a notable place among ancient monuments, both as a subject of topographical controversy and as an interesting architectural type. I should like to turn to it again for a short time and in particular to examine at greater length than was possible in a brief review C. Anti's theory of its genesis, given in Chap. IX of his Teatri Greci Arcaici. As the non-committal name given to it in my heading shows, I should like for the present to steer clear as far as possible of the difficult problem of its identification. Anti confidently assumes that the building was the Stoa Basileios; indeed his theory of the origin of the type depends partly on the correctness of this assumption. But the identification has been the subject of a good deal of dispute; even H. A. Thompson, while putting forward with sober confidence his view that the stoa is both the Stoa of Zeus Eleutherios and the Basileios, admits in the end that ‘an element of uncertainty must persist’. I accept Thompson's view, but certainly not with sufficient confidence to use it as a corner-stone in building up any theory. It is very distracting when one finds that whereas Anti links up his Royal Stoa with oriental palaces, A. Rumpf looks the other way in space and time and regards his Royal Stoa (a building of very different type—the spacious hypostyle hall west of the North-West Stoa and north of the temple of Hephaestus) as the Stammutter of the Roman basilica. ‘They ran away in opposite directions, and vanished to the east and to the west.’ Both of course use the name Basileios to support their identifications. One may perhaps be excused for giving up the riddle for a while and concentrating on the architectural form of the North-West stoa as we undoubtedly have it.


1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls

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.


1955 ◽  
Vol 35 (3-4) ◽  
pp. 187-198 ◽  
Author(s):  
Paul Ashbee

Halangy Down (fig. 1) is the lower precipitous slope of the decline from Telegraph Hill (Ordnance Survey B.M. 166. 3 ft.) to the sea at Halangy Porth and Point. Halangy Down and the earlier chambered tomb upon the crest are often referred to locally as ‘Bants Carn’. The true ‘Bants Carn’ is a considerable rock outcrop dominating Halangy Point. This escarpment faces Crow Sound, which separates the north-west part of St. Mary's from the neighbouring island of Tresco. The hill-side is sheltered by the mass of Telegraph Hill from inclement weather from the north-east and east, but is fully exposed to the south-west and west.The existence of an ancient village site here has long been known in the islands. At the close of the last century, the late Alexander Gibson cleared away the underbrush from one of the more prominent huts and made a photographic record of its construction. Shortly after, the late G. Bonsor, of Mairena del Alcor, near Seville, in addition to excavating the chambered tomb, noted a considerable midden together with traces, of prehistoric occupation exposed in the cliffs of Halangy Porth just below the village site. Dr. H. O'Neill Hencken noted Bonsor's description of the midden, and, as nothing was known at the time of the material culture of the ‘village’, he associated the two.


1887 ◽  
Vol 8 ◽  
pp. 376-400
Author(s):  
W. M. Ramsay ◽  
D. G. Hogarth

In May of the current year, while Professor W. M. Ramsay, accompanied by Mr. H. A. Brown and myself, was travelling in the Tchal district, we were informed at Demirdjikeui of the existence of ruins in or near Badinlar, three hours away to the north. In a previous year Professor Ramsay had paid a hasty visit to this village and seen nothing of importance: on this occasion fortune favoured us: for, visiting the village a day or two later, we were guided on Whit Sunday to the site of a small temple situate on a conical eminence, which fell on the further side to the southern bank of the Maeander, which here enters on one of the narrowest passes of its gorge. Only the platform on which the temple had stood remained in situ, and very few fragments could we find of columns or cornice: such as remained of the frieze showed by their formal regular ornament the Ionic of Roman period. Overlooking the river was a vaulted tomb, and traces of sarcophagi were apparent among the heaps of grey stone covering the summit of the hill.


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