Inscriptions from South Etruria

1966 ◽  
Vol 34 ◽  
pp. 56-67
Author(s):  
J. M. Reynolds

The following group of inscriptions includes some unpublished texts found recently during the South Etruria survey and a few published ones in which additional or improved readings can be offered as a result of re-examination. Most of them are tombstones of essentially local significance, but nos. 1 and 4 from Tomba di Nerone, 5 from Casale Spizzichino and 20 from Filissano are of greater importance and interest.I. Sites on or near the Via Cassia.1. Travertine tombstone, damaged at the upper right corner (0·52 × 0·98 × 0·12), with schematic gable and acroteria above and a lightly and crudely incised wreath in the gable; inscribed on the exposed face, whose surface is damaged. Built into the wall of the drive leading to Via Cassia 901, which lies on the west side of the road a short distance beyond Tomba di Nerone. Recent building development revealed drainage cuniculi and other elements of a Roman building, and along the ancient road frontage there were several graves and remains of at least one mausoleum. It is very likely that some or all of the texts (nos. 1–4) were found locally.

Antiquity ◽  
1929 ◽  
Vol 3 (9) ◽  
pp. 49-59 ◽  
Author(s):  
O. G. S. Crawford

Probably not one in ten thousand of those who pass through the middle of Durrington Walls is aware of its existence. Though plainly visible when once pointed out, the earthen ramparts have been so greatly altered by ploughing as to be hardly recognizable, and the reconstruction of their orginal form is a very pretty exercise in field-archaeologyThe walls consists of a round enclosure, cut into two unequal parts by the road from Amesbury to Netheravon (Wilts), about a mile and a half north of Amesbury, on the west bank of the Avon. Woodhenge is only eighty yards to the south, close to and on the west side of the same road. The earthwork differs fundamentally from the ordinary defensive ‘camp’, for it encloses, not a hill-top but a coombe or hollow, and it has its ditch inside, not outside, the rampart. In this latter respect it resembles the circles at Avebury and Marden in Wilts, Knowlton in Dorset, Thornborough in Yorkshire, and Arbour Low in Derbyshire; though there are points of difference. In size, Durrington Walls compares closely with Avebury, whose great earthen circle is slightly smaller in diameter; rom east to west the internal area of the Walls is 1300feet across, and from north to south about 1160 feet. (The average diameter at Avebury is 1130 feet). Both too are within easy reach of a stream, the Avon being IOO yards from the eastern entrance of the Walls, and the Kennet 330 yards from the nearest point of the great circle at Avebury. The enclosure at Marden actually touches the banks of the Avon at a point higher up in its course.


1924 ◽  
Vol 61 (11) ◽  
pp. 513-515 ◽  
Author(s):  
Sidney Melmore

A Small quarry was opened about three years ago at Thwaite Head, which lies between the southern ends of Coniston Lake and Windermere. It is on the west side of the road between that hamlet and Hawkshead, and exposes a nearly vertical sill, 40 feet wide, running E.N.E.-W.S.W. in the Bannisdale slates. On the south side a series of joint-planes running parallel to the bedding of the slates and curving inwards at the top have split the igneous rock into flags, while in the body of the rock the jointing is much coarser, so that it is quarried in large blocks. Both the igneous rock and the slates are much decomposed and friable along the southern junction, and it is here a little galena is said to have been found when the quarry was first opened. This is not improbable, as the old Thwaite Head lead mine is situated not far off on the banks of Dale Park Beck.


Archaeologia ◽  
1932 ◽  
Vol 82 ◽  
pp. 3-18
Author(s):  
A.J.B. Wace

In 1899 during his excavations Tsountas found three rock-cut chamber tombs (Tomb 102, the Fig Tree Tomb, and another, fig. 1) on the west side of the carriage road just to the south of the Treasury of Atreus. In 1904 Bosanquet published the goldwork and other small objects from Tomb 102, together with one of the vases. It is to be hoped that Tsountas will soon be able to publish the rest of the pottery of that tomb and the contents of the others. In 1921 we made trial trenches on the slopes on both sides of the road, and found three similar rock-cut chamber tombs, the positions of which are shown on the accompanying sketch plan, fig. 1. As these tombs lie on either side of the third kilometre stone of the road, we have for the sake of convenience called this the Third Kilometre Cemetery to distinguish it from the other groups of tombs that surround Mycenae. Tombs 502 and 504 were both excavated in 1921; Tomb 505 was begun in 1921 but, owing to difficulties caused by the dangerous state of the doorway, the chamber was not completely cleared till 1922.


1963 ◽  
Vol 29 ◽  
pp. 99-132 ◽  
Author(s):  
G. J. Wainwright

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.


1938 ◽  
Vol 18 (1) ◽  
pp. 68-74 ◽  
Author(s):  
Philip Corder ◽  
I. A. Richmond

The Roman Ermine Street, having crossed the Humber on the way to York from Lincoln, leaves Brough Haven on its west side, and the little town of Petuaria to the east. For the first half-mile northwards from the Haven its course is not certainly known: then, followed by the modern road, it runs northwards through South Cave towards Market Weighton. In the area thus traversed by the Roman road burials of the Roman age have already been noted in sufficient quantity to suggest an extensive cemetery. The interment which is the subject of the present note was found on 10th October 1936, when men laying pipes at right angles to the modern road, in the carriage-drive of Mr. J. G. Southam, having cut through some 4 ft. of blown sand, came upon a mass of mixed Roman pottery, dating from the late first to the fourth century A.D. Bones of pig, dog, sheep, and ox were also represented. Presently, at a depth of about 5 ft., something attracted closer attention. A layer of thin limestone slabs was found, covering two human skeletons, one lying a few feet from the west margin of the modern road, the other parallel with the road and some 8 ft. from its edge. The objects described below were found with the second skeleton, and the first to be discovered was submitted by Mr. Southam to Mr. T. Sheppard, F.S.A.Scot., Director of the Hull Museums, who visited the site with his staff. All that can be recorded of the circumstances of the discovery is contained in the observations then made, under difficult conditions. ‘Slabs of hard limestone’, it was reported, ‘taken from a local quarry of millepore oolite and forming the original Roman road, were distinctly visible beneath the present roadway—one of the few points where the precise site of the old road has been located. On the side of this… a burial-place has been constructed. What it was like originally it is difficult to say, beyond that a layer of thin … slabs of limestone occurred over the skeletons. This had probably been kept in place or supported by some structure of wood, as several large iron nails, some bent at right angles, were among the bones.’ If this were all that could be said about the burials, they would hardly merit a place in these pages. The chief interest of the record would be its apparent identification of the exact course of the Roman road at a point where this had hitherto been uncertain. Three objects associated with the second skeleton are, however, of exceptional interest.


1953 ◽  
Vol 33 (1-2) ◽  
pp. 22-32 ◽  
Author(s):  
Graham Webster ◽  
R. H. Dolley ◽  
G. C. Dunning

On 29th November 1950 workmen employed by the Merseyside and North Wales Electricity Board were relaying a cable on the west side of Castle Esplanade, Chester. In cleaning up the western side of the trench with a spade, 18 in. below the present pavement level and 29 ft. to the south of St. Martin's Court, one of the men cut through a small earthenware vessel and a shower of coins and silver bullion poured into the bottom of the trench. It is distressing to record that although the Grosvenor Museum is only 100 yards from the site, the discovery was not reported. No significance was attached to the find; one of the men stated later that they thought they were milk checks. Three of the men put handfuls of coins into their pockets; others were distributed to children near, and the rest shovelled back into the trench. The engineer-in-charge took several to his office for thepurpose of identification, but later forgot about them. One of the men sent some of the coins to Hunter Street Girls' School, by his niece, for identification, and the mistress immediately sent them to the Curator of the Grosvenor Museum.This happened on 10th December, and the Curator at once appreciating the significance of the discovery, set to work to recover as much as possible of the hoard, and reported the matter to the City Coroner. As a result he recovered a hundred coins, twelve ingots of silver, and a fragment of the vessel.


1969 ◽  
Vol 19 ◽  
pp. 139-142 ◽  
Author(s):  
Theodora S. Mackay ◽  
Pierre A. Mackay

The following random lot of inscriptions was noted during three brief trips into the territory around Olba-Diocaesareia, in the spring of 1966, while we were guests at the British Institute of Archaeology at Ankara. These trips were part of a year of archaeological wandering made possible by the grant of the Olivia James Travelling Fellowship, administered by the Archaeological Institute of America.1. Seleuceia-Korykos: This inscription was discovered by the able and energetic curator of antiquities at Silifke, Mr. Mehmet Belen, to whose great kindness we owe our knowledge of it. It is cut on a rock face above some faint traces of an ancient road from Korasion to Korykos, which runs parallel to the modern coast road at this point. About 19 km. east of Silifke, the modern road turns north away from the shore, and runs inland along the west side of a seasonal watercourse called Kuru Dere, “dry river bed”. Just north of the gravel bank at the mouth of Kuru Dere, at a point where the rock wall cuts back from the west side of the road to form a very small tributary stream bed, there are faint traces of rock cut steps some 5 metres above the road. Above these, on the south side of the tributary stream bed, a roughly dressed rectangular panel, 0·80 × 0·45 m., has been cut into the rock.


1953 ◽  
Vol 8 (22) ◽  
pp. 444-457
Keyword(s):  
The West ◽  

Charles Edward Inglis was the second surviving son of Dr Alexander Inglis, M.D., M.R.C.S.E., of Auchindinny and Redhall, and of his first wife, Florence, the second daughter of John Frederick Feeney, proprietor of the Birmingham Daily Post, whose family founded the Feeney Art Gallery in that city. The Inglis family of Auchindinny appear first as tenants and afterwards owners of the farm of Langbyres, which adjoins the west side of Murdostoun in the parish of Shotts, Lanarkshire. The first mention of them in connexion with the place is found in the Lord High Treasurer’s accounts for 1543 when John Inglis in Langbyres and James Kneland in Swyntre had to pay £13 6s. 8d. to redeem their movable goods, which had been escheated as a penalty for their absence from the army, mustered by James V to invade England, which was routed at Solway Moss. The estate of Auchindinny, about 730 acres, was purchased in 1702 by one John Inglis, a Writer to the Signet, who had succeeded to Langbyres in 1685. Auchindinny lies about eight miles south of Edinburgh, on the right bank of the North Esk and at the south end of the parish of Lasswade. The house, completed in 1707, is a severe substantial sandstone building. John Inglis had eleven children. One of his grand-daughters, Barbara, co-heiress of Archibald, Laird of Auchindinny, married in 1777 her cousin, Captain, afterwards Admiral, John Inglis, R.N., of Redhall, whose father had left Scotland and settled in Philadelphia as a merchant about 1736. Captain Inglis commanded H.M.S. Belliqueux at the battle of Camperdown. The ship took a conspicuous share in the fighting, there being a hundred and three casualties out of a complement of four hundred and ninety-one, and quite redeemed the character which she had lost in the Mutiny at the Nore a few months earlier. It is said that the Captain was puzzled in the battle by his Admiral’s frequent signals and at last threw his signal book on deck exclaiming, ‘Damn the signals; up wi’ the hellem and gang into the middle o’ it’. He thus anticipated Nelson’s celebrated memorandum that ‘when a captain should be at a loss he cannot do very wrong if he lay his ship alongside of the enemy’.


1913 ◽  
Vol 10 (5) ◽  
pp. 205-215 ◽  
Author(s):  
A. R. Horwood

Although the Rhætic beds are not exposed continuously along the eastern boundary of the Keuper outcrop, they have been proved at many points from the River Trent in the north on the Nottinghamshire border to Glen Parva in the south. South of this point there is so much drift, and borings within the Liassic outcrop have been so isolated or shallow, that there is a gap in our knowledge of the intervening ground between the last point and the Rugby district. The Countesthorpe boring, carried to a depth of over 600 feet, encountered Upper Keuper beneath the Drift, with no intervening Rhætics. Commencing in the north in the Gotham district the two outliers are capped above the Red Marl and Tea-green Marl with Rhætic beds, and Lower Lias Limestone (Ps. planorbe zone) above. At Ash Spinney at the south end of the southern outlier, and at the east end of Crownend Wood, Black Shales with Avicula contorta crop out; and on the west side septaria are seen. On the north-west side of the northern outlier at Cottager's Hill Protocardium phillipianum has been found in a well-section near the lane. Rhætic shales are seen in the shafts driven for gypsum works about Gotham.


1967 ◽  
Vol 62 ◽  
pp. 353-371
Author(s):  
J. J. Coulton

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.


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