A Minoan shaft-grave in the bank with Hogarth's Tombs (Knossos Survey 16)

1959 ◽  
Vol 53 ◽  
pp. 283-283
Author(s):  
Sinclair Hood

What seemed to be the covering slabs of a tomb were noticed by the School's foreman, Manoli Markoyiannakis, exposed in the low field bank which forms the southern continuation of the high bank with the Geometric tombs dug by Hogarth and Payne, a couple of metres north of the path running eastwards across the base of the Kefala ridge past the Hellenic tower (BSA 52 (1957) 244ff.). During the course of the School's excavation of the early Christian building on the neighbouring Sanatorium site in 1953 Dr. N. Platon, Ephor of Antiquities for Crete, kindly gave me permission to examine the slabs, which were found to cover a grave roughly rectangular in shape and measuring 1·60 × 0·70 at the bottom (Fig. 1). The grave's floor was only 1·15 at the west end and 1·60 at the east below the modern surface of the rock; but the surface here must have once stood much higher, and have worn away owing to erosion.The three large slabs over the grave were blocks of dressed limestone. That at the east end (A) had a ‘branch’ sign (L. 0·25, max. W. 0·13), boldly carved with broad shallow V-shaped grooves, on the upper exposed face in the north-east corner (Fig. 1, Plate 66d). The joints between the three slabs were carefully wedged with small stones. In the grave below them was a clean fill of kouskouras, the soft white chalky rock of the area, containing a few nondescript Minoan sherds. The cover slabs with the smaller stones wedged in the joints between them seemed to be in place; but the earth below contained small lumps of rock, as if the grave had been deliberately filled before the cover slabs were laid in position. This agrees with what has been observed in the case of other Minoan shaft-graves in the Gypsades cemetery (see p. 219). At the bottom of the grave were the scanty remains of a skeleton, lying on its back with the knees flexed and originally perhaps raised in the usual manner (see p. 218). Although the cover slabs appeared to be in position, and the grave undisturbed, nothing was found with the skeleton. The grave is, however, like other similar shaft-graves at Knossos, presumably Late Minoan, and perhaps early rather than late in the period. The cover slabs may well be old building blocks, and they and the ‘branch’ sign carved on one of them may therefore be considerably earlier than the grave.

1759 ◽  
Vol 51 ◽  
pp. 38-40

About four o’clock on Thursday afternoon, July 13th 1758. a short but severe thunder-storm, with lightning, fell upon the top of an house standing alone, and belonging to a common garden, on the causeway near Sandling's ferry, in the city of Norwich; struck off the tiles of the roof at the east end, to the space of a yard or two 5 burnt a very small hole in the middle of a lath, in piercing into the chamber, and then darted to the north-east; ript off the top of an old chair, without throwing it down; snapt the two heads of the bed-posts, rent the curtains, drove against the wall (the front of the house stands due north-east), forced out an upright of a window frame a yard long, three inches broad, and two thick; smote it in a right line into an opposite ditch, ten or twelve yards distant; then struck down on the wall of the chamber, paring off half a foot s breadth of its plaistered covering quite down to the floor, listed up a board of the floor, and leaving an hole of half an inch diameter, pierced thro’ by the side of the main beam into the kitchen, towards the west end of a pewter- shelf; traversed the whole shelf to the east, and melted superficially to the breadth of a shilling six pewter dishes, two plates, and a pewter bason, all standing touching one another: two of the dishes were thrown down, the rest not displaced.


1876 ◽  
Vol 3 (8) ◽  
pp. 360-361
Author(s):  
T. Mellard Reade

As a contribution to our knowledge of the formation of these very interesting “natural embankments of the sea,” I may point to a little bay in Anglesea, immediately westward of the Bryn Ddu Limestone quarries on the north-east coast of Anglesea, about two miles and a half westward of Puffin Island. This little bay is not more than about a furlong across, and may be roughly described as semicircular in form, lying nearly due west to east from point to point. From being in miniature as it were, the ridge can be readily studied, and it is very striking to see how, commencing in the westward as a beach, it gradually rises into a ridge having very steep sides. No less remarkable is the way in which the stones increase in size as the ridge does in height. At the west end it may be described as composed of Limestone pebbles, with here and there a boulder, while at the east end it is built up almost entirely of large limestone boulders and blocks, many containing from one to two cubic feet and some more. Intermixed there are boulders from the size of the closed hand and upwards. The larger blocks are sub-angular and rounded, and no doubt get gradually worn down smaller and rounder, until they become “boulders.” by being moved about, by the sea; but some on the other hand, being thrown over on to the back of the bank, cannot be further affected by the waves. In this ridge, as I have pointed out is the case with the Chesil Bank, the stones follow the law of the bank itself, the largest being collected to form the highest part of the bank, which in both occurs where the wave-action is most intense.


1973 ◽  
Vol 68 ◽  
pp. 87-101 ◽  
Author(s):  
V. R. Desborough

This cist tomb was uncovered in 1959 during the excavation of the House of Sphinxes,2 and it lay at a distance of only 2 m. from tomb PG 606 (see fig. I and BSA li. 114 fig. 5).It was built on the rock where there was a natural angle and a fairly sharp slope from west to east. The floor of the tomb was in fact for the most part the rock itself, but at the east end a number of small stones, overlying Mycenaean debris, were used. It was of rectangular shape, and orientated W.-E. The west and south walls of the tomb were provided by the rock; two large worked slabs, set upright, formed the north-east corner, and for the rest natural stones were used to line the tomb. There was no evidence of any roofing slabs, nor can one see how such could have been fixed. The inner dimensions were 1·78 × 0·68 m., and the two walling slabs had a height of 0·60 m.


1973 ◽  
Vol 5 ◽  
pp. 4-12 ◽  
Author(s):  
John Humphrey ◽  
Frank Sear ◽  
Michael Vickers

By kind permission of the Department of Antiquities and of Professor Antonino Di Vita, Director of the Italian Mission, and with the financial support of the Society for Libyan Studies, the Oxford Craven Committee and the Cambridge Faculty Board of Classics, the authors spent three weeks in the early summer of 1974 studying the circus at Lepcis Magna. During the sixty years in which Italian archaeologists have been working at Lepcis, parts of the circus have been cleared or excavated on several different occasions. Work was begun in 1924-5 by R. Bartoccini at the monumental arch at the eastern end of the arena and on the seating on the north-east curve. He also uncovered the meta prima and the adjacent east end of the spina. Since 1960 a much larger area has been uncovered successively by E. Vergara-Caffarelli, F. Russo and A. Di Vita, as part of the larger project of clearing and restoring the whole of the amphitheatre-circus complex. Although work in most recent years has concentrated upon the complete clearance and restoration of the amphitheatre (which is cut into the hillside immediately south of the circus), two-thirds of the long south side of the circus has been revealed together with about half of the spina and most of the starting gates (carceres) at the west end.


1964 ◽  
Vol 44 (1) ◽  
pp. 1-8

Early in 1963 much of the land occupied by the Roman building at Fishbourne was purchased by Mr. I. D. Margary, M.A., F.S.A., and was given to the Sussex Archaeological Trust. The Fishbourne Committee of the trust was set up to administer the future of the site. The third season's excavation, carried out at the desire of this committee, was again organized by the Chichester Civic Society.1 About fifty volunteers a day were employed from 24th July to 3rd September. Excavation concentrated upon three main areas; the orchard south of the east wing excavated in 1962, the west end of the north wing, and the west wing. In addition, trial trenches were dug at the north-east and north-west extremities of the building and in the area to the north of the north wing. The work of supervision was carried out by Miss F. Pierce, M.A., Mr. B. Morley, Mr. A. B. Norton, B.A., and Mr. J. P. Wild, B.A. Photography was organized by Mr. D. B. Baker and Mrs. F. A. Cunliffe took charge of the pottery and finds.


1960 ◽  
Vol 26 ◽  
pp. 98-148 ◽  
Author(s):  
John X. W. P. Corcoran

This paper is devoted to a study of the horned-cairns of the North-east of Ireland and their associated artifacts. The term ‘horned-cairn’ is used to describe those segmented gallery-graves set in a long cairn and entered from a semi-circular forecourt delimited by an orthostatic facade. It is realized that this term is not altogether satisfactory, but it has the virtue of brevity and its usage is now well established. Some contemporary Irish prehistorians, notably Professor Ruaidhrí de Valéra, have suggested the term ‘court-cairn’ for all the manifestations in Ireland of the segmented gallery-grave having elaborate structural forecourts. This would include cairns in the West of Ireland with completely enclosed courts (described as court-cairns in this paper) as well as horned-cairns proper. The confusion which might arise from the use of such terms as ‘full court-cairn’, ‘half court-cairn’, ‘forecourt-cairn’ and the like have decided the present writer to retain in this paper the simple terms ‘horned-cairn’ and ‘court-cairn’.This study is divided into two main sections. The first is descriptive, being concerned with horned-cairns and associated artifacts and the second attempts to place the Carlingford Culture as a whole in its context in prehistory. In view of the paucity of detailed information about court-cairns, particularly the almost complete lack of excavation, no detailed study is made of these. At the time of going to press it is understood that a paper by Professor de Valéra on the court-cairns of the west is about to be published in the Proceedings of the Royal Irish Academy.


Author(s):  
A. Volodin

The present article focuses on the entity of middle classes in non-Western societies. The social formation of this kind is a relatively new phenomenon. As far as the modern Western societies are concerned, the social and political “materialization” of the above-mentioned entity has covered the period of no less than five centuries. The middle class in modern transitional societies began to emerge quite recently, with a few notable exceptions, after gaining sovereignty. That is one of the reasons why political systems in the non-Western world are mostly fragile and susceptible to instability of different kinds and origins. The so called “Arab awakening” gives a vivid example for the “underdevelopment” of indigenous middle classes. Whilst in the advanced industrial societies middle classes were (and are) the building blocks of social structure, economic and political development, elite recruitment, etc., among the non-Western societies (with the salient exception of the North-East Asia) the process of the middle class institutionalization as well as its economic and political self-assertion is still under way, somewhere at the initial stage of development. Comparing various non-Western societies from the middle class inner dynamics as well as self-assertion perspective, the author concludes that in the ultimate analysis, the maturity of this process is dependent on the pro-active and creative role of the State. The latter serves as the main driving force of the middle class consolidation and the instrument of political and economic systems for increasing and advancing development. The cases of India, on one hand, and Indonesia, on the other, demonstrate convincingly that the State remains the leading institution of the society able to accelerate economic growth and development, but also to stimulate the emergence and socio-political assertion of the middle class in contemporary non-Western world.


Author(s):  
Penelope M. Allison

The surviving plaster on the walls of this entranceway consisted of a high pink socle, delineated in red, with a white zone above. Ling observed that this overlay an earlier First-Style decoration on the east wall and that it had been patched in antiquity. Breaches are found in both the east and west walls. Outside the entrance, to either side, is a masonry bench (east bench: l.: 2.1 m, d.: 380 mm; west bench: l.: 2.4 m, d.: 460 mm), both much damaged. Finds within the entranceway consisted of bronze and iron studs, undoubtedly from the house door. Remains of plastered decoration survive on the south wall. Elia recorded a yellow dado, surmounted by a red band, with white plaster above. There is a breach in the north-west corner through to Unit no. 9, above a blocked doorway. At the centre of this front hall is a tufa impluvium (2.4 m × 2.1 m). In the north-west corner, 1 m above the pavement, were found: a small bronze ring; a bronze stud, similar to those in the entranceway and probably also from the front door; a fragment of a stone mortar or hand-mill; some glass beads; a small shell; and two bronze quadrantes, one of Nero dated ad 64. The fragmentary or loseable nature of these items suggests that they were disturbed from the ground level. Other small loseable items were found in the north-east corner: a small glass bottle, probably a toilet item; and possibly five more coins. One metre from the west side of the impluvium were found: another part of a hand-mill; two large stone weights; at least fifty-three lead weights, probably from a loom; and two other spherical stones, possibly also weights. The large number of lead weights is comparable with the quantity found under the stairway in room i of the Casa del Principe di Napoli. Another comparable group of forty loom weights was found together in a pit at Zugmantel. As Jongman noted, this amount would be equivalent to that required for one or perhaps two warp-weighted looms. It is therefore commensurate with the existence of such a loom, or looms, in this area, or of replacement loom weights, for domestic use.


Author(s):  
Penelope M. Allison

In November 1926 the excavators recorded moving lapilli from in front of this house and from the entrance but no finds were reported in these areas. On 8 July 1932 they recorded removing disturbed volcanic deposit from the middle levels in the northeast area of this insula. A breach (min. h.: 2 m), now patched, in the south end of the west wall of room 2 and 1.05 m above the floor, presumably penetrated into this space and documents disturbance after ad 79. Elia observed that the room had been covered and had been divided for all or part of its length by a ‘tramezzo ligneo’ which Ling interprets as a wooden partition to screen the stairway. In the north-east corner, are three masonry steps from a stairway which Ling argued ascended along the east wall. Ling argues that the installation of this stairway would have put out of commission the recess and lararium painting (dimensions: 0.55 m × 0.4 m) behind it. The remains of a late Third Style decoration are found on the walls. The loose finds from near the north entrance of this space and from near the entrance to room 3 were predominantly door-fittings, with the possible exception of a small marble base. A small key reported in the latter location may originally have been from storage furniture but was unlikely to have been in use as no other remains of such furnishings were recorded. The only other find in this area was a glass vessel of unknown type. Elia called this room an ‘atrium’. The finds are not particularly diagnostic but, even if this area was disturbed, they hint that it had been relatively unencumbered with furnishings, probably serving predominantly as a reception and access area for the rest of the house. The breach in the south end of the west wall of this room implies that it may have been disturbed after ad 79. The walls had a simple painted decoration but this room had no evident fixtures. According to Elia it was an ‘oecus’. The limited ceramic finds (a jug, a terra sigillata dish, and a lamp) are associated with lighting and probably with the serving or storage of foodstuffs.


1906 ◽  
Vol 41 (1) ◽  
pp. 53-87
Author(s):  
T. J. Jehu

The area embraced in this paper consists of that part of Pembrokeshire which lies to the north and north-east of St Bride's Bay. Bounded on the west by St George's Channel and on the north by Cardigan Bay, it extends to the north-east as far as the mouth of the river Teifi, near Cardigan.That part of the country which lies in the immediate neighbourhood of St David's has, through the laborious researches of the late Dr Hicks and others, become well-known to geologists, and may now be regarded as classic ground. The solid geology of this promontory has given rise to much discussion, and has, perhaps, attracted more attention than that of any other part of the Principality. The reason for this great interest is to be sought in the facts that the rocks of this area are of a very great antiquity, and that the sedimentary series contain the remains of some of the earliest organic forms yet found in the earth's crust, whilst the igneous rocks are also displayed in great abundance and variety, and present us, in the words of Sir Archibald Geikie, with “the oldest well-preserved record of volcanic action in Britain.”


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