scholarly journals VII. An account of a storm of thunder and lightning at Norwich, on the 13th of July 1758

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.


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.


2014 ◽  
Vol 109 ◽  
pp. 357-378
Author(s):  
Chrysanthos Kanellopoulos ◽  
Eleni Zavvou

The Roman ‘Agora’ of Gytheum appears to be a large compound with an interior peristyle; its width is 52 m and its length at least 61 m. Excavations have revealed the remains of the north-east corner and a portion of the west wing. The extant architectural blocks allow the reconstruction of the colonnades. Column shafts were made of local red limestone and at least some of them were crowned with lotus-and-acanthus capitals. Three different interaxial column spacings are present. A single column must have stood on each corner of the peristyle. The style of the column capital suggests a date after the yearad100. The entablature is almost identical, in both style and dimensions, to the one found on the Captives' Facade at Corinth. The inscription on two epistyles reveals the private dedication of an exedra totheoi Sebastoiand the city. Most probably the exedra was behind the colonnaded space; the mention oftheoi Sebastoimight suggest imperial cult either in the exedra alone or both in the exedra and in the entire colonnaded compound. Quite possibly, and following A. Themos' suggestion, a large part of the colonnaded compound that is conventionally termed the ‘Agora’ can be identified with the Sebasteum/Caesareum of Gytheum; this latter structure is attested in other inscriptions from the city.


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.


1996 ◽  
Vol 46 ◽  
pp. 111-144 ◽  
Author(s):  
A. S. Hall ◽  
N. P. Milner ◽  
J. J. Coulton

Among the many tombs still to be seen in the necropolis surrounding the site of Oinoanda, in northern Lycia, the mausoleum built by Licinnia Flavilla for her parents and ancestors enjoys a special distinction, which it owes both to its size and to the vast genealogical inscription, comprising twelve generations of the ancestors and connexions of Licinnia Flavilla and her younger kinsman Flavianus Diogenes, which once covered its eastern façade. The aim of this paper is to present new epigraphic evidence which indicates a second major genealogical inscription on the west end of the mausoleum, and to consider the relation of the inscriptions to the underlying building, to each other, and to the aims of Licinnia Flavilla and her kinsman Diogenes.The mausoleum of the Licinnii lies in rubble (Pl. XV (a)) amid a group of smaller tombs at the southern end of the site, in square Lr of the B.I.A.A.'s site-plan (AnSt XLV (1995) 74, Fig. 1) about 40 m. below an isolated stretch of the Hellenistic southern wall overlooking the saddle at the southern end of the ridge on which stand the main buildings of the city. There is an easy ascent to this point from both the western and eastern sides of the ridge, and thence to the city; the mausoleum will have been conspicuous to visitors and travellers. Since antiquity all the tombs in this area have been plundered or overthrown, especially close to the wall. Three types of tomb are visible: rock-cut tombs, some with lion covers; large, free-standing sarcophagi of various designs; and sarcophagi on high, stepped platforms. An example of this last type (Pl. XV (b)) stands close by the east end of the mausoleum, a few metres to the north.


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.


Antiquity ◽  
1976 ◽  
Vol 50 (200) ◽  
pp. 216-222
Author(s):  
Beatrice De Cardi

Ras a1 Khaimah is the most northerly of the seven states comprising the United Arab Emirates and its Ruler, H. H. Sheikh Saqr bin Mohammad al-Qasimi, is keenly interested in the history of the state and its people. Survey carried out there jointly with Dr D. B. Doe in 1968 had focused attention on the site of JuIfar which lies just north of the present town of Ras a1 Khaimah (de Cardi, 1971, 230-2). Julfar was in existence in Abbasid times and its importance as an entrep6t during the sixteenth and seventeenth centuries-the Portuguese Period-is reflected by the quantity and variety of imported wares to be found among the ruins of the city. Most of the sites discovered during the survey dated from that period but a group of cairns near Ghalilah and some long gabled graves in the Shimal area to the north-east of the date-groves behind Ras a1 Khaimah (map, FIG. I) clearly represented a more distant past.


Author(s):  
Sergey B. Kuklev ◽  
Vladimir A. Silkin ◽  
Valeriy K. Chasovnikov ◽  
Andrey G. Zatsepin ◽  
Larisa A. Pautova ◽  
...  

On June 7, 2018, a sub-mesoscale anticyclonic eddy induced by the wind (north-east) was registered on the shelf in the area of the city of Gelendzhik. With the help of field multidisciplinary expedition ship surveys, it was shown that this eddy exists in the layer above the seasonal thermocline. At the periphery of the eddy weak variability of hydrochemical parameters and quantitative indicators of phytoplankton were recorded. The result of the formation of such eddy structure was a shift in the structure of phytoplankton – the annual observed coccolithophores bloom was not registered.


2020 ◽  
Vol 8 (2) ◽  
pp. 13
Author(s):  
Ankita Pandey

Guwahati derives its name from the Assamese word “Guwa” means areca nut and “Haat” means market. However, the modern Guwahati had been known as the ancient Pragjyotishpura and was the capital of Assam under the Kamrupa kingdom. A beautiful city Guwahati is situated on the south bank of the river Bramhaputra. Moreover, It is known as the largest city in the Indian state of Assam and also the largest metropolis in North East India. It has also its importance as the gateway to the North- East India. Assamese and English are the spoken languages in Guwahati.  In 1667, the Mogul forces were defeated in the battle by the Ahom forces commanded by Lachut Barphukan. Thus, in a sense Guwahati became the bone of contention among the Ahoms, Kochas and the Moguls during the medieval period.  Guwahati the administrative headquarters of Lower Assam with a viceroy or Barbhukan was made by the Ahom king.  Since 1972 it has been the capital of Assam. The present paper will discuss the changes happened in Guwahati over the period of late 1970s till the present time. It will focus on the behavior of people, transformed temples, Panbazar of the city, river bank of Bramhaputra, old Fancy Bazaar, chaotic ways, festivals and seasons including a fifth man made season etc. It will also deal how over the years a city endowed with nature’s gifts and scenic views, has been changing as “a dirty city”. Furthermore, it will also present the insurgencies that have barged into the city. The occurrence of changes will be discussed through the perspective and point of view of Srutimala Duara as presented in her book Mindprints of Guwahati.


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.


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