The Mausoleum of Licinnia Flavilla and Flavianus Diogenes of Oinoanda: Epigraphy and Architecture

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.

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.


Antiquity ◽  
2001 ◽  
Vol 75 (289) ◽  
pp. 509-510 ◽  
Author(s):  
Emma Loosley

The Limestone Massif of northwest Syria has the largest concentration of late antique churches in the world. All date from between the second half of the 4th century and the first decade of the 7th century and are remarkably consistent in their conformity to a recognizably ‘Syrian’ architectural style. Almost without exception they are apsed basilicas varying only in terms of size and the quality of decoration.This region was extensively surveyed in the 1950s by Georges Tchalenko, whose monumental three-volume study Villages antiques de la Syrie du nord remains the definitive work on the area. Of the many ecclesiastical buildings included in this survey Tchalenko identified a group of approximately 45 churches possessing a bema. The bema is a horseshoe-shaped structure in the nave that mirrors the curve of the apse. Entered via steps at the east end, it provided benches for the clergy and a pulpit at the west end that was used for scriptural expositions and homilies.


1953 ◽  
Vol 21 ◽  
pp. 42-73 ◽  
Author(s):  
R. G. Goodchild ◽  
J. B. Ward Perkins

During the North African campaigns of 1941–3 numerous air-photographs of the Tripolitanian coast were taken by the R.A.F. for operational purposes, and the site of Lepcis Magna was included in the area covered. Examination of these photographs (pl. XV) showed many suggestive features relating to the defences of the ancient city, and a preliminary ground survey was later (1947–50) undertaken to establish, with a minimum of excavation, the course of the successive wall-circuits.The results of this investigation are described below, and are discussed in relation to the historical and epigraphic evidence. It is not claimed that these results are exhaustive, or that they will not need modification in the light of future discoveries. Since, however, there is little likelihood of any early resumption of large-scale excavations at Lepcis, this preliminary study may help to illustrate the growth and subsequent decline of the city that came to be the most important centre between Carthage and Alexandria.


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.


1990 ◽  
Vol 36 ◽  
pp. 379-418 ◽  

Juda Hirsch Quastel, who contributed for more than 60 years to the growth of biochemistry, was born in Sheffield, in a room over his father’s rented sweet shop on the Ecclesall Road. The date was 2 October 1899, and his parents, Jonas and Flora (Itcovitz) Quastel, had lived in England for only a few years. They had emigrated separately from the city of Tamopol in eastern Galicia, which was then within the Austro-Hungarian Empire; it has since, after a period under Polish rule, become part of the Ukrainian Republic of the Soviet Union. Tamopol at the end of the 19th century was a city of some 30 000 and the centre of an agricultural district. Its inhabitants were ethnically mixed, but about half of them were Jews, many of whom under the relatively benevolent Austrian regime were fairly prosperous. Quastel used to recall how his father and grandfather had held the Emperor Franz Joseph in great respect. His grandfather, also Juda Hirsch (married to Yetta Rappoport), had at one time worked as a chemist in a brewery laboratory in Tamopol. The parents of the subject of this biography had been in commerce there, and were not poor; but today’s family members know little about the life of Jonas and Flora in Tamopol, or about the reasons that persuaded them, like many of their neighbours, to emigrate to the West. An uncle had already gone to England, and perhaps had encouraged them to follow because of the greater opportunities. In England they lived at first in London’s east end, where they worked in garment factories; but their move to Sheffield, and to Jonas’s modest entrepreneurship, had been completed in the late 1890s. It was there that Juda Hirsch and his four younger siblings (Charles, Doris, Hetty and Anne) were born.


1989 ◽  
Vol 69 (1) ◽  
pp. 119-153 ◽  
Author(s):  
Mark Samuel

Excavation and observations from 1984–6 on the Leadenhall Court site in the City of London revealed elements of the fifteenth-century market building known as ‘The Leadenhall’. The truncated foundations were located in various areas of the site; 177 medieval moulded stones were found reused in later cellar walls; and a fragment of the west wall survived to its full height of 11.17m encased between Victorian buildings. The recording and subsequent study of these features, together with a reassessment of such plans and drawings of the building as have survived, established the ground plan of the quadrangle and chapel, and made possible a complete reconstruction of the north range of this important civic building. The methodology used in the reconstructions is described with particular emphasis upon the analysis of the moulded stones. In conclusion, both the design of the structure and the documentary sources are studied to show how it may have been intended to function.The arcaded ground floor functioned as part of a common market, while the upper floors were intended to be a granary. For convenience, however, this dual-purpose building is referred to as the ‘garner’ throughout the text.


1959 ◽  
Vol 91 (4) ◽  
pp. 232-242 ◽  
Author(s):  
C. D. Dondale

Grammonota Emerton, 1882, is one of the many uniform genera that constitute the large and complex family Erigonidae. All of the 28 species and one subspecies recognized by the present writer are American in range, and representatives occur from southwestern Alaska and James Bay in the north to Central America and the West Indies. A few species are arctic-alpine, or are restricted to the Pacific coast, but most occur east of the Rocky Mountains from southern Canada to the Gulf States.


1951 ◽  
Vol 17 (2) ◽  
pp. 142-143 ◽  
Author(s):  
Ripley P. Bullen

The Crystal River site, on the west coast of Florida about 65 miles north of Tampa, presents one of the many unsolved problems of Florida archaeology. Included in the site is a curving shell ridge, shaped like a fishhook with a temple mound where the barb of the hook would be, a large sand or sand and shell burial mound surrounded by a platform to the north, another temple mound further to the north, and a large deposit of shell to the northwest (Moore, 1903, Fig. 16). Obviously, this is a large and complicated site. Practically the only archaeological work done at Crystal River is that of Moore who, during his three visits, dug all the burial mound and part of its surrounding platform (Moore, 1903; 1907; 1918). Moore did no work in the shell midden or temple mounds and our knowledge of the site is limited to its burial complex.


1951 ◽  
Vol 16 (3) ◽  
pp. 257-260 ◽  
Author(s):  
Charles C. Dipeso

The Amerind Foundation, Inc. spent the first three weeks of December, 1948, excavating a ball court at the archaeological site of Arizona:BB:15:3, which is located in Cochise County, Sec. 20, T15S, R20E. The actual village area is located on the west bank of the San Pedro River twenty-two miles north of the city of Benson at an approximate elevation of 3300 feet.The ball court was located in the north half of the village on a terrace some forty feet above the river channel. It appeared as a shallow but conspicuous oval depression which was overgrown with mesquite trees and other desert flora of the Sonoran plateau type. Fortunately the court had not been disturbed by any previous excavations nor by erosion (Fig. 86, a).


Author(s):  
Gregory Vogel

Cavanaugh Mound (3SB3, also known as Etter's Mound, Jones Mound, Site Zeta, and occasionally misspelled Cavenaugh) is a largely intact Late Prehistoric platform mound on the Arkansas River just east of the Oklahoma border, about 14 km from the Spiro Mounds complex. The site is situated on a high terrace above the Arkansas River as it runs between the Ouachita Mountains to the south and the Ozarks to the north. The Poteau River enters the Arkansas River floodplain just west of Cavanaugh, creating one of the widest stretches of bottomland in the region. The area immediately around Cavanaugh Mound is now a residential neighborhood in the city of Fort Smith, and the mound itself is in a tiny lot with a church to the south, a trailer park to the east (named Indian Mounds Trailer Park), and a row of houses to the west. At about 60 m across and 9 m high, Cavanaugh Mound is one of the largest, if not the largest, prehistoric mound in the region. Very little has been published concerning this site, however, and very little formal archeological work has been done there. This article is partly intended to call attention to Cavanaugh Mound, and to compile all reports and descriptions of the mound in one publication. The first part of the article is therefore mostly descriptive. I also offer some tentative interpretations of the site and its possible relationship to the nearby Spiro and Skidgel sites. The size , shape, and stratigraphy of the mound all indicate that it was constructed and used in a manner similar to other Caddoan era platform mounds in the Arkansas River valley. The mound appears to be alone on the landscape, not connected to a group of surrounding mounds and not located within or near a contemporaneous settlement. It overlooks the Poteau/ Arkansas River bottoms to the west and was probably visible from both the Spiro and Skidgel sites in prehistoric times.


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