A Road Trip with Strabo

Mnemosyne ◽  
2016 ◽  
Vol 69 (2) ◽  
pp. 202-225
Author(s):  
Sarah Pothecary

A number of places that feature in Strabo’s description of the Asian peninsula were situated on the ancient road that ran between the Euphrates river and the city of Ephesus. It is likely that Strabo journeyed along the entire thousand-kilometre length of the road, even though he makes explicit reference to his presence in only a few locations. He most probably made the journey as a youth on his way to Roman Asia, in the south west of the peninsula, from Pontus in the north. Decades pass before Strabo, as an old man, writes the Geography and includes in it the memories of places he had visited. The outdated tone of some of his descriptions reflects this passage of time.

Author(s):  
Roger Ling ◽  
Lesley Ling

We take the opportunity of modifying ideas presented in Volume I, and responding to queries raised by reviewers and other commentators. 1. Street fountains. It was claimed in Volume I (p. 252) that the cutting back of the fac¸ade of I.10.1 to create space round the fountain was almost without parallel in the city: the only other places where we could point to similar sacrifices being made, either for fountains or for the distribution tanks and watertowers which were an integral part of the distribution system provided to feed them, were at the southern tip of Insula VI.1 and the south-east corner of VI.14. We suggested, therefore, that the owner or occupier of I.10.1, rather than being subject to an expropriation order, may have yielded the space voluntarily. It is certainly true that street fountains and water-towers were as far as possible sited to avoid impinging upon existing buildings, even though the installations in question almost invariably ended up both encroaching upon the sidewalk and projecting into the carriageway. In some cases, as at the northeast corner of VI.8, there was no great problem, because there was suficient space for pedestrians and wheeled trafic to get past without dificulty. In other places, the street was closed to vehicles, so the fountain could project freely into the carriageway or even stand wholly within it: such was the case at the north-west corner of VI.13, where the lack of ruts and a strategically placed bollard at the south end conform that the Vico del Labirinto was for pedestrians only. The western stretch of the Via dell’Abbondanza, between the forum and the Via Stabiana crossing, was at least partially closed to vehicles, but there was, in any case, no shortage of space for the fountains at the south-east corners of VII.9 and VII.14. At the north end of the Via delle Scuole, closed off by the forum colonnade, it was even possible to site a fountain in the middle of the road. In other cases, however, accommodating the fountain presented serious difficulties. At the south-east corner of VII.4, for instance, the fountain jutted into the street so far as to leave only a narrow gap for wheeled trafic to squeeze through, and ultimately the street was closed.


1932 ◽  
Vol 1 (3) ◽  
pp. 158-162
Author(s):  
J. J. R. Bridge

In the first number of Greece and Rome Mr. Symonds reminded us that the bearing of art and archaeology on literature can be studied by visits to sites and museums, and suggested that ‘even a holiday expedition to the Roman Wall is not beyond the bounds of ambition’. Indeed, once Newcastle or Carlisle is reached the motor-car has made a trip to the Wall a simple matter. A cursory visit starting from Newcastle takes but a few hours. A twenty-mile drive over the West Turnpike, Wade's Road as it is popularly called, along the line of the Wall with the earthworks visible for most of the way and a fragment of the Wall itself to be seen not far from the city boundary, brings us to Chesters. Here is the camp, or more properly fort, of Cilurnum, the fort baths, the bridge abutment, and the museum. After Chesters we travel a further ten miles. A substantial length of the Wall is soon seen on the right, while the earthworks line both sides of the road for most of the way, and at Limestone Bank are cut through solid rock. Then with less than half a mile's walk across the fields we come to Housesteads. Here we can see the fort of Borcovicium (or Borcovicus), and then walk a few hundred yards to the west to see a milecastle and get the well-known view of the Wall at Cuddy's Crag. If the start is from Carlisle the mileage is more, Housesteads being about half-way to Newcastle but Chesters ten miles farther east. If we come from the south by road we may leave the North Road at Durham and travelling by Lanchester, Consett, and Corbridge (Corstopitum), join the West Turnpike at Portgate where the Roman Road of the first of the Antonine Itineraries passed through the Wall on its way to the Cheviots and Scotland: or we may turn off earlier and make for Teesdale and Alston, to join the West Turnpike three miles north of Haltwhistle.


1953 ◽  
Vol 21 ◽  
pp. 32-41 ◽  
Author(s):  
J. G. Baldacchino ◽  
T. J. Dunbabin

On the 22nd September, 1950, whilst workmen were digging a trench for the laying of a water main at Ghajn Qajjet, near Rabat, Malta (Malta 2″ Map. Ref. 356247) at a depth of 2 ft. 8 in. below the surface of the road, the burial chamber of a rock-cut tomb was broken into (fig. 1).This chamber (fig. 2), rectangular in plan and with a flat ceiling, measured 12 ft. in length, 10 ft. in width, and 5 ft. 7 in. in height; its long axis ran in a north-easterly direction. A slab of Globigerina limestone (pl. XII), 6 ft. 5 in. long, 5 ft. 8 in. wide, and 5 in. thick, rested horizontally on the floor and was set with two of its sides in contact with the north-east and the south-east walls; owing to the slight inclination of the floor, being higher towards the north-east, it was propped up by roughly dressed small blocks of stone. There was also a cavity, 10 in. in diameter and 6 in. deep, cut in the floor at a distance of 4 in. from the south-west side of the stone slab and quite close to the south-east wall of the chamber.


1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.


1985 ◽  
Vol 35 ◽  
pp. 93-97 ◽  
Author(s):  
Stephen Hill

The ruins at Yanıkhan form the remains of a Late Roman village in the interior of Rough Cilicia some 8 kilometres inland from the village of Limonlu on the road to Canbazlı (see Fig. 1). The site has not been frequently visited by scholars, and the first certain reference to its existence was made by the late Professor Michael Gough after his visit on 2 September 1959. Yanıkhan is now occupied only by the Yürüks who for years have wintered on the southern slopes of Sandal Dağ. The ancient settlement at Yanıkhan consisted of a village covering several acres. The remains are still extensive, and some, especially the North Basilica, are very well preserved, but there has been considerable disturbance in recent years as stone and rubble have been removed in order to create small arable clearings. The visible remains include many domestic buildings constructed both from polygonal masonry without mortar and from mortar and rubble with coursed smallstone facing. There are several underground cisterns and a range of olive presses. The countryside around the settlement has been terraced for agricultural purposes in antiquity, and is, like the settlement itself, densely covered with scrub oak and wild olive trees. The most impressive remains are those of the two basilical churches which are of little artistic pretension, but considerable architectural interest. The inscription which forms the substance of this article was found on the lintel block of the main west entrance of the South Basilica.


1927 ◽  
Vol 7 (4) ◽  
pp. 438-464 ◽  
Author(s):  
E. Thurlow Leeds

At the end of April of last year the Rev. Charles Overy drew my attention to the presence of broken animal bones, flints, and sherds of pottery in a gravel-pit on the south side of the road from Abingdon to Radley, about a mile out of Abingdon (fig. 1).The pit lies on the very boundary of the parish of Abingdon in a field at about 200 ft. O.D., just over half a mile north of the Thames and some 30 ft. above the river. On its eastern and southern sides it is bounded by the wide trenches which in the days of the splendour of Abingdon Abbey formed part of the Abbey's fish-ponds ; on the north is the road, and on the east the ground drops to a little brook.


1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.


1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace

The Cyclopean Terrace Building lies to the north-west of the Lion Gate on the northern end of the Panagia Ridge and faces almost due west across the valley of the Kephissos and modern main road from Corinth to Argos. It lies just below the 200 m. contour line, and one terrace below the houses excavated in 1950–51 by Dr. Papadimitriou and Mr. Petsas to the east at the same end of the ridge. The area contains a complex of buildings, both successive and contemporary, and in view of the discovery of structures both to the south-west and, by the Greek Archaeological Service, to the north-east it is likely that this whole slope was covered by a portion of the outer town of Mycenae. This report will deal only with the structure to which the name Cyclopean Terrace Building was originally given, the so-called ‘North Megaron’, supported by the heavy main terrace wall.The excavation of this structure was begun in 1923. The main terrace wall was cleared and two L.H. IIIC burials discovered in the top of the fill in the south room. In 1950 it was decided to attempt to clear this building entirely in an endeavour to find out its date and purpose. The clearing was not, however, substantially completed until the close of the 1953 excavation season, and this report presents the available evidence for the date as determined by the pottery found beneath the building; the purpose is still a matter for study, though various tentative conclusions can be put forward.


Starinar ◽  
2013 ◽  
pp. 269-286
Author(s):  
Perica Spehar ◽  
Natasa Miladinovic-Radmilovic ◽  
Sonja Stamenkovic

In 2012, in the village Davidovac situated in south Serbia, 9.5 km south-west from Vranje, archaeological investigations were conducted on the site Crkviste. The remains of the smaller bronze-age settlement were discovered, above which a late antique horizon was later formed. Apart from modest remains of a bronze-age house and pits, a late antique necropolis was also excavated, of which two vaulted tombs and nine graves were inspected during this campaign. During the excavation of the northern sector of the site Davidovac-Crkviste the north-eastern periphery of the necropolis is detected. Graves 1-3, 5 and 6 are situated on the north?eastern borderline of necropolis, while the position of the tombs and the remaining four graves (4, 7-9) in their vicinity point that the necropolis was further spreading to the west and to the south?west, occupying the mount on which the church of St. George and modern graveyard are situated nowadays. All graves are oriented in the direction SW-NE, with the deviance between 3? and 17?, in four cases toward the south and in seven cases toward the north, while the largest part of those deviations is between 3? and 8?. Few small finds from the layer above the graves can in some way enable the determination of their dating. Those are two roman coins, one from the reign of emperor Valens (364-378), as well as the fibula of the type Viminacium-Novae which is chronologically tied to a longer period from the middle of the 5th to the middle of the 6th century, although there are some geographically close analogies dated to the end of the 4th or the beginning of the 5th century. Analogies for the tombs from Davidovac can be found on numerous sites, like in Sirmium as well as in Macvanska Mitrovica, where they are dated to the 4th-5th century. Similar situation was detected in Viminacium, former capital of the roman province of Upper Moesia. In ancient Naissus, on the site of Jagodin Mala, simple rectangular tombs were distributed in rows, while the complex painted tombs with Christian motifs were also found and dated by the coins to the period from the 4th to the 6th century. Also, in Kolovrat near Prijepolje simple vaulted tombs with walled dromos were excavated. During the excavations on the nearby site Davidovac-Gradiste, 39 graves of type Mala Kopasnica-Sase dated to the 2nd-3rd century were found, as well as 67 cist graves, which were dated by the coins of Constantius II, jewellery and buckles to the second half of the 4th or the first half of the 5th century. Based on all above mentioned it can be concluded that during the period from the 2nd to the 6th century in this area existed a roman and late antique settlement and several necropolises, formed along an important ancient road Via militaris, traced at the length of over 130 m in the direction NE-SW. Data gained with the anthropological analyses of 10 skeletons from the site Davidovac-Crkviste don't give enough information for a conclusion about the paleo-demographical structure of the population that lived here during late antiquity. Important results about the paleo-pathological changes, which do not occur often on archaeological sites, as well as the clearer picture about this population in total, will be acquired after the osteological material from the site Davidovac-Gradiste is statistically analysed.


1981 ◽  
Vol 106 ◽  
pp. 69-75
Author(s):  
I Parsons

A series of smal! volcanic centres cut Ordovician turbidites of Formation A in the southem part of Johannes V. Jensen Land between Midtkap and Frigg Fjord (Map 2). Their general location and main rock types were described by Soper et al. (1980) and their nomenclature is adopted here for fig. 22 with the addition of the small pipe B2. A further small intrusion, south-west of Frigg Fjord, was described by Pedersen (1980). The centres lie 5-10 km south of, and parallel to, the important Harder Fjord fault zone (fig. 22) which traverses the southern part of the North Greenland fold belt and shows substantial downthrow to the south (Higgins et al., this report).


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