ARISTODEMUS ‘THE GOOD’ AND THE TEMPLE OF ARTEMIS AGROTERA AT MEGALOPOLIS

2016 ◽  
Vol 66 (1) ◽  
pp. 128-133
Author(s):  
Annalisa Paradiso

Aristodemus, a Phigalian by birth, was tyrant of Megalopolis for around fifteen years in the first half of the third century b.c., possibly from the time of the Chremonidean War (267–262) until around 251, when he was murdered by two Megalopolitan exiled citizens, Megalophanes and Ecdelus, pupils of the Academic Arcesilaus. While giving an account of his violent death, Pausanias, none the less, draws a very positive portrait of him, also mentioning the nickname ‘the Good’ which he probably read on Aristodemus' grave. Pausanias also reports the foundation of two temples by the tyrant, both dedicated to Artemis. At 8.35.5 he locates one of the two temples at thirteen stades from Megalopolis on the road to Methydrion, so to the north. There, he says, is a place named Scias, where there are ruins of a sanctuary of Artemis Sciaditis. At 8.32.4, Pausanias briefly refers to the temple of Artemis Agrotera at Megalopolis. He says only that the sanctuary was on a hill in the south-east district of the polis, and adds that it was dedicated as an ἀνάθημα by the tyrant as well.

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.


Antiquity ◽  
2012 ◽  
Vol 86 (332) ◽  
pp. 444-455 ◽  
Author(s):  
Paul Arthur ◽  
Girolamo Fiorentino ◽  
Anna Maria Grasso

The cumulative power of botanical and chemical analysis is demonstrated here by our authors, who succeed in opening a window on Europe's most obscure period, in the south as in the north, the time after the Roman and then the Byzantine empire lost its hold. The emphasis here is on the rise in production and trade of cash crops in the eighth century as detected by survey, pollen, charcoal and residues. Taken together, the new data show a community well on the road to economic recovery after two centuries of recession and monetary failure.


1967 ◽  
Vol 35 ◽  
pp. 12-22
Author(s):  
Nancy L. Hirschland

Sardis, most famous as the capital of Lydia in the seventh and sixth centuries B.C., was also a major Roman city under the Roman empire. The wealth of Croesus had dissipated, but the Roman inhabitants of Sardis again had the good fortune to live in a prosperous time. The fertility of the Hermus plain and its strategic inland position on the road to the Roman east stood the city in good stead. Nowhere among the ruins of Sardis is the opulence of the third century better to be seen than in the rich and elaborate Marble Court of the Roman gymnasium.The Marble Court was first built, along with the gymnasium proper, under Lucius Verus in A.D. 165. At that time it served as an independent unit which was connected with—but did not lead directly into—the gymnasium. It was architecturally a part of the palaestra in front. Then in the early third century (212–213) elaborate additions were made : pavilions adorned three sides of the court, a monumental pedimented gate led into the gymnasium, and on the fourth side a screen colonnade was erected between the Marble Court and the palaestra. From this colonnade have come most of the head-capitals at Sardis (fig. 1).


Author(s):  
Andrei Sokolov ◽  
Andrei Sokolov ◽  
Boris Chubarenko ◽  
Boris Chubarenko

Three dumping sites located at the south-eastern part of the Baltic Sea (Kaliningrad Oblast) at shallow depths are considered. The first one is located to the south of the Vistula Lagoon inlet in front of a permanently eroded open marine shore segment. The second one is located to the north of the Vistula Lagoon inlet, and is used now for disposing of dredged material extracted from the Kaliningrad Seaway Canal. The third dumping site is located near the northern shore of the Sambian Peninsula to the east of the Cape Gvardeijski and assigned for disposing the dredged material extracted from the fairway to the Pionerskij Port located nearby. The last site is planned to be used for disposing of dredged material from the future port that should be constructed there before the beginning of the FIFA World Cup 2018. All three dumping sites are located not far from the eroded segments of the shore. The question behind the study is: would it possible that disposed material will naturally transported from the damping site to the shore and accumulate there to protect it from erosion? A numerical hydrodynamic-transport 3D model (MIKE) was used to model sediment transport under different wind actions. The winds with the speed stronger than 15 m/s complete wash out disposed material from the dumping site and spreading it over the wide area with a negligible layer thickness. Winds of about 7-10 m/s transport material along the shore at a distance of few kilometers that may be useful for shore protection. The first location of the dumping site (to the south of the Vistula Lagoon inlet) looks very ineffective for potential protection the shore nearby. At the other hand, the second and especially the third locations are favorable for transport of disposed material to the shore, the most favorable conditions are at onshore or alongshore currents.


Author(s):  
Andrei Sokolov ◽  
Andrei Sokolov ◽  
Boris Chubarenko ◽  
Boris Chubarenko

Three dumping sites located at the south-eastern part of the Baltic Sea (Kaliningrad Oblast) at shallow depths are considered. The first one is located to the south of the Vistula Lagoon inlet in front of a permanently eroded open marine shore segment. The second one is located to the north of the Vistula Lagoon inlet, and is used now for disposing of dredged material extracted from the Kaliningrad Seaway Canal. The third dumping site is located near the northern shore of the Sambian Peninsula to the east of the Cape Gvardeijski and assigned for disposing the dredged material extracted from the fairway to the Pionerskij Port located nearby. The last site is planned to be used for disposing of dredged material from the future port that should be constructed there before the beginning of the FIFA World Cup 2018. All three dumping sites are located not far from the eroded segments of the shore. The question behind the study is: would it possible that disposed material will naturally transported from the damping site to the shore and accumulate there to protect it from erosion? A numerical hydrodynamic-transport 3D model (MIKE) was used to model sediment transport under different wind actions. The winds with the speed stronger than 15 m/s complete wash out disposed material from the dumping site and spreading it over the wide area with a negligible layer thickness. Winds of about 7-10 m/s transport material along the shore at a distance of few kilometers that may be useful for shore protection. The first location of the dumping site (to the south of the Vistula Lagoon inlet) looks very ineffective for potential protection the shore nearby. At the other hand, the second and especially the third locations are favorable for transport of disposed material to the shore, the most favorable conditions are at onshore or alongshore currents.


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.


2021 ◽  
Author(s):  
Giles Clarke

Outside the north gate of Venta Belgarum, Roman Winchester, a great cemetery stretched for 500 yards along the road to Cirencester. Excavations at Lankhills from 1967 to 1972 uncovered 451 graves, many elaborately furnished, at the northern limits of this cemetery, and dating from the fourth century A.D. This book, the second in a two-part study of Venta Belgarum, which forms the third volume of Winchester Studies, describes the excavations of these burials and analyses in detail both the graves and their contents. There are detailed studies and important re-assessments of many categories of object, but it is the information about late Roman burial, religion, and society which is of special interest.


1936 ◽  
Vol 8 (2-3) ◽  
pp. 419-435 ◽  
Author(s):  
T. Burrow

The “North-Western Prakrit” as Konow has called it is represented by the following documents.(1) The two versions of Aśoka's edicts preserved at Mansehra’ and Shahbazgarhi. At this stage many of the characteristic features of the language have not yet developed, e.g. śr > ṣ, śv > śp.(2) The later Kharoṣṭhi inscriptions, mostly short, collected by Konow in the second volume of the Corp. Inscr. Ind.(3) The Kharoṣṭhi manuscript of the Dhammapada discovered near Khotan (Manuscript Dutreuil du Rhins).(4) The Kharoṣṭhi documents from Niya, representing the administrative language of the Shan-Shan kingdom in the third century A.D. In the Journ. As., 1912, pp. 337 ff., J. Bloch examined the dialectical peculiarities of the Manuscript Dutreuil du Rhins and showed that they appeared in modern times in the languages of the North-West.


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