The Ruin at Thésée

Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 102-106
Author(s):  
R. M. Butler
Keyword(s):  
The West ◽  
Main Road ◽  
Railway Line ◽  
The North ◽  
Large Size ◽  
North Bank ◽  
Road Following ◽  
The Village

The aim of this note is to bring to the attention of English readers a Roman building of large size, whose impressive ruins are well preserved, but whose purpose is uncertain and existence little known.The Roman road from Tours to Bourges ran along the north bank of the river Cher and for much of its length is followed by the modern N76. Two settlements or posting-stations lying on this road and marked on the Peutinger map under the names Gabris and Tasciaca can be located at the villages of Giévres and Thésée respectively. At this latter place, otherwise called Thézée or Tézée, 31 miles east of Tours, the main road, following the course of the Roman route, runs close beside the river, with the railway line separating them and low, bare hills rising immediately to the north. The towns of Montrichard to the west and St. Aignan on the east are respectively 4 and 5 miles away, and the village lies in the Loir-et-Cher département.

scholarly journals The Tsakonian Dialect.—I

1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt
Keyword(s):  
East Coast ◽  
Mountain Range ◽  
The South ◽  
The West ◽  
Northern Boundary ◽  
Grazing Land ◽  
Bare Rock ◽  
The North ◽  
Cultivable Land ◽  
The Village

The area over which the Tsakonian dialect is spoken lies on the east coast of the Peloponnese between the Parnon range and the sea. Its northern boundary is roughly the torrent which, rising on Parnon above Kastánitsa, flows into the sea near Ayios Andréas, its southern the torrent which, also rising on Parnon, passes through Lenídhi to the sea. A mountain range stretches along the coast from end to end of the district, reaching its highest point (1114 metres) in Mt. Sevetíla above the village of Korakovúni. Between Tyrós and Pramateftí, the seaward slopes of this range are gentle and well covered with soil. Behind these coast hills there stretches a long highland plain, known as the Palaiókhora, which, in the north, is fairly well covered with soil, but gradually rises towards the south into a region of stony grazing land, and terminates abruptly in the heights above Lenídhi. The high hill of Oríonda rises out of the Palaiókhora to the west and forms a natural centre-point of the whole district. Behind it stretching up to the bare rock of Parnon, is rough hilly country, cut here and there by ravines and offering but rare patches of cultivable land.

Pre-Kuṣāṇa Reliquaries from Pātaka, Swāt

1997 ◽  
Vol 7 (2) ◽  
pp. 249-255
Author(s):  
Muhammad Farooq Swāti
Keyword(s):  
The West ◽  
Main Road ◽  
The North ◽  
The Way

Pātaka marks the site of a Buddhist establishment that lies about two miles to the west from Chindākhwara village, situated on the main Kabal–Parrai road, in the Kabal Tehsīl of the Swāt District. The site is situated in the midst of cultivated fields, at the foothills of the mountains that stretch between Koṭlai and Khiamdara. On the way, from the main road to the site, one encounters four dry beds of hill torrents, khwars. Immediately to the north of the site, there is a seasonal stream called Pātaka khwargai, descending from the nearby hills to the west of the site and forming the only source of water in this far flung area.

The Excavation of an Iron Age Souterrain and Settlement at Carn Euny, Sancreed, Cornwall

1978 ◽  
Vol 44 ◽  
pp. 309-433 ◽  
Author(s):  
Patricia M. L. Christie ◽  
S. M. Elsdon ◽  
G. W. Dimbleby ◽  
A. Saville ◽  
S. Rees ◽  
...  
Keyword(s):  
Iron Age ◽  
Word Meaning ◽  
The West ◽  
North West ◽  
The North ◽  
South West ◽  
Dry Valley ◽  
The 19Th Century ◽  
The Hill ◽  
The Village

The ancient village of Carn Euny, formerly known as Chapel Euny, lies on a south-west slope just above the 500 foot contour in the parish of Sancreed in West Cornwall (fig. 1). The granite uplands of the region are rich in antiquities, as a glance at a recent survey shows (Russell 1971), not least those of the prehistoric period. The hill on which the site is situated is crowned by the circular Iron Age Fort of Caer Brane (pl. 27). Across the dry valley to the north-west rises the mass of Bartinny Down, with its barrows, while in the valley below the site near the hamlet of Brane is a small, well preserved entrance grave and other evidence of prehistoric activity. To the south-east about one mile away is the recently excavated village of Goldherring dating from the first few centuries of our era (Guthrie 1969). From later times, the holy well of St Uny and the former chapel which gave its name to the site, lie nearby to the west. The village contains a fine souterrain, locally known as a fogou, after a Cornish word meaning a cave (Thomas 1966, 79).Nothing appears to have been known of the settlement or Fogou before the first half of the 19th century when the existence of an unexplored fogou at Chapel Uny is first mentioned by the Reverend John Buller (1842), shortly followed by Edmonds (1849) who described to the Penzance Natural History and Antiquarian Society an ‘Ancient Cave’ which had been discovered by miners prospecting for tin.

scholarly journals XI.—Notes on the Geology of the Eildon Hills, in Roxburghshire

1853 ◽  
Vol 20 (2) ◽  
pp. 211-217
Author(s):  
James D. Forbes
Keyword(s):  
Small Group ◽  
The Other ◽  
Careful Examination ◽  
Eastern Slope ◽  
The West ◽  
North East ◽  
The North ◽  
South West ◽  
North Bank ◽  
The Town

The following remarks, being the result of a careful examination of a small district of country characteristic of the relations of the trap formations, are perhaps worthy of being recorded; although the general features of the county of Roxburgh have been very clearly stated in a paper by Mr Milne, published in the 15th volume of the Edinburgh Transactions.The outburst of porphyritic trap forming the conspicuous small group of the Eildon Hills, may be stated to be surrounded by the characteristic greywacke of the south of Scotland. It forms an elongated patch on the map, extending from the west end of Bowden Muir in the direction of the town of Selkirk, and running from west-south-west to east-north-east (true) towards Bemerside Hill, on the north bank of the Tweed. The breadth is variable, probably less than is generally supposed; but it cannot be accurately ascertained, owing to the accumulated diluvium which covers the whole south-eastern slope of this elevated ridge. On this account, my observations on the contact of rocks have been almost entirely confined to the northern and western boundaries of the trap, although the other side was examined with equal care.

Laconia

1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls
Keyword(s):  
Sea Level ◽  
The Other ◽  
The South ◽  
The West ◽  
Urban Settlement ◽  
West Side ◽  
The North ◽  
The Village

The village of Kalývia Sokhás lies against the base of one of the massive foothills in which Taygetus falls to the plain three or four miles to the south of Sparta (Plate 26, 1). It is bounded by two rivers which flow down in deep clefts from the mountain shelf. The hillside above rises steeply to a summit which is girt with cliffs on all but the west side and cannot be much less than four thousand feet above sea level; this von Prott believed to be the peak of Taleton. Its summit is crowned by the ruins of a mediaeval castle which was undoubtedly built as a stronghold to overlook the Spartan plain; the only dateable object found there, a sherd of elaborate incised ware, indicates occupation at the time when the Byzantines were in possession of Mystra. The location of the other sites mentioned by Pausanias in this region remains obscure, but fortunately that of the Spartan Eleusinion has not been in doubt since von Prott discovered a cache of inscriptions at the ruined church of H. Sophia in the village of Kalývia Sokhás. In 1910 Dawkins dug trenches at the foot of the slope immediately above the village and recovered a fragment of a stele relating to the cult of the goddesses and pieces of inscribed tiles from the sanctuary. The abundance of water in the southern ravine led von Prott to conclude that the old town of Bryseai with its cult of Dionysus also lay at Kalývia Sokhás; but no traces of urban settlement have come to light at the village, and the name rather suggests copious springs such as issue from the mountain foot at Kefalári a mile to the north where ancient blocks are to be seen in the fields.

Note on the Occurrence of Dayia navicula (J. de C. Sowerby) in the Lower Ludlow Rocks of Shropshire

1939 ◽  
Vol 76 (8) ◽  
pp. 360-361 ◽  
Author(s):  
J. Shirley
Keyword(s):  
Thin Layer ◽  
The West ◽  
West Side ◽  
Great Thickness ◽  
Railway Line ◽  
North East ◽  
The North ◽  
North Side ◽  
Large Numbers ◽  
Type Area

In the type area the Ludlow Rocks generally have been divided into Lower Ludlow Shales, Aymestry Limestone, Dayia Shales and Whitcliffe Flags in upward sequence. The Dayia Shales are characterized by the presence of enormous numbers of Dayia navicula (J. de C. Sowerby). This preponderance of D. navicula in the shales immediately above the Aymestry Limestone has caused a tendency to regard beds in other localities containing this fossil as being on the same stratigraphical horizon in spite of the character of the accompanying fauna. In two recent papers on the Ludlow Rocks of the Welsh Borderland (Straw, 1937, and Earp, 1938) it has been shown that D. navicula ranges through at least 3,000 feet of strata, occurring commonly throughout this great thickness and outlasting more than one change of fauna. Although, in this area, the brachiopod ranges from the zone of Monograptus nilssoni into the Upper Ludlow it has not hitherto been recorded below the Aymestry Limestone in Shropshire. This gap in our knowledge is now filled by the discovery of specimens in Lower Ludlow Shales exposed in a small quarry 40 yards north-east of Stokewood Cottage, which is on the west side of the railway line a little over a mile south of Craven Arms. The quarry shows about 15 feet of nodular shales with thin limestone seams. The commonest fossils are Chonetes laevigata (J. de C. Sowerby), C. minima (J. de C. Sowerby), and Stropheodonta filosa (J. de C. Sowerby) which occur in large numbers on some of the bedding surfaces. Other fossils are Stropheodonta euglypha (Dalman), Delthyris sp., Orthoceras sp., Dalmanites sp., and a plectambonitid. Dayia navicula seems to be confined to a thin layer on the north side of the quarry. Graptolites referable to Monograptus cf. chimaera occur fairly commonly. About 400 yards in a south-easterly direction another small quarry exposes Conchidium Limestone which is about 170 feet stratigraphically above the beds in the first quarry.

A Ball Court Located on the San Pedro River in Southeastern Arizona

1951 ◽  
Vol 16 (3) ◽  
pp. 257-260 ◽  
Author(s):  
Charles C. Dipeso
Keyword(s):  
Archaeological Site ◽  
River Channel ◽  
The West ◽  
San Pedro River ◽  
The North ◽  
San Pedro ◽  
Cochise County ◽  
Desert Flora ◽  
The Village ◽  
The City

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).

scholarly journals THE TERRITORY OF THE CENTRAL SCYTHIA (FROM SOLOKHA TO CHORTOMLYK)

2018 ◽  
Vol 26 (1) ◽  
pp. 147-168 ◽  
Author(s):  
Yu. V. Boltryk ◽  
V. M. Okatenko ◽  
G. M. Toscev
Keyword(s):  
Eastern Europe ◽  
Second Order ◽  
Marmara Sea ◽  
Burial Ground ◽  
Eastern European ◽  
The West ◽  
The North ◽  
Burial Mounds ◽  
The Village

This article is devoted to the extensive description of the environment of the two largest settlement structures of the Eastern European steppes — the Kapuliv and Kamyanka which date V—III centuries BC. These two powerful settlements appeared on the opposite banks near the ancient crossings through the Dnipro. They formed the main core of the Scythian state, in which Kapuliv served as the capital and Kamyanka was its economic partner. Intense life here has arisen from the time of Ariapet’s rule to the life of the descendants of King Ateus. The Scythians chose the best place in the Pontic steppe, where in the zone of floodplain meadows and forests there were numerous straits with lakes surrounded by magnificent pastures. Therefore, along with these two main settlements, on the banks and partly in the floodplain, there were many settlements of the second order. The importance of this zone is emphasized by the accumulation of kurhans and graveyards placed almost symmetrically on different shores. In the immediate surrounding of the settlements there are almost equal in importance burial mounds of the ordinary population. Among them are the burial ground near the village Kut, the Nikopol mound field and the burial ground of Mamay-Gora. The last one is the largest in the Eastern Europe in terms of the number of excavated burials. This graveyard is unique due to five large kurhans, located in one line: three long kurhans and two round in plan. It is possible that there was a general Scythian cult center. Further from the Dnipro there were burial memorials of representatives of the higher social stage, among which were the largest burial mounds of Scythia — Solokha and Chortomlyk. There is a noteworthy mound alley (1.6 km long), which retreated to the west of the Solokha kurhan and turned slightly to the north, where it probably connected with a part of another smaller kurhan alley. Not far from a smaller alley there was the recently opened manufacturing settlement Sorokina Balka. The time of its existence (all IV BC) is recorded by the findings of the coins of the cities of the North Pontus, the Marmara Sea and Macedonia.

scholarly journals Notes on some Flint-Chipping Sites at Risby, Suffolk

1919 ◽  
Vol 3 (1) ◽  
pp. 67-72
Author(s):  
H. Dixon Hewitt
Keyword(s):  
The West ◽  
Small Stream ◽  
Main Road ◽  
Eastern Boundary ◽  
Dry Valley ◽  
The Village

My attention was first drawn to this locality in the summer of 1915. I exhibited the first few specimens obtained before this Society at the meeting held at Norwich on December 13th of that year, and a brief notice of the exhibit appeared in the Appendix to the “Proceedings,” Vol. II., p. 321.The site or sites (numbered for reference purposes LV.), are in the parish of Risby, two miles West of the village, on the Cavenham road, from which village they are only distant about one mile.The sites occupy the Northern bank and bottom of a small dry valley on Risby Poor's Heath. This little valley runs towards the (now) very small stream which crosses the main road at Roberts'-Bridge, which stream is itself a feeder of the Lark; hence the fall is from the Eastern boundary of the heath towards the West. The first site was indicated to me by numerous shallow, somewhat rectangular, excavations, apparently made, say, within the last thirty or forty years, presumably for the purpose of getting road-stone.

scholarly journals Point Seroprevalence Survey of Ehrlichia ruminantium Infection in Small Ruminants in The Gambia

2005 ◽  
Vol 12 (4) ◽  
pp. 508-512 ◽  
Author(s):  
Bonto Faburay ◽  
Susanne Munstermann ◽  
Dirk Geysen ◽  
Lesley Bell-Sakyi ◽  
Ansumana Ceesay ◽  
...  
Keyword(s):  
Immunosorbent Assay ◽  
Small Ruminants ◽  
The Gambia ◽  
Enzyme Linked Immunosorbent Assay ◽  
Serum Samples ◽  
The West ◽  
Ehrlichia Ruminantium ◽  
The North ◽  
North Bank ◽  
Western Division

ABSTRACT Using the MAP1-B enzyme-linked immunosorbent assay, we tested 1,318 serum samples collected from sheep and goats at 28 sites in the five divisions of The Gambia to determine the Ehrlichia ruminantium seroprevalence rates and to assess the risk for heartwater. About half (51.6%) of 639 sheep were positive, with seroprevalence rates per site varying between 6.9% and 100%. The highest seroprevalence was detected in the western part of the country (88.1% in the Western Division and 62.1% in the Lower River Division). Sheep in the two easterly divisions (Central River and Upper River divisions) showed the lowest seroprevalence of 29.3% and 32.4%, respectively, while those in the North Bank Division showed an intermediate prevalence of 40.6%. In goats, less than one-third (30.3%) of 679 animals tested were positive. The highest seroprevalence was detected in goats in the North Bank Division (59%) and Western Division (44.1%). Goats in the Lower River Division showed an intermediate level of 21.9%, whereas the lowest rates were found in the eastern part of the country (4.8% in the Central River Division and 2.3% in the Upper River Division). At nearly all sites, seroprevalence rates were higher in sheep than in goats. The results show a gradient of increasing heartwater risk for susceptible small ruminants from the east to the west of The Gambia. These findings need to be taken into consideration when future livestock-upgrading programs are implemented.

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