I. The site and its environs

1959 ◽  
Vol 53 ◽  
pp. 1-8 ◽  
Author(s):  
J. M. Cook
Keyword(s):  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
High Terrace ◽  
Circular Platform ◽  
East End ◽  
Olive Trees ◽  
Fig Trees ◽  
South Axis

The site of Old Smyrna lies on a low spur at the foot of the Yamanlar Daği, or Mountain of Unco Things, at a distance of 450 metres east of the present coastline. The spur is 365 metres long on a north-south axis, with a maximum breadth of 250 metres. On the north-east and east its outline is marked by a bank, revetted in large part by a high terrace wall of small stones. The elevated north-west corner of the site is encircled by superimposed terraces leading up to a circular platform or belvedere, which dominates the site, at an altitude of 21·3 m. above sea-level (Plates 2c, 6a, Squares G–Hix). On the west side the spur is bounded by a cart road leading inland to Bornova, and at the south tip it merges into the low-lying pasturage by a sluggish stream. The terracing of the hillock, which in the north-west presents a picturesque aspect, is believed in the main to be the work of a landowner named Turlita in the nineteenth century. A zone along the north side of the site, corresponding in width to the main sector of our excavations there, is planted with olive trees, of which we were obliged to cut down a score; there is also a narrow fringe of olives along the eastern edge of the site. The greater part of the surface of the hillock is divided between two vineyards, the upper on the north and the lower on the south, separated by a bank which is bordered near its east end by a row of fig trees (Squares Nxvi to Gxix); there is also a smaller vineyard of triangular outline on the slope between the upper vineyard and the Bornova road.

Part VI. The Cyclopean Terrace Building and the Deposit of Pottery beneath It

1954 ◽  
Vol 49 ◽  
pp. 267-291
Author(s):  
Elizabeth B. Wace
Keyword(s):  
Contour Line ◽  
The South ◽  
Main Road ◽  
North West ◽  
North East ◽  
The North ◽  
South West

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.

The ziggurrat and temples of Nimrud

Iraq ◽  
2002 ◽  
Vol 64 ◽  
pp. 135-216 ◽  
Author(s):  
J. E. Reade
Keyword(s):  
Nineteenth Century ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
Directorate General ◽  
The 1950S

The buildings on the citadel of Nimrud, ancient Kalah or Kalḫu, constitute a most impressive monument (Fig. 1; Postgate and Reade 1980), but the sporadic way in which they have been excavated leaves many questions unanswered. One puzzling area lies north and north-east of the great North-West Palace. It includes the ziggurrat, and the shrines of Ninurta, of Ištar Šarrat Nipḫi (formerly read Bēlat Māti) and of the Kidmuri (or Ištar Bēlat Kidmuri). Their interrelationships have yet to be established, and texts refer to further gods resident at Kalah. Excavations in this quarter were conducted by Layard, Rassam, Rawlinson, Loftus and Smith in the nineteenth century, and by Mallowan in the 1950s, and were resumed by staff of the Iraq Directorate-General of Antiquities in the early 1970s. This paper summarizes some of what we know or may deduce about the area, and defines some of the remaining problems; it does not include, except in passing, the relatively well-known Nabû Temple to the south. I have endeavoured to refer to all items except sherds found during British excavations in the area, but have not attempted the detailed publication which many of the objects, groups of objects, and pottery records may merit.A possible arrangement of the buildings in this area of Nimrud about 800 BC is given in Fig. 2, but it is a reconstruction from inadequate evidence. The relative dates, dimensions, locations and orientations of many excavated structures are arguable, and the plans published by different excavators cannot be fully reconciled. Major uncertainties concern the ziggurrat, the citadel-wall, the Kidmuri shrine and the area between the North-West Palace and the Ninurta shrine. There are many minor uncertainties. My reconstruction includes speculative features, while omitting some excavated walls which I regard as secondary.

VI. The Stained Glass of the Chapel of the Vyne and the Chapel of the Holy Ghost, Basingstoke

Archaeologia ◽  
1982 ◽  
Vol 107 ◽  
pp. 141-152 ◽  
Author(s):  
H. G. Wayment
Keyword(s):  
Virgin Mary ◽  
Henry Viii ◽  
Stained Glass ◽  
The South ◽  
Holy Ghost ◽  
North East ◽  
The North ◽  
East End ◽  
Upper Register ◽  
Patron Saints

Among the few ensembles of stained glass which survive in this country from the early Renaissance the windows of the Chapel of the Vyne, near Sherborne St. John, Hampshire, are one of the most remarkable (pl. XL). Though much smaller in scale and extent than the glass in King's College Chapel, Cambridge, they are no less distinguished in quality, and their state of preservation is almost as good. Moreover, there are still in existence important fragments from a larger but closely related set which formerly stood in the Chapel of the Holy Ghost at Basingstoke. Both sets were evidently commissioned by Sir William, later Baron Sandys, a distinguished soldier and administrator who, without ever reaching the highest levels, served Henry VIII both at home and abroad from the beginning of the reign until his death in 1540. After campaigning in Guienne and Picardy early in the reign he was appointed Treasurer of Calais from 6th October 1517, and spent much of the next nine years there. Meanwhile he had married Margery, the niece and heiress of Sir Reginald Bray, one of Henry VII's most trusted administrators, and begun the reconstruction of the Vyne which had belonged to the Sandys family since the midfourteenth century. There had since the twelfth century been a chapel of the Virgin in the grounds, and this foundation he incorporated into the eastern end of the house itself. Sir William's chapel measures 35 ft. in length, 19 in width, and 25 in height (10·67 × 5·79 × 7·62 m.). The apsidal east end ie three-sided, and in the east wall and the two canted walls are three windows, each consisting of three transomed lights forming an upper and lower register. The lower lights represent donors at prayer supported by their patron saints: King Henry VIII can be recognised in the east window with St. Henry the Emperor; in the north-east Catherine of Aragon with St. Catherine of Alexandria; and in the south-east the king's sister, Margaret, Queen of Scots, with St. Margaret issuing from the dragon. In the upper register three Passion scenes proceed from south to north: in the south-east Christ carries his cross from right to left, assisted by Simon of Cyrene, while St. Veronica, the Virgin Mary and her attendant women move towards him from the left; in the east is a narrative Crucifixion animated by a large number of figures; and in the north-east the resurrected Christ scatters the astonished soldiers to either side.

IV.—The Upper Trias of Leicestershire

1913 ◽  
Vol 10 (5) ◽  
pp. 205-215 ◽  
Author(s):  
A. R. Horwood
Keyword(s):  
Black Shales ◽  
The South ◽  
The West ◽  
West Side ◽  
North West ◽  
The North ◽  
Eastern Boundary ◽  
East End

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.

Social Administration of the Kru. A Preliminary Survey

Africa ◽  
1937 ◽  
Vol 10 (1) ◽  
pp. 75-96 ◽  
Author(s):  
H. Scudder Mekeel
Keyword(s):  
West Africa ◽  
West African ◽  
Preliminary Survey ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
Archaeological Work ◽  
Opening Paragraph ◽  
Physical Type

Opening ParagraphThe Kru, a West African Negro group, inhabit the central and southern part of Liberia. They are surrounded by the Basa peoples to the north-west, by the Grebo to the south-east and by the Putu to the north-east. The informant, Thomas Tarbour (Sieh Tagbweh), from whom the following material was derived, was a native of Grand Cess (Siglipo), a large coast town near the border of the Grebo country. The Kru, along with other related groups in that part of West Africa, have a tradition of having migrated from far to the north-east. The physical type is that of the short, stocky Bush negro. No archaeological work has been done in the region, and such ethnological material as has been collected is a mere beginning.

scholarly journals CHECKLIST AND DISTRIBUTION OF MARINE AND FRESHWATER LEECHES (ANNELIDA, CLITELLATA, HIRUDINEA) IN TUNISIA WITH IDENTIFICATION KEY

2015 ◽  
Vol 2 (1) ◽  
pp. 3-19 ◽  
Author(s):  
Raja Ben Ahmed ◽  
Yasmina Romdhane ◽  
Saïda Tekaya
Keyword(s):  
Identification Key ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
West Region ◽  
The World ◽  
The Future

In this study 13 leech species from Tunisia are listed. They belong to 2 orders, 2 suborders, 4 families and 11 genera. The paper includes also data about hosts and habitats, distribution in the world and in Tunisia. Faunistic informations on leeches were found in literature and in the results of recent surveys conducted by the authors in the North East and the South of the country. The objectives of this study were to summarize historical and recent taxonomic data, and to propose an identification key for species signalized. This checklist is to be completed, taking into account the hydrobiological network of the country especially the North West region, which may reveal more species in the future

scholarly journals A plutonic diorite complex in the north of the Fiskenæsset region

1976 ◽  
Vol 73 ◽  
pp. 72-80
Author(s):  
W.R Fitches
Keyword(s):  
The Body ◽  
Main Body ◽  
The South ◽  
North East ◽  
The North ◽  
South West ◽  
West Part ◽  
Preliminary Account ◽  
East End

A thick diorite-monzodiorite sheet over 2 km in length and up to 600 m in width (fig. 35) is exposed at 50°25'E and 63°55'N, about 7 km south of Qeqertaussaq by Kangerdluarssûngûp taserssua. Several diorite dykes, some over 10 m in thickness, tie parallel to the main body and up to 300 m from it. The north-east end of the body is covered by superficial deposits whilst the south-west part has not yet been mapped out. This is therefore a preliminary account, including petrography, fie1d relations and some geochemistry, and more information will become available during subsequent field seasons.

III.—On the Discovery of a Quartzose Conglomerate at Caldon Low, Staffs

1919 ◽  
Vol 6 (2) ◽  
pp. 59-64 ◽  
Author(s):  
J. Wilfrid Jackson ◽  
W. E. Alkins
Keyword(s):  
The South ◽  
North West ◽  
Good Fortune ◽  
North East ◽  
The North ◽  
South West ◽  
Limestone Quarries ◽  
Strong Joint

During a visit to the limestone quarries at Caldon Low last September we had the good fortune to discover an interesting exposure of a quartzose conglomerate containing numerous fossils. The bed was exposed in a strong joint-face running approximately N.N.W. to S.S.E., at the northern extension of the quarry on the north-west flank of the Low, just beyond the mineral line of the North Staffordshire Railway. The altitude is about 900 feet O.D. The conglomerate apparently extended some little distance to the south-west before the opening of the quarry, as we ascertained that some 20 or 30 yards had been removed in gaining access to the limestone behind. It appears to extend for some distance round the flank of the Low towards the north-east.

Habitat of the Eastern Barred Bandicoot, Perameles gunnii, in Tasmania: an Analysis of Road-kills

1996 ◽  
Vol 23 (6) ◽  
pp. 721 ◽  
Author(s):  
M.M Driessen ◽  
S.A Mallick ◽  
G.J Hocking
Keyword(s):  
Agricultural Land ◽  
Soil Depth ◽  
Traffic Volume ◽  
Private Land ◽  
The South ◽  
Management Options ◽  
North West ◽  
Road Kill ◽  
North East ◽  
The North

The habitat requirements of the eastern barred bandicoot, Perameles gunnii, in Tasmania were investigated with road-kill survey data and by mapping habitat features along survey routes. Road-kills of eastern barred bandicoots were most numerous in the South-east and North-west, less common in the North-east and Midlands, and very uncommon on the East Coast. Logistic regression of bandicoot presencelabsence data suggested that traffic volume is the major determinant of the road-kill distribution of eastern barred bandicoots around Tasmania. Along with traffic volume, rainfall was found to be strongly associated with the presence of eastern barred bandicoot road-kills for the state combined and for the South-east and Northeast, while along the Huon Highway in the South-east, soil depth was associated with the presence of roadkills. Favoured habitat of the eastem barred bandicoot is high-quality agricultural land with deep soils and high rainfall. It is hypothesised that clearing for agriculture in south-eastem, north-eastem and north-westem Tasmania has opened up previously unsuitable, heavily forested habitat for colonisation by eastern barred bandicoots. The resulting mosaic of pasture and remnant bush appears to provide ideal habitat for the eastern barred bandicoot. However, the majority of bandicoot habitat is found on private land, making the species vulnerable to changes in farming practices. Possible management options are briefly discussed.

X.—Geology of the Outer Hebrides. Part III.—North Uist and Benbecula

1926 ◽  
Vol 54 (2) ◽  
pp. 467-489 ◽  
Author(s):  
T.J. Jehu ◽  
R.M. Craig
Keyword(s):  
Narrow Channel ◽  
Central Position ◽  
The South ◽  
North West ◽  
North East ◽  
The North ◽  
Outer Hebrides ◽  
The Hill ◽  
North And South ◽  
Southern Extremity

Benbecula signifies “the hill of the fords,” and the island was so designated owing to the fact that there is on it only one hill of any prominence, and that it is connected with the larger islands to the north and south by fords passable only at low water. The origin of the name “Uist” is referred to in a previous communication.These islands occupy a central position in the Outer Hebrides, lying between South Uist and Harris. They are bounded on the west and north-west by the Atlantic Ocean; on the north-east by the Sound of Harris; on the east by the Little Minch, which at its narrowest part is about 16 miles broad; and on the south by a narrow channel separating Benbecula from South Uist. The area embraced in this communication extends from the Isle of Shillay in the north to the Isle of Wiay at the south-east corner of Benbecula, and includes not only the main islands of North Uist and Benbecula but also a number of smaller isles adjoining the main ones. Including the intervening channels, the total length from Shillay in the north to the southern extremity of Benbecula is about 28 miles.

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