Cyrene: A Survey of Certain Rock-Cut Features to the South of the Sanctuary of Apollo

1957 ◽  
Vol 77 (2) ◽  
pp. 301-310 ◽  
Author(s):  
G. R. H. Wright
Keyword(s):  
Basic Structure ◽  
Water Tank ◽  
The South ◽  
The West ◽  
Lower Face ◽  
South West ◽  
Ancient Rock ◽  
The Temple ◽  
Two Sides

Basic Structure: A broad flight of twenty-one steps leads up from the south-west angle of the Temple of Apollo to a partially paved court immediately in front of the lower face of the scarp. This is given a quadrilateral delimitation by the angular revetment of an irregularity in the scarp to the west, and by the monumental water tank to the east of the entrance to the grotto. The entrance was hewn in the cliff face in the form of three arches (now much destroyed), and was revetted with large well-draughted limestone blocks. Of these, only the lower two courses are now in situ, but individual blocks of the upper courses have been collected and amongst them are those with crowning mouldings and one bearing the fragment of a Greek inscription (height:of letters, 25 cm. approximately).The interior of the grotto consists basically of a central oblong depression, paved and cemented, surrounded on the two sides and the back by a raised staging—thus giving rise to the term of reference ‘TRICLINIUM’—while between the staging and the walls are the tanks and channels: associated with the water supply and drainage.Considered longitudinally, the interior may be divided into three entities. The first extends from the entrance to a pair of rock-hewn columns bearing rude inscriptions. Immediately above this compartment lay the terrace of an ancient rock-cut path and its collapse has breached the path and totally unroofed this section of the grotto.

Five tombs at Knossos

1963 ◽  
Vol 58 ◽  
pp. 30-43 ◽  
Author(s):  
J. N. Coldstream
Keyword(s):  
Good Condition ◽  
Good Deal ◽  
Lower Edge ◽  
Water Pipe ◽  
The West ◽  
Light In August ◽  
South West ◽  
History Of ◽  
The Temple

On the east slope of Lower Gypsades hill, about 100 metres west of the Temple Tomb, a chamber tomb came to light in August 1958, when a cutting for a new water pipe was driven through the area (A in Plate 9 a). In the course of this operation, part of a plain larnax (iii) was sliced off, and much earth removed from the west end of the collapsed chamber: at no point, however, had the municipal workmen penetrated to the tomb floor.The chamber was approached by a sloping dromos (Plate 9 a: length 2·80 metres; max. width 1 metre), roughly cut into the natural kouskouras rock: its walls were approximately perpendicular. Although the gradient varied a good deal, there was no suggestion of a stairway.The blocking wall was found in good condition. Of especial interest were the numerous fragments of larnakes that had been built into its fabric: some of them could be recognized as belonging to each of the three fragmentary larnakes (i, ii, v) whose scattered pieces were found below and around the two undisturbed burials in the chamber (iii, iv). We may thus distinguish two periods in the history of the tomb: larnakes i, ii, and v were evidently smashed up in order to make room for iv and iii, which must have been deposited in that order. The debris of v was found under iv, with a few adult bones in its wreckage. Part of i lay on the floor near the south-west corner, where two plain vases (2, 3) were found in situ, hence, also, came most of the fragments of the fine L.M. IIIA 2 stirrup vase (1), although its other pieces were scattered all over the floor of the tomb. This small group of offerings may belong to the disturbed adult skeleton, whose skull lay up against the lower edge of iii. Curiously, some fragments of i and ii were also found above the broken lid of iv (Plate 9 b): perhaps the lid of the later larnax was accidentally smashed at the time of the funeral, in which case the debris from earlier burials could have been piled up above it, as a rough and ready means of protection.

scholarly journals TEMUAN FRAGMEN GERABAH SEBAGAI INDIKASI PERMUKIMAN KUNO DI SITUS BOROBUDUR

2013 ◽  
Vol 33 (2) ◽  
pp. 211-226
Author(s):  
Agni Sesaria Mochtar
Keyword(s):  
20Th Century ◽  
Cultural Context ◽  
The Other ◽  
Back Side ◽  
The South ◽  
South West ◽  
Pottery Sherds ◽  
Few Data ◽  
The Temple

Borobudur temple has been famously known as one of the Indonesian heritage masterpiece. Various aspects of it had been studied thoroughly since the beginning of 20th century A.D. Those studies tended to be monumental centric, giving less attention to the cultural context of the temple and its surroundings. Settlement in the nearby places is one of the topics which not have been studied much yet; leaving a big question about how the settlement supported continuity of many activities in the temple, or even the other way around; how the temple affected the settlement. There is only a few data about old settlement found in situ in Borobudur site, only abundance of pottery sherds. The analysis applied on to the potteries find during the 2012 excavation had given some information about the old settlement in Borobodur site. The old settlement predicted as resided in the south west area, in the back side of the monument.

The Base and Top of the Coral-rock in Barbados

1937 ◽  
Vol 74 (8) ◽  
pp. 337-359 ◽  
Author(s):  
C. T. Trechmann
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
East Part ◽  
Varying Thickness ◽  
South West ◽  
New Information ◽  
Main Portion ◽  
Coral Rock

1. The coral-rock commences nearly everywhere with a basal bed of varying thickness containing a fauna of pre-Pleistocene aspect among which the genus Haliotis (absent from these coasts at the present day), Pleurotomaria, Meiocardia, etc., are noticeable. This faunule may have lived at a depth of 700–1,000 feet.2. The supposition that the southerly anticlines are a later uplift than the main portion of Barbados is supported by the absence of ravines, and the presence of post-coral-rock beds which occur as coastal veneers at low altitudes, and in greater thickness in the south-east corner near Whitehaven.3. The south-east part of the island from Consett Point to Ragged Point has probably extended further seawards in comparatively recent times ; the series of converging faults and dislocations in the cliff sections suggest that the thrusts from the west or south-west may have been resisted by this part of the island.4. The relative claims of fault-scarping or marine erosion in production of the rising terraces is discussed ; and new information regarding the thickness of the coral-rock at sea-level from a boring is detailed.5. The finding of a faunule with Pliocene or possibly Miocene affinities at the base of the coral-rock puts the Oceanic series further back, into the Miocene.

scholarly journals The Results of a Chemical, Microscopical and Bacteriological Examination of Samples of London Milks

1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton
Keyword(s):  
Bacteriological Examination ◽  
Milk Supply ◽  
The South ◽  
The West ◽  
The North ◽  
South West ◽  
Pure Milk

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.

Archaeological Discoveries in Sicily and Magna Graecia

1939 ◽  
Vol 59 (2) ◽  
pp. 213-228
Author(s):  
Umberto Zanotti-Bianco
Keyword(s):  
Eighteenth Century ◽  
Ground Level ◽  
The South ◽  
Total Length ◽  
Magna Graecia ◽  
South West ◽  
Southern Side ◽  
The Temple ◽  
Southern Flank

In my previous report (JHS, 1938, p. 247) I spoke of the work being carried on at Syracuse to bring to light the remains of the temple of Apollo. The east, north, and west sides had been freed by then, whilst the southern side was still hidden under seventeenth- and eighteenth-century houses, so that it had never been possible to dig trial trenches through their foundations to ascertain if any part of the temple was preserved there. The demolition of the houses and the excavation under the modern ground level beginning from the south-west angle have fully satisfied our hopes. Five columns of the southern flank of the peristasis have appeared, preserved to a height of over 2 metres, with the stylobate beneath them (Fig. 1): only the angle column had been destroyed during the building of the walls of the Spanish barracks. The cella is equally well preserved, and a third of its total length has already been liberated, although the work is in temporary suspense owing to unsettled disputes with the owners of the houses. The southern flank of the archaic Syracusan temple appears to be in much better condition than the others.

Prehistoric Roads and Tracks in Somerset, England: 2. Neolithic

1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
Extensive Region ◽  
Peat Deposits ◽  
Third Millennium ◽  
South West England

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).

Athens Honours Proxenos (IG i2. 146)

1974 ◽  
Vol 69 ◽  
pp. 295-298
Author(s):  
Michael B. Walbank
Keyword(s):  
West Coast ◽  
Fifth Century ◽  
Small Island ◽  
The South ◽  
The West ◽  
South West

This document is one of a number of Attic proxeny-decrees that A. G. Woodhead considered to be evidence for Athenian concern with the south-west Aegean towards the end of the fifth century B.C. He identified the honorand Proxenos as a native of Chalke, a small island off the west coast of Rhodes. I share the view of J. and L. Robert that Woodhead has not proved his case either for the date or for the ethnic.The inscription is non-stoichedon, its engraving inexpert and careless, with several mistakes untidily erased and corrected. There is a mixture of Attic and Ionic letter-forms in the first three lines (gamma, eta, and lambda are Ionic, while xi is written chi sigma); otherwise the lettering is Attic, indicating a date before 403 B.C.

Population and Habitat Selection of the Noisy Scrub-bird, Atrichornis clamosus, 1962-83

1985 ◽  
Vol 12 (3) ◽  
pp. 479 ◽  
Author(s):  
GT Smith
Keyword(s):  
Habitat Selection ◽  
Incomplete Data ◽  
The South ◽  
The West ◽  
Population Index ◽  
South West ◽  
Number Of Males ◽  
Selection Of

The noisy scrub-bird Atrichornis clamosus at Two Peoples Bay was censused, the number of singing males being used as the population index. Incomplete data from 1962 to 1968 suggest that the number of males varied from 40 to 50 during this period. The first rigorous census found 45 males in 1970 and this number increased to 138 in 1983. The most likely reason for this increase is the absence of fire from the area since 1970. Since 1975 the population has expanded out of its headland stronghold to the south-west of Two Peoples Bay to form a subpopulation around Lake Gardner that is well separated from the headland population by roads, firebreaks and a strip of control burnt blocks. The growth of this subpopulation has added a further safeguard to the population. Observations on the vegetation formations (heath, thicket, low forest A and low forest B) used by male noisy scrub-birds on the headland indicate that most of the best habitat (low forest B) is occupied and that an increasing number of males are occupying suboptimal habitat (heath and thicket). There is sufficiently good habitat to the west of Lake Gardner to allow at least 30 additional males to live in the area.

Forest Dialect

English Today ◽  
2020 ◽  
Vol 36 (3) ◽  
pp. 70-76
Author(s):  
Michelle Straw
Keyword(s):  
Identity Construction ◽  
Nation State ◽  
The South ◽  
The West ◽  
South West ◽  
Special Place ◽  
West Midlands ◽  
National Borders

The Forest of Dean (henceforth Forest) is one of the lesser known English Royal Forests. The area is considered locally to be a special place with a distinctive dialect. The Forest lies at the intersection of three regions: South East Wales, West Country, also known as the South West, and the West Midlands. The Forest is situated between two rivers: the River Severn to the East separates it from the rest of Gloucestershire; the River Wye to the West separates it from Wales. National borders and physical boundaries seem to play an important role in identity construction. ‘Identities matter most’ (Llamas & Watt, 2010: 17) to those communities ‘at the physical margins of the nation state’ (Llamas, 2010: 225). Such communities may engage in practices that differentiate their dialect and situate it at the centre of their own region.

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