A Hellenic Fortification Tower on the Kefala Ridge at Knossos

1957 ◽  
Vol 52 ◽  
pp. 224-230
Author(s):  
Sinclair Hood ◽  
John Boardman
Keyword(s):  
First Year ◽  
The West ◽  
North West ◽  
High Bank ◽  
The Hill

In the course of a search for tombs in the Knossos area during the spring of 1951 I noticed some large blocks of limestone masonry with curved edges that had just been removed from a newly planted vineyard, the property of Georgios Kargatzes, near the top of the hill forming the southern end of the long ridge on the northern tip of which stands the Isopata Royal Tomb. The site is about 250 metres north-west of the Zafer Papoura cemetery of Late Minoan tombs dug by Evans in 1904, and at the bottom of the slope to the west is a high bank with important Geometric tombs (Knossos Survey 15), explored by Hogarth during the first year of the excavations at Knossos in 1900.The curving blocks, together with the situation on the top of a hill less than half a kilometre south of the Kefala tholos tomb (Knossos Survey 8), excavated by Mr. R. W. Hutchinson in 1939, immediately raised hopes that another tholos tomb might await discovery here; and the fragments of Minoan pottery everywhere on and below the surface encouraged this belief. Dr. N. Platon, Ephor of Antiquities for Crete, visited the site and granted permission for the School to make trials to discover from what the blocks came. The Director of the School, Mr. J. M. Cook, gave his sanction for the work and asked me to undertake it. The plans were drawn by Mr. Piet de Jong, then the School's Curator at Knossos; the drawings of the vases are by Miss Susan Wood.

An Iron Age A site on the Chilterns

1951 ◽  
Vol 31 (3-4) ◽  
pp. 132-148 ◽  
Author(s):  
K. M. Richardson ◽  
Alison Young
Keyword(s):  
Water Supply ◽  
Iron Age ◽  
The West ◽  
North West ◽  
The North ◽  
Roman Villa ◽  
Adjoining Area ◽  
Cursory Examination ◽  
A Site ◽  
The Hill

In 1946 a visit to the barrow, which lies on the edge of the western scarp of Chinnor Common, and a cursory examination of the adjoining area, cultivated during the war, resulted in finds of pottery and other objects indicating Iron Age occupation. The site lies on the saddleback of a Chiltern headland, at a height of about 800 ft. O.D. Two hollow ways traverse the western scarp, giving access to the area from the Upper Icknield Way, which contours the foot of the hill, then drops to cross the valley, passing some 600 yards to the north of the Iron Age site of Lodge Hill, Bledlow, and rising again continues northwards under Pulpit Hill camp and the Ellesborough Iron Age pits below Coombe Hill. The outlook across the Oxford plain to the west is extensive, embracing the hill-fort of Sinodun, clearly visible some fourteen miles distant on the farther bank of the Thames. The hollow way at the north-west end of the site leads down to a group of ‘rises’ hard by the remains of a Roman villa, and these springs are, at the present day, the nearest water-supply to the site.

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.

New Evidence Concerning the Original Order of Deposition of the Longmyndian Rocks

1948 ◽  
Vol 85 (2) ◽  
pp. 107-109 ◽  
Author(s):  
John Challinor
Keyword(s):  
Coarse Grained ◽  
The West ◽  
North West ◽  
The Road ◽  
Fine Grained ◽  
Original Order ◽  
The North ◽  
The Hill ◽  
New Evidence ◽  
The Village

During the war a large new quarry was opened in the Longmyndian rocks of Haughmond Hill, Shropshire. It is near the south-east edge of the hill, to the west of the road running north from Upton Magna and one mile from the village. On the sketch-map in the Shrewsbury Memoir (p. 58) two arrows are shown, at about this locality, recording dips of 50° in a south-easterly direction. I was told that there was a very small quarry here before the large quarry was excavated. The present quarry is even larger than that near Haughmond Abbey (Shrewsbury Memoir, p. 48), on the north-west side of the Pre-Cambrian outcrop, and the two quarries offer extensive and splendidly displayed exposures of Longmyndian rocks, one in the coarse-grained Western Longmyndian and the other in the fine-grained Eastern Longmyndian.

An Iron Age Hill-Fort at Grimthorpe, Yorkshire, England

1969 ◽  
Vol 34 ◽  
pp. 148-190 ◽  
Author(s):  
I. M. Stead ◽  
M. Jarman ◽  
Angela Fagg ◽  
E. S. Higgs ◽  
C. B. Denston
Keyword(s):  
Iron Age ◽  
The South ◽  
The West ◽  
Circular Area ◽  
North West ◽  
The North ◽  
South West ◽  
White Horse ◽  
The Hill ◽  
Grave Goods

The Iron Age hill-fort at Grimthorpe (Grid reference SE.816535) in the parish of Millington, East Riding of Yorkshire, is on the western edge of the Yorkshire Wolds, with a commanding position over the Vale of York. There is an uninterrupted view to the White Horse on the Hambleton Hills, 25 miles to the north-west; beyond York, 13 miles to the west, to the Pennines; and to the south 25 miles to the chimneys of Keadby and Scunthorpe. To the west and south the land slopes away to the Vale of York, and to the north and east there is a sharper fall to Given Dale and Whitekeld Dale. The hill-fort defences follow the 520 feet contour, and enclose an approximately circular area of eight acres (fig. 1).A traditional reference may be preserved in the field-name—Bruffs—perhaps a variation of ‘Brough’, which ‘refers in all cases to ancient camps, usually Roman ones’. But all surface indications have now been obliterated by ploughing, and even a century ago there was little more to be seen. John Phillips in 1853 noticed ‘unmistakable traces of ancient but unascertainable occupation’, and in 1871 an excavation by J. R. Mortimer located ‘the filled up inner ditch of a supposed camp’. But Mortimer was not concerned with the settlement; his interest had been aroused by the discovery, in 1868, of a burial with rich grave-goods, including metalwork with La Tène ornament, in a chalk-pit within the south-west sector of the hill-fort.

scholarly journals II.—On the Cudgegong Diamond Field, New South Wales

1879 ◽  
Vol 6 (10) ◽  
pp. 444-458
Author(s):  
Norman Taylor ◽  
R. Etheridge
Keyword(s):  
New South ◽  
The West ◽  
North West ◽  
The North ◽  
North Side ◽  
South Wales ◽  
Northern Half ◽  
Southern Half ◽  
Extreme North ◽  
The Hill

The next appearance of the older lead is at the “Rocky-ridge,” where the river, after running northerly for three-quarters of a mile, along the strike of the metamorphic beds, turns abruptly to the west. This ridge is a basalt-capped hill on the north side of the river, running in a north-west direction; it is about a mile long, with a bold rocky escarpment on its west side, facing the Sandy or Cudgebeyong Creek. Some tunnels have been driven in, and shafts sunk on this hill, and tolerably rich deposits of gold were found, but never followed out.Only in the southern half of the hill have diamonds been found(all more or less spotted).The drift is remark-able for the number and size of the agates it contains.The northern half of “the ridge” is underlaid by another outlier of the before-mentioned doubtful purple conglomerate, into which some tunnels have been driven in the western escarpment.The basalt is merely a fringe here, resting against the flank of the conglomerate, in which a small quantity of nuggetty gold was obtained;and form one to two inches thickness of lignite, or carbonaceous clay, is seen between it and the bottom of the basalt. Tte basali is intersected by numerous veins of a mineral allied to kaolin. The purple con-glomerate is similar in character to that near “the flat”and contains, on some of the joint faces, smll spherical crystalline aggreations of chalybite(carbonate of iron).At the extreme north ead of “the ridge”are great quantities of ironstone and conglomerate, but, from their Carbpniferous series, which is largely developed further north.The first diamonds which found their way to Melbourne were obtained.

scholarly journals Le Bosquet del Vau un établissement du néolithique final

2022 ◽  
Author(s):  
heller frederic
Keyword(s):  
Bronze Age ◽  
Late Neolithic ◽  
The West ◽  
North West ◽  
Northern Side ◽  
Western Side ◽  
The One ◽  
The Hill ◽  
Steep Slopes ◽  
Made In

Summary:The Neolithic site of the Bosquet del Vau is located in the Brabant Province in Belgium. Two different rescue excavations took place on the site both in 2006 and 2007 : the first was subsequent to a housing project of about 110 houses, the latter to the building of the R.E.R. (Express Regional Transportation System).The site was discovered in the 1980 by a group of three teenagers going flint tools hunting all around Waterloo and Braine l’Alleud. Flint tools pertaining to the Late Neolithic and Early Bronze Age were recovered on site as well as some Mesolithic flint tools.The site is located on a small sandy hill and covers 2.5 hectares. Steep slopes surround it to the west and north-west and gentler ones to the northeast and south, an isthmus exists to the east linking it o the plateau.The settlement is protected by a palisade to the east and south, a wide ditch links the palisade to the nearly valley to the west. The western side of the hill has seen its slope artificially steepened as did part of the northern side. No palisade was found on either of those two sides.Part of one house and a complete second one were discovered in 2006 and 2007. They are aligned north to south, 18 meters long and 4.5 meters wide. A narrow ditch houses the post holes, posts are maximum 0.30 m in diameter and spaced evenly. Central posts suggest a two-sloped roof. No hearth was found inside of the first house, the one of the second has yet to be associated with the house.A phosphate map was made in both cases, evidence points to a house divided into three parts, with maybe a cattle area next to the second one.Potsherds recovered in two postholes of the 2007 house fit together and could be dated to the Late Neolithic Period.Flint tools are mostly micro-denticulates though a few polished axes fragments have been discovered as well as arrowheads and a beautifully knapped flint knife.The various types of stones used: from black flintstone to Parisian flintstone and phtanite suggest here again a Late-Neolithic dating.

Nemesis: A Mycenaean settlement near the Menidi Tholos Tomb

1959 ◽  
Vol 53 ◽  
pp. 292-294
Author(s):  
R. Hope Simpson
Keyword(s):  
Ground Level ◽  
The West ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
Original Size ◽  
The Hill ◽  
East West ◽  
Ancient Remains

The site to be described lies on a low hill a little to the north of the small village or suburb of Nemesis, about 150 metres to the west of the main road from Patisia to Koukouvaounes, and 1 kilometre to east-south-east of the Mycenaean tholos tomb at Λυκὸτρυπα, which was excavated by the German Institute in 1879, and is usually called the Menidi Tomb. The site at Nemesis is visible from the tholos tomb, and is separated from it by a gentle valley through which run, in a southerly direction, two streams with steep banks. The eastern stream is the river Kephissos, whose name goes back at least as far as the classical period.The hill of Nemesis stands about 15 to 20 metres above the level of the surrounding land, and measures about 160 m. north-west to south-east × 120 m. north-east to south-west. The hill is an isolated outcrop of conglomerate rock, thinly covered with stony brown earth. It has been eroded over an area about 250 m. north-south × 50 m. east-west, so that its original size was considerably larger than at present, in all about 30,000 square metres. Mycenaean sherds were found over the whole of this area, though mainly in the eroded part, among the lumps of fallen earth and rock. Remains of rubble walling together with several Mycenaean sherds were found here, and also in the steep cliffs formed by the erosion on the west and south sides (this part of the hill has been undermined by recent excavation of the beds of grey clay, which here lie at between 2 and 3 metres below the original ground level). The ancient remains are particularly noticeable in the south-west angle of the cliffs (roughly in the centre of the part of the hill shown on Plate 71a), where there is a greater depth of earth above the rock than is visible elsewhere on the hill.

Excavations on Pilsdon Pen, Dorset, 1964–71

1977 ◽  
Vol 43 ◽  
pp. 263-286 ◽  
Author(s):  
Peter S. Gelling
Keyword(s):  
Natural History ◽  
Iron Age ◽  
The South ◽  
The West ◽  
North West ◽  
The North ◽  
Nearest Point ◽  
Daunting Task ◽  
East End ◽  
The Hill

Pilsdon Pen is in west Dorset, very close to the Devon border, some 6 miles north-west of Bridport, and about 5½ miles from the nearest point of the coast (ST 413013). It is a long flat-topped hill, the highest in Dorset, reaching 908 ft above OD, and dominating Marshwood Vale from the north. The hill-fort occupies the south-east end of the Pen, at the north-west end of which there is a small embanked enclosure, much levelled by ploughing, which could be of Iron Age date also. The two nearest hill-forts are Lambert's Castle and Coneys Castle, about 3 and 3½ miles away respectively, which overlook Marshwood Vale from the west (fig. 1).Excavation began in 1964, and continued annually until 1971, all but one of the seasons lasting four weeks. The work was initiated, and largely supported, by the owner of the site, Mr Michael Pinney, of Bettiscombe Manor, to whom archaeology owes a great debt. Mrs Betty Pinney was one of our most skilful excavators, and all those who took part will remember her hospitality. Financial help was also given by the Dorset Natural History and Archaeological Society and by Birmingham University. Among many helpers, to all of whom I am most grateful, I should like to mention in particular my wife, who shouldered the daunting task of keeping the camp supplied, and Mr Jack Wells, of Tanyard Farm, Marshwood, without whose regular assistance the excavation would have taken much longer, and cost a great deal more.

VIII.—The Soils and Vegetation of the Bin and Clashindarroch Forests

1941 ◽  
Vol 60 (1) ◽  
pp. 233-341 ◽  
Author(s):  
A. Muir ◽  
G. K. Fraser ◽  
H. M. Steven
Keyword(s):  
Rough Boundary ◽  
The South ◽  
The West ◽  
North West ◽  
The North ◽  
The Hill

The Bin and Clashindarroch Forests lie some 40 miles to the north-west of Aberdeen. Clashindarroch Forest, the larger of the two, stretches from the Rhynie-Cabrach road in the south almost to the Huntly–Glass road in the north. The Bogie valley in the east forms another rough boundary for the hill mass that the forest occupies. On the west the area marches with the county boundary. The Bin Forest consists of two main sections—the Bin itself to the north-west of Huntly, and the Balloch which lies between Keith and Grange, being partly in Banffshire. Both of these areas are more or less isolated hills.

SMALL BOWEL CAPSULE ENDOSCOPY IN THE WEST OF IRELAND: A CLOSER LOOK AT THE FIRST YEAR

2020 ◽  
Author(s):  
H O’Donovan ◽  
H Yousuf ◽  
D Gallagher ◽  
C Goulding
Keyword(s):  
Small Bowel ◽  
Capsule Endoscopy ◽  
First Year ◽  
The West ◽  
West Of Ireland
Sign in / Sign up

Export Citation Format

Share Document