VII.—Notgrove Long Barrow, Gloucestershire

Archaeologia ◽  
1937 ◽  
Vol 86 ◽  
pp. 119-161 ◽  
Author(s):  
Elsie Margaret Clifford
Keyword(s):  
Northern Boundary ◽  
Ordnance Survey ◽  
North West ◽  
The Road ◽  
The North ◽  
The Village

The Long Barrow lies one mile north-west of the village close to the northern boundary and near the north-west corner of the parish of Notgrove, Gloucestershire. It is situated in a field called ‘Poors' lot’, or ‘Poors' allotment’, by the road from Cheltenham to Bourton-on-the-Water, and is about a quarter of a mile east from Notgrove G.W.R. Station. It is one of the Cotswold long barrows of which there are two others about two miles away, while the Swell group is only four and a half miles distant. It is marked as the remains of a long barrow on the 6-in. Ordnance Survey, Gloucestershire XXVIII. 10, latitude 51° 53′ 20″, longitude 1° 51′ 40″.

Excavation of a homestead of the Roman era at Halangy Down, St. Mary's, Isles of Scilly, 1950

1955 ◽  
Vol 35 (3-4) ◽  
pp. 187-198 ◽  
Author(s):  
Paul Ashbee
Keyword(s):  
Material Culture ◽  
Ordnance Survey ◽  
North West ◽  
North East ◽  
The North ◽  
South West ◽  
West Part ◽  
Neighbouring Island ◽  
The Hill ◽  
The Village

Halangy Down (fig. 1) is the lower precipitous slope of the decline from Telegraph Hill (Ordnance Survey B.M. 166. 3 ft.) to the sea at Halangy Porth and Point. Halangy Down and the earlier chambered tomb upon the crest are often referred to locally as ‘Bants Carn’. The true ‘Bants Carn’ is a considerable rock outcrop dominating Halangy Point. This escarpment faces Crow Sound, which separates the north-west part of St. Mary's from the neighbouring island of Tresco. The hill-side is sheltered by the mass of Telegraph Hill from inclement weather from the north-east and east, but is fully exposed to the south-west and west.The existence of an ancient village site here has long been known in the islands. At the close of the last century, the late Alexander Gibson cleared away the underbrush from one of the more prominent huts and made a photographic record of its construction. Shortly after, the late G. Bonsor, of Mairena del Alcor, near Seville, in addition to excavating the chambered tomb, noted a considerable midden together with traces, of prehistoric occupation exposed in the cliffs of Halangy Porth just below the village site. Dr. H. O'Neill Hencken noted Bonsor's description of the midden, and, as nothing was known at the time of the material culture of the ‘village’, he associated the two.

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.

Akeman Street and the River Cherwell

1929 ◽  
Vol 9 (1) ◽  
pp. 30-34
Author(s):  
B. H. St. J. O'Neil
Keyword(s):  
Fixed Points ◽  
The South ◽  
The West ◽  
Ordnance Survey ◽  
North West ◽  
The Road ◽  
The North ◽  
Straight Lines

The exact course of the Roman road called Akeman Street in the neighbourhood of the river Cherwell, some 9 miles north of Oxford, for a distance of a little over a mile, has long remained uncertain. The road is traceable from the west as far as the south-east corner of Tackley Park, and from the east as far as the north-west corner of Kirtlington Park. Between these two fixed points the road is, conjecturally, marked on the Ordnance Survey map merely by two parallel dotted straight lines, drawn with the aid of a ruler.

Excavations at Caerau Ancient Village, Clynnog, Caernarvonshire, 1933 and 1934

1936 ◽  
Vol 16 (3) ◽  
pp. 295-320 ◽  
Author(s):  
B. H. St. J. O'Neil
Keyword(s):  
Large Area ◽  
Mountain Slope ◽  
Ordnance Survey ◽  
North West ◽  
The Road ◽  
The North ◽  
Excellent Preservation ◽  
A Site ◽  
North And South ◽  
Agricultural Settlement

Mynydd Craig-goch, the westernmost height of a rocky ridge of the Snowdon mountains, slopes gently down to a watershed at the head of the Afon Dwyfach, over which run the railway and the main road from Criccieth and Portmadoc to Caernarvon. Between the ninth and tenth milestones from Caernarvon, immediately to the east of the road and thus on the lowest part of the mountain slope, there lie the remains of a most extensive primitive agricultural settlement. It is not marked on the Ordnance Survey map (6 in. 26 NE.), but was known locally, and the farm within which most of it lies bears the significant name Caerau. Its recognition as a site of great possibilities on account of its excellent state of preservation is due to Mr. W. J. Hemp, F.S.A. The settlement must originally have extended north and south for a distance of about half a mile. It may, indeed, have been contiguous with other settlements on the north and north-west, thus forming part of a large area of cultivated land, since there exists in excellent preservation a house or hut-group of the same type with at least one typical field about one mile to the west on the farm of Cefn Graianog. This point, however, cannot now be determined on account of more recent agricultural developments around the farm of Bodychain.

Matronianus, Comes Isauriae: an Inscription from an Early Byzantine Basilica at Yanıkhan, Rough Cilicia

1985 ◽  
Vol 35 ◽  
pp. 93-97 ◽  
Author(s):  
Stephen Hill
Keyword(s):  
The South ◽  
Late Professor ◽  
The Road ◽  
Scrub Oak ◽  
The North ◽  
Wild Olive ◽  
On The Road ◽  
Olive Trees ◽  
The Village ◽  
Early Byzantine

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.

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.

The Making of the Himalaya, Karakoram, and Tibetan Plateau

2013 ◽  
Author(s):  
Mike Searle
Keyword(s):  
Tibetan Plateau ◽  
Plate Boundary ◽  
Indian Plate ◽  
North West ◽  
Geological Interpretation ◽  
Mountain Ranges ◽  
The Road ◽  
The North ◽  
On The Road ◽  
The Himalaya

My quest to figure out how the great mountain ranges of Asia, the Himalaya, Karakoram, and Tibetan Plateau were formed has thus far lasted over thirty years from my first glimpse of those wonderful snowy mountains of the Kulu Himalaya in India, peering out of that swaying Indian bus on the road to Manali. It has taken me on a journey from the Hindu Kush and Pamir Ranges along the North-West Frontier of Pakistan with Afghanistan through the Karakoram and along the Himalaya across India, Nepal, Sikkim, and Bhutan and, of course, the great high plateau of Tibet. During the latter decade I have extended these studies eastwards throughout South East Asia and followed the Indian plate boundary all the way east to the Andaman Islands, Sumatra, and Java in Indonesia. There were, of course, numerous geologists who had ventured into the great ranges over the previous hundred years or more and whose findings are scattered throughout the archives of the Survey of India. These were largely descriptive and provided invaluable ground-truth for the surge in models that were proposed to explain the Himalaya and Tibet. When I first started working in the Himalaya there were very few field constraints and only a handful of pioneering geologists had actually made any geological maps. The notable few included Rashid Khan Tahirkheli in Kohistan, D. N. Wadia in parts of the Indian Himalaya, Ardito Desio in the Karakoram, Augusto Gansser in India and Bhutan, Pierre Bordet in Makalu, Michel Colchen, Patrick LeFort, and Arnaud Pêcher in central Nepal. Maps are the starting point for any geological interpretation and mapping should always remain the most important building block for geology. I was extremely lucky that about the time I started working in the Himalaya enormous advances in almost all aspects of geology were happening at a rapid pace. It was the perfect time to start a large project trying to work out all the various geological processes that were in play in forming the great mountain ranges of Asia. Satellite technology suddenly opened up a whole new picture of the Earth from the early Landsat images to the new Google Earth images.

scholarly journals XXXVI. An account of the effects of lightening at South Weald, in Essex

1764 ◽  
Vol 54 ◽  
pp. 198-200
Keyword(s):  
The West ◽  
North West ◽  
The Road ◽  
The North ◽  
Neighbouring Country ◽  
The Church

South Weald is a village in Essex, about eighteen miles distant from London, and two to the north west of Brentwood. In the road from London there is an almost continual ascent for the last four or five miles, which makes a considerable eminence above any parts of the neighbouring country. On the highest part of it stands the church, which has at the west end a tower, and in one corner of this there is a round turret, being a continuation of the stair-case, about four feet wide, eight feet high, and the walls of it one foot thick. In the top of the wall of this turret, which was leaded, are fixed several iron bars, that are bent so as to meet in the middle and support a weather-cock, which was put up about sixteen years ago.

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.

I.—Belgic and Roman Silchester: the Excavations of 1954–8 with an Excursus on the Early History of Calleva

Archaeologia ◽  
1969 ◽  
Vol 102 ◽  
pp. 1-81 ◽  
Author(s):  
George C. Boon
Keyword(s):  
Field Work ◽  
Early History ◽  
Total Evidence ◽  
The South ◽  
Public And Private ◽  
Ordnance Survey ◽  
North West ◽  
The North ◽  
History Of

SummaryThe excavations were undertaken by the Silchester Excavation Committee supported by donations from public and private bodies and from individuals and by permission of the Duke of Wellington, K.G., F.S.A. Their purpose was the investigation of (a) a previously unsuspected polygonal enclosure of about 85 acres, here named the Inner Earthwork, which lay partly inside and partly outside the line of the familiar Roman town wall; and (b) a western extension to the known line of the Outer Earthwork, which increased the size of this enclosure from about 213 to 233 acres. With the assistance of the Ordnance Survey, the aerial traces of these earthworks, first observed and recorded by Dr. J. K. St. Joseph, F.S.A., were confirmed and extended by field-work and excavation, and have been planned as appears on pl. I.The excavations showed that the Inner Earthwork was a defence of Gaulish ‘Fécamp’ type, and that it was erected, on the south, over an area of late pre-Roman occupation, the first clearly identified at Calleva Atrebatum, but one with strong ‘Catuvellaunian’ influences in its pottery-series. It is claimed that the Inner Earthwork was constructed by the client King Cogidubnus in or shortly after A.D. 43–4, as the defence of this, the most important settlement in the north-west of his dominions. It is further suggested that the Inner Earthwork was replaced by the Outer Earthwork also during the reign of Cogidubnus.The excursus attempts to collate with the results of excavation the earlier discoveries of pre-Conquest material. The total evidence is finally related to the Belgico-Roman topography of Silchester and its neighbourhood, within the historical framework of the century and a half which separated the arrival of the earliest Belgic immigrants in the region from the death of Cogidubnus and the consequent emergence of the Roman Civitas Atrebatum.

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