scholarly journals XX. Account of the Remains of a Roman Villa, discovered at Bignor, in Sussex, in the Years 1811, 1812, 1813, 1814, and 1815. By Samuel Lysons, Esq. V.P. F.R.S.

Archaeologia ◽  
1817 ◽  
Vol 18 ◽  
pp. 203-221 ◽  
Author(s):  
Samuel Lysons
Keyword(s):  
The South ◽  
The North ◽  
Roman Villa ◽  
North Side ◽  
The Common ◽  
The Village ◽  
The Town ◽  
The Church ◽  
Common Field

The village of Bignor, in Sussex, is pleasantly situated on the north side of the South Downs, at the distance of about nine miles from the sea, six miles from Petworth, and about the same distance from Arundel. Within half a mile of the village runs a Roman road very distinctly marked, leading from Chichester by way of Pulborough (where it crosses the river Arun) to Dorking, and from thence to London. On this road there was great reason to expect some traces of a Roman station about Bignor, as Richard of Cirencester, in his fifteenth Iter, next after Regnum, proceeding eastward, introduces a station which he terms “Ad decimum,” not noticed in the Itinerary of Antonine; and Bignor is, by the Roman road, about ten miles disstant from Chichester, the Regnum of the Romans. No Roman remains had however been noticed near this place till the year 1811, when a mosaic pavement was discovered by the plough in the month of July, in a field called the Deny, about a quarter of a mile east of the church, part of a copyhold estate held under the Earl of Newburgh by Mr. George Tupper, a respectable farmer, by whom it is also occupied. The inhabitants of the village have a tradition, that Bignor formerly stood in this field, and the common field adjoining, on the east, called the Town-Field.

Epitaphic Nation: The Problem of the South and Necropolitics in Early Modern Vietnamese National Literature

PMLA ◽  
2011 ◽  
Vol 126 (3) ◽  
pp. 685-692
Author(s):  
Nguyễn-Võ Thu-Hương
Keyword(s):  
Early Modern ◽  
Literary History ◽  
State Violence ◽  
The South ◽  
The North ◽  
Literary Genealogy ◽  
The Republic ◽  
The Village ◽  
North And South ◽  
The Church

Whoever goes down to Bà Ria and happens by the cemetery in the sand at the village of Phu'ó'c Lě, I beg you to go in that cemetery and look for the grave with a cross painted half black, half white, by the side of the Church of Martyrs–to visit that grave lest it become pitiful. Because it has been two years since anyone visited or cast as much as a glance.—Nguyễn Trong QuanSO opens nguyễn trọng quản's thẩy lazaro phiển (“lazaro phiển” 22). The narrative begins at an obscure gravesite evokes the life of a man as both victim of state violence and perpetrator of private deaths. Lazaro Phiển is a ictional work written in the romanized script and was published in Saigon in 1887 in a novelistic format almost forty years before Hoàng Ngọc Phách's Tố Tâm. Yet the latter, published in Hanoi in 1925, is oten touted in official literary history as the first modern Vietnamese novel. Although Nguyễn Trọng Qu.n's narrative revolves around the recovery of an elided story, the author could not have anticipated the elision of his work from a nationalist literary genealogy that locates the origin of modern Vietnamese literature in the North. he elision was part of a general omission of works from the South in the last decades of the nineteenth century and irst two decades of the twentieth. his genealogy was by no means limited to the Democratic Republic of Vietnam in the North but was also perpetuated in the Republic of Vietnam in the South ater independence and the partitioning of the country into North and South in 1954

scholarly journals XV.—The Alien Priority of St. Andrew, Hamble and its transfer to Winchester College in 1391

Archaeologia ◽  
1887 ◽  
Vol 50 (2) ◽  
pp. 251-262
Author(s):  
Thomas F. Kirby
Keyword(s):  
Fifteenth Century ◽  
The South ◽  
Southampton Water ◽  
Parish Church ◽  
The North ◽  
North Side ◽  
South West ◽  
A Cell ◽  
The Church

The Priory of St. Andrew, at Hamble, near Southampton, was a cell to the Benedictine abbey of Tyrone (Tirun or Turun), in La Beauce, a district southwest of Chartres, included in the old province of Orléannois. In the Monasticon and Tanner's Notitia it is called a Cistercian abbey, but this is a mistake, and so is the statement in the Notitia that the priory was annexed to New College, Oxford. The priory stood on a “rise” or point of land.—“Hamele-en-le-rys” or “Hamblerice” is its old name—at the confluence of the Hamble river with southampton Water, opposite Calshot castle. Hamble gets its name from Hamele, a thane of the Saxon Meonwaris. Leland calls the place “Hamel Hooke.” The priory church of St. Andrew is now the parish church. It was rebuilt by winchester college in the early part of the fifteenth century, and consists of channel and nave, to which a south aisle was added five or six years ago, and a tower with three bells. There are scarcely any traces above ground of the priory buildings. Like those of the Benedictine convent of St. Swithun, at Winchester, they stood on the south and south-west of the church, so that the graveyard, as at Winchester, is on the north side of the church.

scholarly journals IV.—The Geology of the Dolgelley Gold-belt, North Wales

1910 ◽  
Vol 7 (4) ◽  
pp. 159-171 ◽  
Author(s):  
Arthur R. Andrew
Keyword(s):  
The South ◽  
Ordnance Survey ◽  
Gold Mines ◽  
South Eastern ◽  
North East ◽  
The North ◽  
North Side ◽  
North Wales ◽  
The Town ◽  
Gold Bearing

The town of Dolgelley lies slightly outside the main tract of gold-bearing country of Merionethshire, but it forms a convenient headquarters from which to visit the various gold-mines and auriferous lodes. The Dolgelley Gold-belt lies within the area covered by the quarter-sheets 27 N.E., 27 S.E., 32 S.E., 33 N.W., 33 N.E., 33 S.W., 36 N.W., 36 N.E. of the 6 inch Ordnance Survey maps of Merionethshire. It is on the north side of the estuary of the Mawddach, extending from the sea at Barmouth to the locality of Gwynfynydd on the north-east. The belt forms the south-eastern flank of a range of high ground sloping down to the south and south-east from the mountains of Rhinog, Diphwys, and Garn. It is drained by several tributaries of the Mawddach, of which the principal are the Afons Hirgwm, Cwm-llechen, Cwm-mynach, Wnion, Las, Gamlan, Eden, and Gain.

II.—The Ice-Avalanche on the Gemmi Pass (Switzerland)

1896 ◽  
Vol 3 (3) ◽  
pp. 103-106
Author(s):  
C. S. Du Riche Preller
Keyword(s):  
Central Alps ◽  
The North ◽  
North Side ◽  
Alpine Glaciers ◽  
Rhone Valley ◽  
The Village ◽  
The Town ◽  
Ice Avalanche

It is a noteworthy fact that, although Alpine glaciers have, during the last few years, not shown any very marked oscillations, the Central Alps have, since the year 1892, been annually visited by a disaster caused, directly or indirectly, by the bursting or falling of a glacier. Thus, in 1892, the Tête Rousse glacier of the Mont Blanc group swept away the Baths of St. Gervais; in 1893, the village of Taesch, between Viess and Zermatt, was devastated by the torrent of the Weingarten glacier, not far from the village of Randa, which was destroyed by a glacier avalanche in the year 1819; again, in 1894, the torrent of the Crête glacier (Grand Combin group, Rhone valley) suddenly poured its flood into the river Dranse, and thereby endangered the town of Martigny; while last year the record was swelled by the avalanche of the Altels glacier on the north side of the Gemmi Pass, in the Bernese Oberland.

scholarly journals Notes and Inscriptions from Pamphylia

1911 ◽  
Vol 17 ◽  
pp. 215-249
Author(s):  
H. A. Ormerod ◽  
E. S. G. Robinson
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The North ◽  
Great Rivers ◽  
Short Time ◽  
The Village ◽  
The Town

The following notes were made by us on a short journey in Pamphylia during March 1911.It had been our intention on reaching Adalia about the middle of the month to go at once into Lycia, but the lateness of the season made the higher ground impossible, and it seemed better to spend a short time in examining the country in the immediate neighbourhood of Adalia, much of which was still imperfectly known (Fig. 1).The best description of the Pamphylian plain is that given by Lanckoronski. From the Kestros to the Melas stretches a low-lying, swampy plain, traversed by three great rivers which come down from the Pisidian highlands, feverish in summer, and during the winter months impossible for wheeled traffic. To the west of the Kestros rises a rocky plateau of travertine some hundred feet above sea-level, on which stands the town of Adalia (Attaleia) on cliffs above the sea, which diminish towards the west. To the north of Adalia rises a third level, which viewed from the south, resembles a high raised beach, running roughly parallel with the present coast as far as the village of Barsak. To the east of that point the hills turn in a north-easterly direction and sink gradually down towards the Kestros. The western part of the plateau is crossed by two main roads, leading respectively to Istanoz and Buldur.

scholarly journals XXIII.—On the Position of the Portus Lemanis of the Romans

Archaeologia ◽  
1867 ◽  
Vol 40 (2) ◽  
pp. 361-374
Author(s):  
Thomas Lewin
Keyword(s):  
The South ◽  
The West ◽  
Historic Period ◽  
South Side ◽  
North East ◽  
The North ◽  
The Common ◽  
East And West ◽  
The Hill ◽  
The Village

The Portus Lemanis must clearly have been one of the great thoroughfares between Britain and the Continent, and it is not a little singular that the position of a port once so famous should never have been satisfactorily settled. The common impression is that it lay at the foot of Lymne Hill. For the benefit of those who are not familiar with this neighbourhood, I should mention, in limine, that the village of Lymne or Lympne stands about 2½ miles to the west of Hythe, on the highest part of the cliff which girds in the eastern portion of Romney Marsh. On the declivity of the hill, about half-way down, is seen the old Roman castrum, called Stuttfall, occupying 10 or 12 acres. There are walls on the north, east, and west, and the east and west walls run down to the marsh itself; but, what is remarkable, the south side towards the marsh had never any wall,” and hence the erroneous notion so generally prevalent that at the foot of the castrum was once the Portus Lemanis, and that in the course of ages the sea retired from Lymne, when the port shifted to West Hythe, and that the sea again retired, when the port was transferred to Hythe. I shall endeavour to show that these changes, if they ever occurred, must have preceded the historic period, and that in the time of the Romans, as for many centuries afterwards, the only port was Hythe. In fact Portus and Hythe are the same thing, Portus in Latin being Hyð in Saxon.

New Miocene Faunas from Cyprus

1932 ◽  
Vol 69 (11) ◽  
pp. 511-517 ◽  
Author(s):  
F. R. Cowper Reed
Keyword(s):  
Volcanic Rocks ◽  
The South ◽  
Ample Evidence ◽  
North West ◽  
Pillow Lavas ◽  
The North ◽  
North Side ◽  
Fossil Evidence ◽  
The Village

AN interesting collection of Tertiary fossils has recently been sent me for determination by Mr. C. P. Manglis, Manager of the Mitsero mines in Cyprus, who has collected them from the neighbourhood of these mines. Mitsero village stands near the head of a valley running down the north side of the Troodos mountains to the plains of Morphou and is described by Messrs. Cullis and Edge (1, p. 38) as standing on volcanic rocks close to the junction of the pillow-lavas with the overlying marls and limestones, while “ behind it is a bold sedimentary escarpment breached by the valley just mentioned and culminating in Koroni Mountain (2,140 feet), 1½ miles to the westnorth-west ”. The Koronia Limestone, the outcrop of which on the Evrykou road the author visited in 1929 (2, p. 443), occupies the top of the escarpment, as shown on a map sent to me by Mr. Manglis of the immediate district (scale, 1: 10,000) from the village of Kato Moni on the north-west to the village of Mitsero on the south-east. The position and age of the Koronia Limestone have been uncertain owing to the lack of definite fossil evidence, though the author (2a, p. 251) was inclined to put it in the Miocene rather than the Pliocene on the strength of a species of Cerithium which he discovered in it. The majority of the fossils in Mr. Manglis’s collection come from this limestone and provide ample evidence of its Miocene age.

A Romano-British Pottery Kiln at Weston Favell, near Northampton

1954 ◽  
Vol 34 (3-4) ◽  
pp. 218-224
Author(s):  
Brian Bunch ◽  
Philip Corder
Keyword(s):  
Raw Material ◽  
The South ◽  
North East ◽  
The North ◽  
North Side ◽  
Education Committee ◽  
Cherry Orchard ◽  
Pottery Kiln ◽  
The Village

The village of Weston Favell is situated on high land to the north of the river Nene, some 2½ miles to the north-east of the centre of Northampton. On the north side of the Wellingborough Road at this point the Northampton Education Committee are erecting the Cherry Orchard School. In April 1953, during the filling in of a disused quarry preparatory to building, one of the writers noticed sherds of Roman pottery in a disturbed patch in the quarry face (Nat. Grid 5237.2819). Further examination disclosed two large burnt stones protruding from it, which proved on excavation to be the cheeks of the stokehole flue of a small pottery kiln.The quarry was some 16 to 18 ft. deep, and had been used to get the local limestone. The field to the south of it shows disturbance of the surface over a considerable area. Overlying the stone hereabouts is an extensive layer of grey clay, which may well have served as the raw material of the potters. It contains pockets of whitish sand similar to that which gives the clay of the local ware its characteristic texture.

V.—An Anglo-Saxon Cemetery at Bidford-on-Avon, Warwickshire

Archaeologia ◽  
1923 ◽  
Vol 73 ◽  
pp. 89-116 ◽  
Author(s):  
John Humphreys ◽  
J.W. Ryland ◽  
E.A.B. Barnard ◽  
F.C. Wellstood ◽  
Thomas G. Barnett
Keyword(s):  
Anglo Saxon ◽  
The North ◽  
North Side ◽  
High Street ◽  
Western Border ◽  
A Site ◽  
The Village ◽  
The Church

In June 1921, during the cutting of a new road in the village of Bidford-on-Avon, Warwickshire, various articles were brought to light indicating an Anglo-Saxon cemetery. The excavation took place on a site at the back of the High Street, on the north side, in a gravel plateau about 100 yds. from the present bank of the river Avon, 150 yds. from the Roman Rycknild Street, and 200 yds. from the old ford, which lies to the east of the church. The site is on the extreme western border of Warwickshire, within a mile of the Worcestershire boundary.

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.

Sign in / Sign up

Export Citation Format

Share Document