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

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

Slovene ◽  
2016 ◽  
Vol 5 (2) ◽  
pp. 136-178
Author(s):  
Pasko Kuzman

Among the activities of St. Clement of Ohrid was the construction of the church and monastery in Ohrid, which was carried out at the end of the 9th century at the location where some Byzantine basilicas had stood previously. As findings of archaeological excavations have shown, St. Clement first built a small triconch church at the location of the ruined basilica. This triconchos was later expanded by the addition of a capacious “pronaos” in inscribed-cross form, where St. Clement was interred. This “pronaos” was characterized by entrances on the north and south sides that were identical to those of the inscribed-cross church that existed near the village of Velcë along the Šušica River (in southern Albania) at the turn of the 9th‒10th century. During the tenure of Archbishop Dmitrios Chomatianos (1216–1236), the “pronaos” was replaced with a new church into which the relics of St. Clement were placed. In the Ottoman period, the Church and Monastery of St. Clement were disassembled to build a mosque. At the very beginning of the 10th century, the triconchal church in the Monastery of St. Clement served as a model for the church in the Monastery of St. Naum, in the southern part of the Ohrid lake area. The groundwork(s) of a further church in a triconchal shape, whose construction can be traced back to the time of St. Clement, has also been discovered at Gorica, near Ohrid. Ruins of yet another triconchal church which also belongs to the period under review can be found near the village of Zlesti, in the Dolna Debarca region, not far from Ohrid. In the vicinity of the village of Izdeglavje, in the Gorna Debarca region, there is also a church whose establishment is related to the activity of St. Clement of Ohrid as well.


1909 ◽  
Vol 6 (11) ◽  
pp. 507-508
Author(s):  
F. R. Cowper Reed

The occurrence of a pre-Glacial marine terrace and raised beach along the coast of the south of Ireland was described by Messrs. Wright & Muff in 1904, and its development in the eastern part of co. Waterford was the subject of two short papers by the author in 1907 in this Magazine. Messrs. Wright & Muff (op. cit.) observed the same raised beach only in the south-eastern portion of co. Wexford, so that its recognition this summer by the author further north along the east coast of Ireland deserves recording, for it has been traced for several miles to the north and south of Courtown Harbour, and its height, characters, and relations to the overlying deposits show that it is a continuation of the same feature. The first locality to be mentioned is about 3 miles to the south of the village of Courtown, where relics of it are preserved between Roney Point and Salt Rock; it is still more distinct as a rock-terrace a little further north at Pollshone Head and Breanoge Head, but in the bays between these points the conditions are not favourable for its exposure, as there are no rocky cliffs, only extensive sand-dunes stretching along the shore. From Courtown Harbour northwards for about 2 miles to Duffcarrig Rocks sand-dunes are similarly developed, forming a nearly continuous line of ridges rising to heights of over 50 feet. Thick drift deposits occur behind them, but no pre-Glacial cliff or platform is exposed. At Duffcarrig Rocks solid rock again appears forming the headland, and we can recognize remnants of the rock-cut shelf in a much eroded and fissured condition.


Archaeologia ◽  
1882 ◽  
Vol 47 (1) ◽  
pp. 161-178
Author(s):  
Charles Edward Keyser

The village of South Ferriby is situate on the south bank of the Humber, and is the northernmost of a chain of small villages nearly all having names terminating in “by,” placed under or on the western escarpment of the Lincolnshire Wolds, where they approach the Humber, and overlook the valley through which flows the river Ancholme. The small parish church, dedicated to St. Nicholas, is chiefly deserving of notice on account of its peculiar situation and plan, and for the curious early Romanesque doorhead or tympanum shown by the accompanying illustration (Fig. 1). The church is built on a level platform cut out about half way up the hill. It consists of a nave standing north, and south, with a small chancel projecting eastward and considerably above the level of the nave, a low tower occupying the north-east angle between the nave and chancel, and a west porch opposite the chancel. Judging from some window tracery still remaining, the church seems to be of fourteenth century date, but it has been subjected to numerous alterations culminating in a restoration, in which the chancel has been converted into a vestry and the altar placed at the north end of the nave, which has been lengthened and made precisely like a barn in its general plan and arrangement. It is said that at one time there was a kind of western aisle formed by oak posts and struts supporting a beam, but no traces of this remain in the present renovated nave.


Archaeologia ◽  
1817 ◽  
Vol 18 ◽  
pp. 203-221 ◽  
Author(s):  
Samuel Lysons

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.


2019 ◽  
Author(s):  
Hamed D. Ibrahim

North and South Atlantic lateral volume exchange is a key component of the Atlantic Meridional Overturning Circulation (AMOC) embedded in Earth’s climate. Northward AMOC heat transport within this exchange mitigates the large heat loss to the atmosphere in the northern North Atlantic. Because of inadequate climate data, observational basin-scale studies of net interbasin exchange between the North and South Atlantic have been limited. Here ten independent climate datasets, five satellite-derived and five analyses, are synthesized to show that North and South Atlantic climatological net lateral volume exchange is partitioned into two seasonal regimes. From late-May to late-November, net lateral volume flux is from the North to the South Atlantic; whereas from late-November to late-May, net lateral volume flux is from the South to the North Atlantic. This climatological characterization offers a framework for assessing seasonal variations in these basins and provides a constraint for climate models that simulate AMOC dynamics.


Zootaxa ◽  
2020 ◽  
Vol 4758 (1) ◽  
pp. 45-82 ◽  
Author(s):  
L. LEE GRISMER ◽  
PERRY L. JR. WOOD ◽  
EVAN S. H. QUAH ◽  
MYINT KYAW THURA ◽  
JAMIE R. OAKS ◽  
...  

An integrative taxonomic analysis based on morphology, color pattern, and the mitochondrial gene ND2 recovered four new species of Hemiphyllodactylus Bleeker that are endemic to the Shan Plateau or Salween Basin in eastern Myanmar. Hemiphyllodactylus ngwelwini sp. nov. from the Shan Plateau is part of the earlier described “eastern Myanmar clade” renamed herein as the north lineage and H. kyaiktiyoensis sp. nov. and H. pinlaungensis sp. nov. of the Shan Plateau and H. zwegabinensis sp. nov. of the Salween Basin compose an entirely new Burmese clade herein referred to as the south lineage. Although the north and south lineages come within 46 km of one another on the Shan Plateau, they are not sister lineages but sequentially separated by two lineages from Yunnan, China and another from northwestern Thailand. Hemiphyllodactylus zwegabinensis sp. nov. is the first species of this genus to be recorded from the Salween Basin and is known only from a wind-blown cloud forest on the top of the insular, karstic mountain Zwegabin in Kayin State. All other Burmese species except for H. typus, are endemic to the various localities throughout the Shan Plateau. These four new species bring the total number of Hemiphyllodactylus in Myanmar to at least 10 which is certainly an extreme underestimate of the diversity of this genus given that we discover new species at every upland locality we survey. 


1985 ◽  
Vol 35 ◽  
pp. 93-97 ◽  
Author(s):  
Stephen Hill

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.


1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.


2019 ◽  
Vol 30 ◽  
pp. 97
Author(s):  
Luís Miguel Moreira

Resumen: La progresiva radicalización ideológica del régimen republicano, instaurado en Portugal en octubre de 1910, provocó una oposición conservadora y monárquica que se organizó en el exilio, sobre todo en el sur de Galicia. Entre octubre de 1911 y junio de 1912, estacionados en varios pueblos y villas gallegas en la raya con Portugal, los monárquicos hicieron dos incursiones en territorio portugués —el primero en Vinhais y el segundo en Chaves— con el fin de fomentar la rebelión contra régimen instaurado. Sin embargo, las tropas republicanas, más numerosas y mejor equipadas, vencieron todos los combates. En la época, este episodio de guerra civil mereció amplia cobertura periodística, particularmente por la prensa afecta al régimen republicano. Los mapas y las fotografías de la frontera fueron ampliamente utilizados para localizar e ilustrar los acontecimientos. En este texto, pretendemos reconstituir estos movimientos, proponiendo una lectura geográfico-histórica de la raya luso-gallega, en el contexto de este episodio.Palabras clave: República portuguesa, incursiones monárquicas, raya galaico-portuguesa, cartografía propaganda.Abstract: The ideological radicalisation of the republican regime, established in Portugal in October 1910, gave rise to the forming of a conservative and monarchical opposition in exile, in the south of the Spanish historic region of Galicia. Between October 1911 and June 1912, from several Galician villages not far from the Portuguese border, the monarchists made two incursions into the north of the country - the first to Vinhais and the second to Chaves - with the aim of fuelling popular uprisings and a military rebellion against the new regime. However, the Republican troops, more numerous and better equipped, won all the battles. At the time, this episode of civil war received extensive journalistic coverage particularly from the newspapers close to the republican regime. Maps and photographs of the border were widely used to locate and illustrate the events. From the historic-geographical perspective of the Portuguese-Galician border, this paper reconstitutes these movements in the broader historical context.Key words: Portuguese Republic, monarchical incursions, Portuguese-Galician border, propaganda maps.


1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt

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.


Sign in / Sign up

Export Citation Format

Share Document