Gabriel Dumont’s Account of the North West Rebellion, 1885

2021 ◽  
Vol 102 (s1) ◽  
pp. s108-s129
Author(s):  
George F.G. Stanley
Keyword(s):  
Point Of View ◽  
The Other ◽  
Diplomatic History ◽  
North West ◽  
Documentary Sources ◽  
The North ◽  
Accurate Picture ◽  
The Hill

Good generalship requires imagination in the sense of foreseeing what the probable moves of the enemy may be; good military historiography requires not only imagination but the actual study of the documentary sources on each side. It is well known that military, like diplomatic history, is too often presented only from one point of view. A certain bias is unavoidable when the author is familiar with the movements of an army on one side of the hill but can only guess at those of the enemy on the other; an accurate picture of any war, campaign, or battle cannot be presented by a writer who is limited to the records, official and unofficial, available at one G.H.Q., but has nothing more than the conjectures of Intelligence as to what went on at the other.

A New InscribedKioniskosfrom Thebes

2006 ◽  
Vol 101 ◽  
pp. 369-377 ◽  
Author(s):  
Vassilis L. Aravantinos
Keyword(s):  
Point Of View ◽  
The Other ◽  
City Centre ◽  
North West ◽  
Railway Line ◽  
The North ◽  
The One ◽  
The City ◽  
Roofing System

A fragmentary inscription found at Thebes casts new light on the abortive invasion of Athens in 506 by Kleomenes, the Boiotians, and the Chalkidians. On the one hand, it provides valuable confirmation, soon after the event, of the general drift of Herodotos' account of events; on the other, even in its incomplete state, it adds one important detail lacking in Herodotos. And, of course, it tells the story from the Boiotian point of view.The excavation took place in the winter of the year 2001–2 in the property of Evanghelia Madhis at Thebes following her application for the construction of a new house. The plot is situated in the suburb of Pyri, in the north-west periphery of Thebes, about 800 m from the city centre of Thebes, and just beyond the Athens–Thessaloniki railway line (FIG. 1). In it was unearthed a well-built tomb-like cist, made of three rows of large conglomerate stone blocks in regular masonry; similar blocks form its pavement. No traces of covering stones or other relevant materials have so far been discovered. However, since the contents of the cist—including objects such as the bronze inscribed sheets found at the bottom—were probably thrown there when it was abandoned, it may never have been properly covered: no trace of a superstructure or roofing system is preserved on the upper surface of the walls of the cist.

scholarly journals I.—Microscopic Structure of Irish Granites. No. 2. Granite of Aillemore, Co. Mayo

1874 ◽  
Vol 1 (1) ◽  
pp. 1-2
Author(s):  
Edward Hull
Keyword(s):  
The Other ◽  
Microscopic Structure ◽  
South Side ◽  
North West ◽  
Fine Grained ◽  
Lower Silurian ◽  
The North ◽  
Geological Map ◽  
Vertical Walls ◽  
Dark Green

This granite forms an isolated mass, rising into two eminences a few miles south of Louisburg, called Corvock Brack (1287 feet) and Knockaskeheen (1288 feet). It is a greyish granite—generally fine—grained—consisting of quartz, two felspars,—one orthoclase, the other triclinic, probably oligoclase—and dark green mica. In some places there are patches in which the felspar assumes the appearance of “graphic granite.” Numerous boulders of this granite are strewn over the district to the north-west, and on the south side of Knockaskeheen; the rock is traversed by regular joints ranging N. 10 W., along which it splits off into nearly vertical walls. The position of the granite is shown on Griffith's Geological Map of Ireland, and it is surrounded by schistose beds, generally metamorphosed, and probably of Lower Silurian age. The granite itself is of older date than the Upper Llandovery beds, which lie to the southward.

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.

Ugliness and Beauty: the Politics of Landscape in Walter Greenwood's Love on the Dole

2013 ◽  
Vol 29 (1) ◽  
pp. 35-47
Author(s):  
Claire Warden
Keyword(s):  
Twentieth Century ◽  
Working Class ◽  
The Other ◽  
Surrounding Area ◽  
North West ◽  
Avant Garde ◽  
The North ◽  
The One ◽  
The University ◽  
Open Fields

The multi-spatial landscape of the North-West of England (Manchester–Salford and the surrounding area) provides the setting for Walter Greenwood's 1934 play Love on the Dole. Both the urban industrialized cityscape and the rural countryside that surrounds it are vital framing devices for the narrative – these spaces not simply acting as backdrops but taking on character roles. In this article Claire Warden reads the play's presentation of the North through the concept of landscape theatre, on the one hand, and Raymond Williams's city–country dialogism on the other, claiming that Love on the Dole is imbued with the revolutionary possibility that defines the very landscape in which it is set. From claustrophobic working-class kitchen to the open fields of Derbyshire, Love on the Dole has a sense of spatial ambition in which Greenwood regards all landscapes as tainted by the industrial world while maintaining their capacity to function independently. Ugliness and beauty, capitalist hegemony and socialistic hopefulness reside simultaneously in this important under-researched example of twentieth-century British theatre, thereby reflecting the ambivalent, shifting landscape of the North and producing a play that cannot be easily defined artistically or politically. Claire Warden is a Lecturer in Drama at the University of Lincoln. Her work focuses on peripheral British performances in the early to mid-twentieth century. She is the author of British Avant-Garde Theatre (Palgrave MacMillan, 2012) and is currently writing Modernist and Avant-Garde Performance: an Introduction for Edinburgh University Press, to be published in 2014.

scholarly journals Балцкія элементы ў граматыцы традыцыйных мясцовых гаворак паўночна‑заходняй Беларусі

2015 ◽  
Vol 36 ◽  
pp. 51-59
Author(s):  
Вера [Vera] Астрэйка [Astrėĭka]
Keyword(s):  
The Other ◽  
North West ◽  
Language Support ◽  
The North ◽  
The Status ◽  
Formal Level ◽  
The Baltic ◽  
Language Assimilation ◽  
The Given ◽  
North Western

The Baltic elements in the grammar of traditional local dialects of north-western BelarusThe article analyzes a number of grammatical features typical for the North-West dialect zone of the Belarusian language. These peculiarities are interpreted as a possible result of Slavic-Baltic contacts in the region. Some phenomena can be explained as a Baltic (mainly (great)Lithuanian) substratum in North-West Belarusian dialects.The factor of areal neighborhood has to be taken into consideration too. Such phenomenon as language support has effect just in connection with the last one. A lot of the appropriate lingual facts are in restricted and inconsistent use. However, it is possible to be said about more or less significant (now or/and before) tendencies of regional lingual development. These tendencies has not got the status of a structural (= constitutional) lingual regularity. As a rule the wide and compact areas are characterized of some lingual facts (= lexemes), which illustrate the given transformations in the system of Belarusian dialects. Baltic influence upon the North-West Belarusian dialects grammar is detected on as the formal level so the structural one. And it is not noticeable at all times. The definite changes in the sphere of morphology and syntax can provoke different modifications in the other parts of a language system (word building, semantics). The results of this process are the evidences of ethnic and language assimilation of native Balts by Slavs in the region. That comes in support of forming the singular North-West Belarusian regiolect (= the regionally marked variety of a dialect language). Балтийские грамматические элементы в говорах северо-западной БеларусиВ статье анализируется ряд грамматических черт, характерных для говоров северо-западной диалектной зоны беларусского языка. Эти особенности квалифицируются автором как весьма вероятное следствие славяно-балтского языкового взаимодействия в соответствующем регионе. Отдельные явления есть основания рассматривать в качестве возможного проявления балтского (главным образом (пра-) литовского) субстрата в северо-западных беларусских говорах. Фактор ареальной смежности здесь также должен быть принят во внимание. В связи с последним следует упомянуть и действие феномена языковой поддержки. Многие соответствующие языковые факты имеют существенные ограничения в употреблении, в говорах выступают не всегда последовательно и регулярно. В некоторых случаях, однако, можно говорить о действии более или менее выраженных (в настоящем и/или прошлом) тенденций регионального языкового развития, которые пока не приобрели статус структурно значимой (= конститутивной) языковой закономерности. Широкие и компактные ареалы образуют, как правило, лишь отдельные языковые факты (= лексемы), иллюстрирующие данные трансформации в системе традиционных беларусских говоров. Балтское влияние на грамматический строй беларусских говоров северо-западной диалектной зоны выявляется как в плане формального выражения, так и на внутриструктурном уровне. Оно не всегда может быть заметно на первый взгляд. Определенные сдвиги в сфере морфологии и синтаксиса могут повлечь за собой изменения в других областях языковой системы (словообразовании, семантике). Результаты этого процесса являются ярким свидетельством того, что на отмеченной территории действительно имела место этноязыковая ассимиляция неславянского (= балтского) населения и происхо- дило формирование своеобразного северо-западного беларусского региолекта (= регионально обусловленной разновидности диалектной речи).

scholarly journals The Caratacus Stone on Exmoor

1919 ◽  
Vol 9 ◽  
pp. 208-210
Author(s):  
F. A. Bruton
Keyword(s):  
The Other ◽  
Southern Limit ◽  
North West ◽  
The Hill

On the very top of Winsford Hill, the southern limit of Exmoor, more than twelve hundred feet above the sea, two roads meet at right angles, at a point called Spire Cross. One connects the ancient (some say prehistoric) bridge known as Tarr Steps, on one side of the hill, with the picturesque village of Winsford, lying deep down in the valley of the Exe, on the other. The second road runs north-west from Dulverton to Exford, and so to Porlock and Lynmouth, passing on the left Hawkcombe Head, the favourite meeting-place of the Somerset and Devon Staghounds, and the Lorna Doone country.

NEW INSIGHTS INTO THE PAINTED CRUCIFIX ATTRIBUTED TO ANTONIO DE SALIBA, IN THE V&A MUSEUM, LONDON

2020 ◽  
pp. 1-32
Author(s):  
Charlene Vella
Keyword(s):  
Sixteenth Century ◽  
Small Town ◽  
North West ◽  
Documentary Sources ◽  
The North ◽  
Contractual Agreement

The V&A is home to a painted crucifix that has been attributed to the Sicilian master, Antonio de Saliba (c 1466/7–c 1535), who was active in Venice and eastern Sicily during the Renaissance. This paper takes a fresh look at the documentary sources that were published before the devastating earthquake that struck Messina, in the north west of Sicily, in 1908. In re-examining these sources, this paper reveals new insights into Antonio de Saliba’s oeuvre and enables a possible identification of the V&A’s painted crucifix with a specific contractual agreement that links this crucifix’s commission to the artist – specifically with a commission de Saliba received in 1508 from Limina, a small town in the province of Messina. The roots of this provincial commission would explain the persistence of a retardataire production visible in this early sixteenth-century painted crucifix. This paper also challenges the preconceived idea that such painted crucifixes were destined to be displayed high up in a church, on a tramezzo or beam.

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.

Deep Sinking for Coal in the Wyre Forest Coal-Field

The Geologist ◽  
1861 ◽  
Vol 4 (11) ◽  
pp. 468-469
Author(s):  
George E. Roberts
Keyword(s):  
Coal Seam ◽  
Coal Mining ◽  
The Other ◽  
Coal Field ◽  
Coal Seams ◽  
North West ◽  
The North ◽  
Western Border ◽  
Shaft Sinking ◽  
Considerable Range

Some other memoranda which I find among my papers relating to this work (for a section of which, with particulars of shaft-sinking, see “Geologist” of last month) may not be unacceptable to your coal-mining readers.The spot where the shaft was sunk was 476 feet above the level of the Severn Valley Railway at Eymoor, and about 510 feet above the ordinary height of the River Severn, from which it was distant about two miles. The coal seam met with and worked at the depth of 176 yards, has in other parts of the coal-field a thickness of four feet. The colliers regard it as a Flying Reed (red?) coal. Two of the thin coal-seams afterwards sunk through were entirely made up of the remains of Sigillariæ; the coal, in consequence, was “long grained” and slaty. These Sigillarian coals have a considerable range through the Wyre Forest field, and in common with most of the other seams, crop out along the western border. At the Baginswood pits, in the north-west corner of the coal·field, the upper coal, two feet four inches in thickness, worked by hand-draw, being only ten yards from surface, is a most interesting seam, made up entirely of compressed Sigillariæ.

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